How Gateway’s plans to dredge Douglas Channel show the limitations of the JRP mandate and ruling

(First in series of reports on how the Joint Review Panel report will affect the Kitimat region)

JRP map of blasting on Douglas Channel
Joint Review map of Northern Gateway plans for dredging and blasting on Douglas Channel (JRP)

 

If there is a significant flaw in the Joint Review Panel report on Northern Gateway, it can be found in the panel’s analysis of Enbridge Northern Gateway’s plans to blast and dredge at the proposed Kitimat terminal site.

While the Joint Review Panel does consider what it calls “cumulative effects,” the panel plays down those effects and offers no specifics about interaction between the Northern Gateway project and the two liquified natural gas projects, the KM LNG project at Bish Cove and the BC LNG floating terminal at the old log dump.

It appears the JRP considered the legacy effects of the Rio Tinto Alcan smelter and other Kitimat industries while not taking into consideration future development.

The dredging and blasting planned by Northern Gateway, as Enbridge said in its evidence,  appears to have only a minimal effect on Douglas Channel.

A glance at the map in the Joint Review ruling shows that that the dredging and blasting site is directly opposite Clio Bay, where Chevron, in partnership with the Haisla Nation, plan a remediation project using marine clay from the Bish Cove construction site to cap decades of sunken and rotting logs.

The Clio Bay project was not part of the evidence before the Joint Review Panel, the plans for the project were not formulated until well after the time for evidence before the JRP closed. But those deadlines show one area where the rules of evidence and procedure fail the people of northwestern BC.

The JRP is a snapshot in time and changes in the dynamics of the industrial development in the Kitimat Arm are not really considered beyond the terms of reference for the JRP.

It appears from the report that Enbridge plans to simply allow sediment from the blasting and dredging to float down Douglas Channel, dispersed by the currents and the outflow from the Kitimat River.

Northern Gateway said that dredging and blasting for marine terminal construction would result in a sediment plume that would extend over an area of 70,000 square metres for the duration of blasting activities.

Approximately 400 square metres of the assessed area of the marine terminal is expected to receive more than 1 centimetre of sediment deposition due to dredging. Outside of this area, typical sediment deposition levels alongshore where sediment is widely dispersed (a band approximately 4 kilometres long and 400 metres wide) are very low; in the range of 0.001 to 0.1 centimetres. Dredging and blasting activities are expected to occur over a period of approximately 18 weeks.

Northern Gateway expected most of the sediment plume created by construction activities to be minor in relation to natural background levels.

Northern Gateway would use bubble curtains to reduce pressure and acoustic effects of blasting, and silt curtains to reduce the effect of sedimentation from dredging. It said that bubble curtains are used extensively for other activities, such as pile driving, to reduce the effect of high pressure pulses that can cause injury to fish.

It added that bubble curtains have been tested extensively with blasts, and literature shows they are effective.

Northern Gateway said that physical effects from suspended sediment on marine fish and invertebrates could include abrasion and clogging of filtration mechanisms, which can interfere with ingestion and respiration. In extreme cases, effects could include smothering, burial, and mortality to fish and invertebrates. Direct chemical-related effects of suspended sediment on organisms, including reduced growth and survival, can also occur as a result of the uptake of contaminants
re-suspended by project construction activities, such as dredging and blasting, and as a result ofstorm events, tides, and currents.

The Haisla Nation and Raincoast Conservation objected to Northern Gateway’s figures, noting

Northern Gateway’s sediment and circulation model and its evidence related to contaminated sediment re-suspension at the terminal site. Both parties said that the sediment model was applied for the spring, when the increase in total suspended solids would be negligible compared to background values. In the event of delays, blasting and dredging would likely occur at other times of the year when effects would likely be higher, and these scenarios were not modelled.

The panel’s assessment of the area to be blasted found few species:

Species diversity within Kitimat Arm’s rocky intertidal community is generally low. Barnacles, mussels, periwinkles, and limpets can be found on rocky substrate. Sea urchins, moon snails, sea anemones, sea stars, and sea cucumbers are in shallow subtidal areas. Sandy areas are inhabited by commercially-harvested bivalves such as butter clams and cockles.

Northern Gateway told the JRP that it would “offset” any damage to Douglas Channel caused by the blasting and dredging

Northern Gateway said that construction, operations, and decommissioning of the marine terminal would result in both permanent and temporary alteration of marine fish habitat. Dredging and blasting, and installing physical structures in the water column for the marine terminal would permanently alter marine fish habitat. Based on the current terminal design, in-water site preparation would result in the physical alteration of approximately 1.6 hectares of subtidal marine habitat and 0.38 hectares of intertidal marine habitat. Northern Gateway expected approximately 353 square metres of subtidal marine habitat and 29 square metres of intertidal habitat to be permanently lost.This habitat would be compensated for by marine habitat offsets.

The project’s in-water vertical structures that would support the mooring and berthing structures could create new habitat, offsetting potential adverse effects. The structures may act as artificial reefs, providing marine fish habitat, food, and protection from predation. Although organisms currently inhabiting the work area would be killed, the exposed bedrock would be available for colonization as soon as the physical works are completed.

In its finding on marine sediment, the panel, as it does throughout the ruling, believes that the disruption to the environment caused by previous and ongoing human activity, means that the Northern Gateway Kitimat terminal won’t make that much difference.

Sediment quality in the marine environment is important because sediment provides habitat for benthic aquatic organisms. Northern Gateway’s baseline data for the area immediately surrounding the marine terminal indicated some contamination of water, sediments, and benthic organisms from previous industrial activity. Industrial activities in the Kitimat area have released contaminants through air emissions and effluent discharges since the 1960s. Sources of contaminants to Kitimat Arm
include effluent from a municipal wastewater treatment plant, the Alcan smelter, Methanex Corporation’s methanol plant, and the Eurocan pulpmill, as well as storm water runoff from these operations and the municipality.

Area is largely controlled by natural outflow from the Kitimat River with suspended sediment levels being highest during peak river runoff (May to July, and October) and lowest during winter. Storm events, tides, and currents can also suspend sediments. Levels of total suspended solids fluctuate seasonally and in response to climatic variations, but are generally highest during the summer.

Commercial and recreational vessels currently operating in the area may increase suspended solids by creating water turbulence that disturbs sediments. Given the current sediment contamination levels and the limited area over which sedimentation from construction activities would be expected to disperse, the Panel finds that the risk posed by disturbed contaminated sediment is low. Northern Gateway has committed to monitoring during construction to verify the predicted effects on sediment and water quality for both contaminants and total suspended solids..

The dredging and blasting section of the Joint Review Report is small when compared to the much more extensive sections on pipeline construction and tanker traffic, and the possible effects of a catastrophic oil spill.

Although minor, the marine sediment section exposes the question that was never asked, given the disruptions from years of log dumping at Clio Bay and Minette Bay and the decades of  developments at the mouth of the Kitimat River, and future development from LNG, when do cumulative effects begin to overwhelm? How much is enough? How much is too much? If every project continues to be viewed in isolation, what will be left when every project is up and running?

 

Commentary: The earthshaking difference between Enbridge and LNG

Joint Review Panel
The Northern Gateway Joint Review panel, Kenneth Bateman, Sheila Leggett and Hans Matthews, listen to final arguments in Terrace, June 17, 2013. (Robin Rowland/Northwest Coast Energy News)

Buried deep in the LNG Canada environmental assessment application, a reader will find a key difference in attitude with at least one of the group of companies planning liquified natural gas development in the northwest and Enbridge Northern Gateway.

It’s an earthshaking difference, since it’s all about earthquakes.

The documents filed by LNG Canada with the BC Environmental Assessment Office and the Canadian Environmental Assessment Agency acknowledge that there is a possibility of an earthquake (a one in 2,475 year event) at the LNG terminal site.

Northwestern British Columbia was shaken by two major earthquakes in the months before the Joint Review Panel concluded its hearings in Terrace. Both were far from Kitimat, but felt across the District. On October 27, 2012, there was a magnitude 7.8 earthquake on the Queen Charlotte Fault off Haida Gwaii. That quake triggered a tsunami warning, although the actual tsunami was generally limited to the coast of Haida Gwaii. Both landline and mobile phone service in Kitimat was briefly disrupted by both the quake and overloads on the system. Kitimat was also shaken by the 7.5 magnitude earthquake centered at Craig, Alaska a few weeks later on January 9, 2013.

With the exception of one vague reference in its final argument documents presented to the Joint Review Panel, Enbridge has stubbornly refused to consider any seismic risk to the region.

That was the company’s policy long before the October. 27, 2012 Haida Gwaii earthquake and was Enbridge policy after October 27, 2012.

In a public meeting in Kitimat on September 20, 2011, more than a year before the Haida Gwaii earthquake, John Carruthers, Northern Gateway president, insisted to skeptical questioners at a community forum at Mount Elizabeth Theatre that there was no earthquake danger to the proposed Northern Gateway pipeline and bitumen terminal in Kitimat.  One of the questioners, Danny Nunes, of Kitimat, asked could the pipes withstand an earthquake? Carruthers repeated that Kitimat was not in an earthquake zone, that the fault was off Haida Gwaii and so would not affect Kitimat.

After the September, 2011 meeting, I asked Carruthers if Enbridge knew about the March 27,1964 “Good Friday” magnitude 9.2 Alaska earthquake that, because of its high magnitude, had caused major shaking in Kitimat. That earthquake destroyed much of Anchorage and triggered tsunamis that caused damage and death across Alaska and in parts of British Columbia, Oregon and California.

Carruthers promised to get back to me and never did.

On June 17, 2013, six months after the Craig, Alaska earthquake, in his opening summation before the Joint Review Panel, Richard Neufeld, lead lawyer for Northern Gateway, stayed on message track, telling the JRP, referring to pipelines: “The route is not seismically unstable. The seismic risk along the pipeline right-of-way is low, with only a few locations of moderate risk encountered, none of which are within the Haisla territory.”

That brought a gasp from spectators in the room, or at least those who had felt the October and January earthquakes.

The following day, June 18, Murray Minchin of Douglas Channel Watch found an anomaly in the Enbridge documentation, arguing in the group’s summation:

“The Proponent’s written final argument gets on shaky ground regarding design and construction of the storage tanks on a ridge beside Douglas Channel in paragraph 249 where they say:

“‘It also involves the safe construction and operation of the Kitimat terminal in Kitimat Arm in an area subject to seismic activity which encompasses both terrestrial and marine components.’

“Now, that’s interesting because isn’t that the first time — the first admission by the Proponent in a little over 10,000 pages of documents that the area they intend to build their project is in a seismically-active area?

“Haven’t they been telling us all along to this point that the only seismic concerns would be from the distant Queen Charlotte fault off of Haida Gwaii?

“Now, this completely contradicts Mr. Neufeld’s statement yesterday where he described the Project area as not “seismically unstable”. So what is it? This is their final argument and they’re contradicting themselves.”

Minchin went on to quote from the Enbridge argument: “’Seismic conditions in the project area have also been addressed.’

“Well, really? Is that a truthful statement, considering Natural Resources Canada has only submitted a preliminary report concerning a 50-kilometre fault line and massive submarine landslides they accidentally discovered last year in Douglas Channel while doing a modern survey of the Channel for navigation hazards.

“How can the Proponent claim to have adequately addressed seismic forces in their design of this Project when they don’t know what those forces are or for what duration they may be subjected to those forces.

“Has there ever been a paleoseismological study in the Project area to establish past earthquake or tsunami history?

“Wouldn’t it be in the best interest of the Proponent, the Panel and Canadians to know the risks before 1.3 billion litres of liquid petroleum products are allowed to be stored on a low ridge right beside Douglas Channel?”

In his final rebuttal on June 24, Neufeld did not address the contradictions that Minchin had pointed out.

Compare Enbridge’s attitude to the view of LNG Canada, which at very least, appears willing to consider that major events could have adverse consequences on the terminal and liquifaction facilities.

    • The first one is a bit puzzling to Kitimat residents “A 1 in 100 year 24 hour rain event,” after all the town often gets rain for 24 hours straight or more fairly often.
    • The second, 1 in 200 year flood of the Kitimat River. Flooding has always been a concern and will be even more so, because as the pipelines come into town, whether natural gas or bitumen, those pipelines will be close to the river bank.
    • The 1 in 2,475 year seismic event. That figure is probably correct for a local event given the geology of the Kitimat Valley—unless, of course, the fault line discovered by the Geological Survey of Canada on Hawksbury Island proves to be a potential danger.
    • A tsunami.
    • Change in flow of the Kitimat River.
    • Even more interesting is that LNG Canada is willing to consider possible effects of climate change on the project, saying: “Predicted climate change effects during the project lifecycle on sea-level rise, precipitation and temperature. Where relevant and possible, the implications of such climate induced changes to the extreme weather events given above will also be addressed.”

.

Although the hydrocarbon industry as a whole is reluctant to acknowledge climate change, it appears that on a practical level, the LNG Canada partners, if they are about to invest billions of dollars in a natural gas liquifaction plant and marine terminal, will certainly take steps to protect that specific investment from the effects of climate change.

On the other hand, the National Energy Board, as matter of policy and the Northern Gateway Joint Review Panel, both still stubbornly refuse to even consider any effects of climate change, even possible effects locally on a specific project application.

The Joint Review Panel decision on the Northern Gateway is expected sometime in the next three weeks. While most reports seem to indicate that the decision will be released after Christmas before the Dec. 30 deadline, there has been recent media speculation that the decision could be released next week.

In the meantime, Enbridge has pulled out all stops in a public relations campaign to build support for the Northern Gateway. While a recent poll indicates that advertising campaign may be having some success in the Lower Mainland, the same poll showed that 65 per cent of northern BC residents oppose or strongly oppose the Northern Gateway.

The problem for Enbridge is that the new public relations campaign is repeating the blunders that began when they first proposed Northern Gateway in 2005. There have been meetings across the northwest, but those meetings have been invitation only affairs at chambers of commerce and community advisory boards, with possible opponents or skeptics and media perceived as critical of Enbridge not invited. So Enbridge still wants to control the message and will only talk to friendly gatherings.

Then there are the television spots featuring Janet Holder, the Enbridge vice president in charge of Northern Gateway, supposedly showing her commitment to wilderness. Those commercials would have had more credibility if the agency had produced the ads with actual video of Holder walking through the bush, rather than shooting the spots in front of a green screen in a studio, with pristine wilderness stock video in the background, and Holder acting as if she was a model for an adventure clothing company rather than  vice president of a pipeline company.

Right-wing business columnists in Toronto and the countless Albertans fume at the so-called “hypocrisy” of British Columbians who support LNG and oppose bitumen.

Of course, those critics didn’t feel the earth move under their feet.  The critics don’t see the difference between natural gas and bitumen, differences very clear to the people of British Columbia.

It’s more than the fact, that so far, the LNG projects have been relatively open and willing to talk to potential adversaries,  as Chevron has done on the controversial Clio Bay project; more than the fact that if even a fraction of the LNG projects go ahead, the money coming into northwestern BC means that the handful of permanent jobs promised by Enbridge will be literally a drop in a bucket of warm bitumen.

Although there are many other environmental issues on the Northern Gateway project, the fact the potential for earthquakes in Kitimat is brushed off by Enbridge while LNG Canada is at least willing to consider the problem, sums it all up.

 

Updated with link to Sept. 2011  questions and answers

 

 

 

 

 

 

 

Clio Bay: Clay capping “relatively new technique”: DFO statement

Carrie Mishima, a communications advisor for the Department of Fisheries and Oceans sent this statement in response to questions from Northwest Coast Energy News:

· The proposal by the Kitimat LNG project uses a relatively new technique that is expected to improve aquatic habitat in Clio Bay. The bay has been used as a log handling site for decades, resulting in areas of degraded habitat from woody debris on the seafloor. The project will cap impacted areas with inert material to restore the seafloor.

· Capping at smaller-scale sites in Canada has shown that the technique has successfully restored low-value aquatic habitat.

· The project will implement standard and project-specific measures to protect fish and aquatic habitat and will conduct a five-year monitoring program to determine how well the habitat is recovering.

· Data from the monitoring program will be used to guide future habitat reclamation at impacted habitat sites. Reference sites are being established as benchmarks against which the capped sites can be measured.

· Site-specific standards for dissolved oxygen levels will be developed for the enhanced site by sampling a control site having similar habitat parameters.

· Detailed mapping has been done to identify the best areas for the soil placement and to protect sensitive habitat such as intertidal areas, rocky substrates and eelgrass beds.
· Other required mitigation measures will include analyzing the cap material to confirm it is free of contaminants and placing this material during appropriate tidal conditions to ensure accurate placement of the cap in accordance with design plans.

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Special report: Clio Bay cleanup: Controversial, complicated and costly

Special report: Clio Bay cleanup: Controversial, complicated and costly

Log booming at Clio Bay
Log booming operations at Clio Bay, August 21, 2013. (Robin Rowland/Northwest Coast Energy News)

Chevron, the company operating the KM LNG project at Bish Cove and the Haisla Nation have proposed that marine clay from the Bish Cove construction site be used to cap more than 10,000 sunken and rotting logs in Clio Bay. Haisla Chief Counsellor Ellis Ross says he hopes that using clay to cover the logs will help remediate the environmentally degrading sections of the Bay. The proposal has brought heated controversy over the plan, both among residents of Kitimat and some members of the Haisla Nation, who say that Clio Bay is full of life and that the capping will cause irreparable damage.

An investigation by Northwest Coast Energy News shows that capping thousands of sunken logs is a lot more complicated and possibly costly than anyone has considered. It is also clear that many of the comments both supporting and opposing the Clio Bay project are based on guesses rather than the extensive scientific literature available on the subject.

Northwest Coast Energy News findings include:

  • In 1997, the Department of Fisheries and Oceans surveyed sunken log sites in Douglas Channel. The results, published in 2000, identified 52 sites just on Douglas Channel and the Gardner Canal that had various levels of enviromental degradation due to sunken logs. Clio Bay was not the list. The DFO scientists recomended followup studies that never happened.
  • Scientific studies show that degradation from sunken logs can vary greatly, even within one body of water, due to depth, currents, number of logs, and other factors. So one part of a bay can be vibrant and another part environmentally degraded due to low levels of dissolved oxygen and decaying organic material.
  • If  KM LNG wasn’t paying for the remediation of Clio Bay, it could be very expensive. Capping sunken logs at a cove near Ketchikan, Alaska, that is the same size and shape as Clio Bay cost the US and Alaska governments and the companies involved $2,563,506 in 2000 US dollars. The total cost of the cleanup of the site which was also contaminated with pulp mill effluent was $3,964,000. The estimated cost of capping the logs in the Alaska project was $110 per cubic yard.
  • The Alaska project shows that a remediation project means while most of the logs in a bay or cove can be capped, in some parts of a water body, depending on currents, contamination and planned future use, the logs have to be removed and the area dredged.
  • Agencies such as the State of Alaska, the US Environmental Protection Agency and the US Army Corps of Engineers all recommend using “clean sand” for capping operations. Although “clay balls” have been used for capping in some cases, the US officials contacted say they had no record of large amounts of marine clay ever being used for capping. They also noted that every log capping project they were aware of happened in sites that had other forms of contamination such as pulp mill effluent.
  • Chevron only recently retained the environmental consulting firm Stantec to study Clio Bay. The Department of Fisheries and Oceans has told District of Kitimat Council it recently completed mapping of the seafloor at Clio Bay. The Alaska project was preceded by five years of monitoring and studies before capping and cleanup began.
  • A letter from Fisheries and Oceans to the District of Kitimat says that Clio Bay has been mapped and the department is planning to monitor any capping operations. However, it appears from the Department of Fisheries and Oceans website that the department has no current policies on remediation since the Conservative government passed two omnibus which weakened the country’s environmental laws. According to the website, new remediation policies are now being drafted. That means that although DFO will be monitoring the Clio Bay operation, it is uncertain what standards DFO will be using to supervise whatever happens in Clio Bay.

Northwest Coast Energy News is continuing its investigation of the sunken logs problem.  Expect more stories in the days to come.

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Clio Bay: Dead or alive?

Special report: Clio Bay cleanup: Controversial, complicated and costly

Log booming at Clio Bay
Log booming operations at Clio Bay, August 21, 2013 (Robin Rowland/Northwest Coast Energy News)

Updated October 3, 2013, with DFO statement

One of the major concerns about Clio Bay is the possible lack of oxygen to support sealife. While some people have called Clio Bay “dead,” others have pointed to catches of crab, cod and salmon to dispute that.

The experience at Ward Cove, Alaska, even though it was more polluted than Clio Bay, shows that oxygen levels are highly variable, depending on season, location and depth.

In 1995, the DFO`s Institute of Ocean Siences studied dissolved oxygen levels in Minette Bay, and concluded, according to a report posted on the DFO website, that because Minette Bay was stagnant from May to November” and those conditions existed even before industrial development in the Kitimat Valley:

Examination of all the dissolved oxygen  data showed that conditions before  or early in the industrial  development  of  the  region  were  not  significantly different from those observed in the 1995 to 1996  study.  On the basis  of these analyses we concluded that log storage and handling  activities in the bay do not appear to have exacerbated the naturally occurring low dissolved oxygen conditions.

Ward Cove

The US Enviromental Protection Agency studied disolved oxygen levels at Ward Cove during water quality monitoring from 1998 to 2002. The monitoring found that dissolved oxygen levels of less than 4 milligrams per litre commonly occurred in Ward Cove during the summer and early fall. “During this time, hypoxic  conditions (dissolved oxygen less than 2 milliggrams per litre) occurred occasionally at and near the bottom and less frequently in midwater areas. Hypoxia can be dangerous to both fish and bottom dwelling species.

The EPA study showed that water circulation is restricted within Ward cove. A counter-clockwise circulation brings ocean water from Tongass Narrow into the cove along the south shore. That water usually exits after 15 days.

The EPA studied dissolved oxygen in Ward Cove from November 1995 to October 2002, using 13 monitoring stations, nine inside the cove and four outside in Tongass Narrows.

Water monitoring stations at Ward Cove, Alaska
Map of water quality sampling stations in Ward Cove, Alaska (EPA)

This monitoring found that the water column is strongly stratified during the summer resulting in poor mixing of bottom water. The EPA says during the monitoring period:

dissolved oxygen levels between 2 and 4 mg/1 were commonly observed in Ward Cove. These conditions began at water depths greater than approximately 20 metres in mid to late July and continued until early October, but oxygen levels between 2 and 4 mg/1 may also occur in water as shallow as 15 metres.

The EPA says the normal oxygen level for the surface waters of Ward Cove is approximately 8 mg/1 at 10°C. Under natural conditions and vertical stratification, dissolved oxygen levels in deeper waters can vary considerably and be reduced significantly below 8 mg/1 by respiration and the decay of organic materials, including sunken logs.

Since Clio Bay is deeper than Ward Cove, that means dissolved oxygen levels could be decreased at the greater depths.

Map of oxygen levels in Ward Cove
Maps showing differing levels of dissolved oxygen during monitoring at Ward Cove. Alaska (EPA)

Salmon

The Ward Cove study also confirmed laboratory studies that showed that salmon can detect and avoid areas of low oxygen. Coho, pink, sockeye, chum, steelhead, Dolly Varden and Cutthroat trout are all native to the cove. Introduced Chinook are also found at Wards Cove.

A Ward Cove report says:

Depressed dissolved oxygen conditions are unlikely to significantly affect the growth of juvenile or adult salmonids migrating through or feeding in or near Ward Cove. Some minor indirect effects, however, may occur as a result of hypoxia-induced changes to food chain organisms inhabiting the cove and adjacent waters.
The growth cycles of the adult stage of all seven anadromous salmon and trout species native to Ward Creek should be completed prior to their arrival in the cove from the ocean. Some feeding by adult cutthroat trout and Dolly Varden may occur in or near the cove as they hold in preparation for entering Ward Creek. The growth of subadult chinook salmon, a fish species not native to Ward Creek, is also not likely affected by exposures to these conditions.
Returning adult salmonids may be present in the cove when the lowest dissolved oxygen and highest water temperatures occur in late summer and early fall. Adult salmonids will usually avoid hypoxic conditions, except when staging to enter freshwater during the latter part of their annual spawning migrations. Severe depressed DO levels at this time in combination with low flows and high water temperatures in Ward Creek can result in adult mortality. Fish kills have not been observed recently in the cove, likely because the depressed DO conditions have not extended into a greater portion of the water column in combination with low flows in Ward Creek.

As for other species, the report says reaction varies, with species that are able to swim often leaving areas of depressed oxygen. Previous studies have shown that bottom dwelling species may be able to tolerate low oxygen for a short time and become susceptible if they don’t swim out of the area. Those species who are are not mobile, have weak swimming abilities, or live within the sediment are more likely to be susceptible.

That means that changes in oxygen level could mean that deaths or migration of mobile bottom dwelling species at a location, leaving the impression that species are no longer around, even though the changes may be seasonal. Scientific studies show that low oxygen levels can also make all species in that area vulnerable to disease due to stress. Low oxygen also limits swimming ability and makes a species more prone to predation.

Minette Bay

Log boom at Minette Bay
Log boom at Minette Bay. April 14, 2013. (Robin Rowland/Northwest Coast Energy News)

From August 1995  until October 1996, the Department of Fisheries and Oceans (Institute of Ocean Sciences and the North Coast Division  of Habitat  Management)  with  the support local companies studied the water quality in Minette Bay.

A 1961 study of oceanography of the BC fjords and a second study of in 1968 had already reported finding low dissolved oxygen levels in Minette Bay.

As far back as 1975, the report says:

Concerns have been raised that the poor water quality of the bay is exacerbated if not caused directly by the log handling practices there.  Other habitat disruptions have been attributed to the industrial activities associated with log handling practices in this bay, e.g. bottom scouring, bark litter, and sinkers.

The DFO report says that the purpose of our study of Minette Bay was to determine if log handling in the bay “significantly contributed  to  low dissolved oxygen concentrations.”

The study of Minette Bay was similar to the one then starting at Ward Cove, but on a much smaller scale, checking salinity, temperature and levels of dissolved oxygen.

The report says:

The renewal of Minette Bay deep waters occurs annually during the winter and early spring months.  Renewal occurs in the form of multiple events, some of which penetrate to the bottom while others only affect the intermediate waters.  These events are caused by the outbreaks of the Arctic air mass over the region.   The cold air temperatures reduce run-off thereby increasing  surface salinity while at the same time the strong outflow winds push the surface layer away from the head of Kitimat Arm and bring denser water closer to the surface. The cold outflow winds also cool and mix the surface waters.  In the stagnant period from May to November, dissolved oxygen concentrations in the deep waters decline rapidly to near zero conditions by July and remain low until the late fall.

The 1995 study concluded, based on surveys and reports from the previous 45 years, that measurements of dissolved oxygen in 1951 before the Alcan smelter was built, through measurements in the 1960, were not different from the 1995 measurements in the deep waters.`and concluded  “that log handling practices in the bay have not exacerbated the naturally occurring low DO conditions in the bay.”
`
It goes on to say while log storage and handling at Minette Bay had no apparent effect on dissolved oxygen:

other deleterious effects on water quality and  habitat  are  possible.  These impacts might include: the disruption of animal and plant ‘life on and in the sediments by the grounding of log booms or scouring  of the bottom  sediments   by  the  movement  of  log  booms;  the  alteration  of  the  natural composition of the sediments and the benthic community by the accumulation of bark, whole logs and other wood debris on the sediments underneath the log storage areas and in the log dump zone; anoxia in sediments due to an increased organic load; and toxic concentrations of leachates from the logs and other wood debris.

It called for further studies of Minette Bay such as using an underwater camera, could provide  a cost effective  way to visually inspect and classify the bottom sediments. Those sediments could then be sampled

based on the preliminary  mapping  of  sediment  characteristics,  log  handling  impacts  and  visual ·surveys. At these locations the benthic community should be sampled for diversity and species composition.  This information by itself or in conjunction with historical surveys in the bay and Kitimat Arm may give a sense of the degree of impact that log handling operations are having on the ecology of Minette Bay.

It also called for studies for “two small inlets that have very shallow sills; Foch Lagoon which has a 4 metre deep sill at low water and the other is Kiskosh Inlet which has a 2 metre deep sill.”

It notes

Kiskosh Inlet has a maximum depth of about 53m and is more like Minette Bay than Foch Lagoon which has a much deeper basin (250m).  Their very shallow sills suggest that the deep basin waters in these two inlets may be oxygen depleted.  A comparison with Minette Bay may be instructive as there are no log storage or handling activities in either of these inlets.

In 1997, DFO created a list of 52 sites on Douglas Channel that were used as active, abandoned or potential log dump sites, as targets for studies. The east and west sides of Minette Bay were two items on the list. Clio Bay, Foch Lagoon and Kiskosh Inlet were not on that list.

Haisla Chief Counsellor Ellis Ross says that if the Clio Bay capping project works, Minette Bay should be next.

Dissolved oxygen standards

The state of Alaska has set standards for dissolved oxygen in marine water with a minimum of six milligrams per litre in the one metre surface layer for coastal water and 5 milligrams per litre in estuaries, “except where natural conditions cause this value to be depressed,” with an additional standard of a minimum of 4 milligrams per litre at any one point in both coastal waters and estuaries.

In a statement to Northwest Coast Energy News, DFO spokesperson Carrie Mishima said, “Site-specific standards for dissolved oxygen levels will be developed for the enhanced site by sampling a control site having similar habitat parameters.”

It appears from documents posted on the DFO website that dissolved oxygen monitoring has been dismissed by DFO as too expensive until the issue became important to fish farming.

A 2005 DFO report on the Bay of Fundy noted

The time has therefore arrived for Canada to proceed seriously and rapidly toward the development and implementation of adequate dissolved oxygen standards and management protocols for the marine coastal zone and aquaculture. Such an effort will enable us to avoid the serious eco-socio-economic consequences associated with poor water quality. From a risk analyses perspective the dissolved oxygen issue might be classified as manageable. Aquaculture takes place in a relatively small proportion of the Canadian coastline and it is only within some of these areas that aquaculture is intense enough to pose potential problems. Hence, the likelihood of a major aquaculture induced depletion of dissolved oxygen is probably low to moderate and the impact of reductions is also probably low to moderate.

Another 2005 DFO report, again on aquaculture, based on meetings in Ottawa noted:

Dissolved oxygen is not yet an easily applied regulatory tool on a specific case-by-case basis, and views were mixed regarding its promise as a candidate for monitoring environmental quality in the coastal zone. However, it is one of the few options available for monitoring over hard bottoms. It is also a useful tool for predicting and assessing far-field effects in environments where oxygen levels may be a concern.

This despite the fact that Alaska and the EPA had been monitoring dissolved oxygen and setting standards for the previous decade.

Canada does not yet have national standards for dissolved oxygen levels in coastal waters. DFO says “site specific” standards will be applied at Clio Bay, but so far there are no details of what those standards will be.

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Clio Bay remediation project “killing two birds with one stone,” Ross says

Special report: Clio Bay cleanup: Controversial, complicated and costly

 

Ellis Ross
Haisla Nation Chief Counsellor Ellis Ross at Bish Cove, June 19, 2013. (Robin Rowland/Northwest Coast Energy News)

Haisla Chief Counsellor Ellis Ross says that capping the logs at Clio Bay was a Haisla idea, taking advantage of the opportunity to use the marine clay from Bish Cove to bring back the Clio ecosystem.

The Haisla were told by experts who video taped the bottom of Clio Bay that are between 15,000 to 20,000 sunken logs in Clio Bay.

“I know because I’ve spent a lot of time down there plus my dad actually worked for the booming company for years and knew what was going on out there,” Ross said. “There are two extreme areas we’re talking about, if you look at Clio Bay where it’s estimated that there 15,000 to 20,000 logs down there, imagine what Minette Bay looks like? And it’s all iron, it’s steel. It’s not just wood, there are a lot of cables down there.

Retrieved cables
Cables retrieved from Ward Cove, Alaska, during dredging and capping in 2001. (EPA)

“The Haisla have known about the degradation of our territory for years. The problem we have as Haisla members is to restore the habitiat is that nobody wants to clean up the habitat. This was our idea, after review from technical experts from DFO as well as our own experts. We’re looking for a three way solution, with the company, DFO and the Crown and the Haisla.”

“I’d love to go and catch halibut and cod, like my ancestors used to.”

He said that the Haisla have beem aware of environmental problems from sunken logs for decades and have been asking for cleanup of degraded areas since 2004, not just at Clio Bay, but in the Kildala Arm and at Collins Bay, which were studied by DFO in 1997.

“The logs are down there, they are oxidizing, but no one wants to do anything about it, including the company and including the Crown. We had independent people come in and review it and have them come up with a recommendation. There was a small scale project [involving marine clay] that proved that this could work.

“This system here is killing two birds with one stone, get rid of the clay and try to remediate some of the habitat,” Ross said.

He said that the original estimate of marine clay excavated at Bish Cove was 10,000 cubic metres. That has now risen to about 3.5 million cubic metres because the KM LNG project is digging deeper for the foundation of the LNG terminal. The original plan called for disposing 1.2 million cubic metres at sea and another 1.2 million cubic metres on land.

“The original idea was to dump the clay in the middle of the ocean. In small amounts it could have been mitigated, but in large amounts we said ‘no.’ If we try to dump clay in the middle of the channel, we have no idea where it’s going to end up, what the effect is going to be.” Ross said. “We did the same thing here for the terrestrial side, we said ‘OK that with the rock quarries above Bees Creek,’ use the clay to help remediate that as well, bring it back.”

Asked about Ward Cove in Alaska, where the US Environmental Protection Agency ordered a cleanup, Ross said. “The difference here is that no one is ordering these companies to clean up the sites, they walk away. No one is taking responsiblity, The Haisla are trying to do this within the parameters they’ve given us.So if someone could come in and order these companies and do something, we’ll look for something else to do with the clay. Until that day comes, the Haisla are still stuck with trying to bring back this land by ourselves. If the District of Kitimat wants to pay the bill, great. Let’s see it.

“We need to put pressure on the province or Canada to cleanup these sites. We’ve been trying to do this for the last 30 years. We got nowhere. Before when we talked about getting those logs and cables cleaned up, it fell on deaf ears [at DFO]. They [DFO] had no policy and no authority to hold these companies accountable. So we’re stuck, we’re stuck between a rock and hard place. How do we fix it?”

Ross also noted that Shell’s LNG Canada project also faces remediation problems, “Shell is going to have the same problem, their’s is going to be different, they’re going to have get rid of contamination on the ocean bottom and beneath that it’s basically going to be gravel, it’s not clay, they’re going to have get rid of that product.”

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Clio Bay: Ward Cove, Alaska, benchmark for log remediation

Special report: Clio Bay cleanup: Controversial, complicated and costly

Ward Cove
Ward Cove, Alaska, in 2005, after the remediation of the bay was completed in 2001 and old industrial buildings were being demolished. (EPA)

 

Ward Cove, just eight kilometres west of Ketchikan, Alaska, was so polluted by effluent from pulp and saw mills and a fish plant, and filled with 16,000 sunken lots that it qualified for a U.S. Environmental Protection Agency Superfund cleanup.

The Ward Cove project is now considered a benchmark for cleaning up similar bays. Alaska officials emphasized to Northwest Coast Energy News, that while Ward Cove does provide guidelines for capping and dredging logs, they were not aware of any project where logs were capped that did not have other forms of contamination.

If you take a look at satellite images of Clio Bay, BC and Ward Cove side by side you immediately you see the similarities and differences between the two bodies of water. (Note due to parameters of Google Earth, images are slightly different scales)

Satellite image of Clio Bay
Google Earth image of Clio Bay
Google Earth image of Ward Cove, Alaska
Google Earth image of Ward Cove, Alaska

Both Clio Bay and Ward Cove are 1.6 kilometres long, somewhat elbow shaped, off a main channel and surrounded by mountains.Ward Cove is 0.8 kilometres wide. Clio Bay is about 0.5 kilmetres wide, 0.8 at its widest point. Both have steep slopes from the mountains. Ward Cove is 61 metres deep at the mouth of the cove, descreasing toward the head. Clio Bay is deeper, 182 metres at the mouth, 90 metres in the centre and between 20 metres and 9 metres at the head.

Both Clio Bay and Ward Cove are subject to tidal circulation. Both Clio Bay and Ward Cove are also influenced by fresh water. Ward Cove is fed by Ward Creek, a smaller Walsh Creek and runoff precipitation the enters the cover from the steep mountain slopes. Clio Bay is fed by one creek, a number of small streams and mountain slope runoff, especially during the spring melt.

Haisla Chief Counsellor Ellis Ross estimates there are between 10,000 and 20,000 sunken logs in Clio Bay. The official summary from the United States Environmental Protection Agency said there were 16,000 sunken logs in Ward Cove.

The major difference with Ward Cove is that it was the site of major industrial development including a pulp mill, a sawmill and a fish plant. That meant the level of pollutants in Ward Cove were much higher than in Clio Bay, which has never been used for an industrial plant. It was the pollutants in Ward Cove, mainly ammonia, hydrogen sulfide, and 4-methylphenol combined with the thousands of sunken logs that made the cove a target cleanup and the associated studies.

A fish plant, Wards Cove Packing opened in 1912 and ceased operations in 2002. The Ketchikan Paper Company mill began operating in 1954 and closed in 1997. Prior to 1971, with the rise of the enviromental movement no permits were required by KPC for discharging effluent into the cove. After that the US Environmental Protection Agency issued a discharge permit and monitored effluent. Throughout the time the KPC mill was operating, the EPA says, “high volumes of log storage (approximately 7 billion board feet) caused accumulation of bark waste and sunken logs at the bottom of the cove.” Gateway Forest Products, a sawmill and veneer plant, continued to store logs in Wards Cove until 2002.

A 2009 monitoring report, conducted by the US Army Corps of Engineers after the cleanup for the EPA noted:

An ecological risk assessment was also conducted using a food-web assessment to estimate risks of bioaccumulative chemicals to representative birds and mammals at the top of the Ward Cove food web. The chemicals evaluated were arsenic, cadmium, mercury, zinc, chlorinated dioxins/furans, and PAHs. The results of this assessment indicated that there are no unacceptable risks to higher trophic level organisms in Ward Cove.

A human health risk assessment was conducted to identify potential risks posed by chemicals detected in sediments or seafood (e.g., fish, shellfish). Ingestion of seafood that may contain chemicals bioaccumulated from the sediments was identified as the only complete exposure pathway for humans. The chemicals that were evaluated included: arsenic, cadmium, mercury, zinc, phenol, 4-methylphenol, chlorinated dioxins/furans, and PAHs. Results concluded that sediments in Ward Cove do not pose an unacceptable risk to human health.

A 2007 report on the Wards Cove remediation from the Alaska Department of Environmental Conservation, noted:

The continuing residues impairment in Ward Cove is caused by the historical accumulation of wood waste on the bottom of the cove. The waste includes an estimated 16,000 sunken logs over at least 75 percent of the bottom and decomposing pulp, wood, and bark waste in sediments in thicknesses up to 10 feet over at least 50 percent of the bottom. Wood waste residues can displace and smother organisms, alter habitat, release leachates, create anoxic conditions, and produce toxic substances, all of which may adversely affect organisms that live both on top of sediments and within sediments.

That is a similar problem to Clio Bay.

The report notes that problems with oxygen increase with depth, noting:

The dissolved oxygen impairment was due largely to the fish-processing waste discharge from the seafood processing facility until 2002, and it was limited to the summer months in deeper waters of the cove (below the picnocline, or stratification layer, approximately 10 meters deep). With that discharge removed, limited monitoring in August and September 2003 indicated that dissolved oxygen impairment might remain near the bottom in waters at depths of 30 meters and greater at certain times and locations due to low natural levels of dissolved oxygen and the continuing decomposition of wood waste. Above 30 meters depth, the waters of the cove appeared to meet the [Alaska state] standard for dissolved oxygen. However, there may be limited capacity for waters at 30 meters and deeper to receive additional loading of oxygen-demanding materials and still meet the standard in summer months.

That should mean that the worries about oxygen depletion at Clio Bay are justified due to Clio’s greater depth.

Studies of the biology of Ward Cove began in 1951, with more in the 1960s and one in 1974. In 1995, Ketchikan Paper Company signed a consent decree with the EPA that called for remediation of Ward Cove, In 2000, KPC and Gateway Forest Products signed a second consent decree with the EPA. Those agreements called on the companies to dredge sediments to improve navigation, remove logs and other debris from the dredging areas and “placing a thin-layer cap of 15-30 cm (six to 12 inches) of sand over about 11 hectares (27 acres) of sunken logs.”

The major studies of Ward Cove began in 1995 after first consent decree. The remediation did not take place until the initial studies were complete in 1999, with dredging and capping taking place from November 2000 to March 2001.

The EPA positioned 13 water quality monitoring stations which operated from 1997 to 2002, to measure salinity, temperature and disolved oxygen, nine inside Ward Cove and four outside the cove in Tongass Narrows. Those studies showed that levels of dissolved oxygen in the cove varied by season, depth and location. Many species from salmon to mobile bottom dwellers like crabs were often able to detect and avoid low oxygen areas.

The plan

The EPA and the companies involved planned the remediation so that it included both dredging, capping logs and sediment and leaving some areas where nature would take its course.

The reports say that complete dredging, removal and disposal of the contamination would have cost $200 million,  The total actual cost of the Ward Cove Remediation Project, beginning with development of the Remedial Design Work Plan, was estimated to have cost $3,964,000 (in 2000 US dollars).

The EPA says cost for the capping component of the project “including preliminary field investigations and reporting, design and plans development, post construction engineering, procurement, construction management, project management, mobilizationm demobilization, engineering/QC and science support, surveys, and capping items” was $2,563,506. Based on the volume of capping material placed, the unit cost of log capping for the Ward Cove Remediation Project was $110 per cubic yard.

Sunken logs retrieved at Ward Cove.
Old logs retrieved from Ward Cove, Alaska during dredging operations to improve navigation. (EPA)

The plan called for dredging about 17,050 cubic yards in the area near the cove’s main dock and the dredging of 3,500 yards metres nearby to improved navigation. Before the dredging, 680 tonnes of sunken logs had to be removed. After dredging, a “thin-layer cap of clean, sandy material” was placed in dredged areas unless native sediments or bedrock was reached during dredging.

In other areas, most covered in sunken logs, the plan called for placement of a thin-layer cap (approximately 6- to 12-inches) of clean, sandy material, with the possibility of “mounding” dropping mounds of sand on specific areas. The 2009 report says the area of sand deposits actually increased “due to the fact that thin layer placement was found to be successful over a broader area, and it was not necessary to construct mounding.”

The plan called for natural recovery in areas where neither capping nor mounding was practicable and so about 50 acres was left alone. (DFO says it plans to leave some parts of Clio Bay uncapped as “reference areas.”)
Slope and sand

Sand capping at Ward Cove
A dredging barge depositing clean sand (originally from Sechelt, BC) during capping operations at Ward Cove, Alaska in 2001. (EPA)

Two studies were carried out as part of the remediation at Ward Cove that do not appear to be contemplated at Clio Bay. The first looked at the “ability of the organic material to support the weight of 15 to 30 centimetres of sand.” Standard engineering equations used at other fill and capping sites were used as part of that study. A second study was carried out to determine the “minimum safety for a given slope,” which given the steep mountains that line Clio Bay, are likely to be factor in the deposit of marine clay. That study determined “For a silty fine sand and a factor of safety of 1.5, the maximum slope would be approximately 40 per cent.”

Those studies led to the conclusion that for the Ward Cove remediation project, the material to be placed on the fine organic sediment could not be gravel and course sand.”

That’s because the larger gravel and course sand “would tend to sink into the sediment and would not provide quality benethic (seabottom) habitat.”

The project decided to use “fine to medium sand with minimal fines.” It also concluded “Because of the very soft existing sediments and steep slopes at Ward Cove, the … material must be released slowly so that the settling velocity is low and bed impact minimized.”

That meant that the EPA had look for a source of quality sand that met their criterion. The sand was found at Construction Aggregates in Sechelt, BC, loaded on 10,000 tonne deck barges, tugged up the coast, unloaded onto land using a conveyor and stockpiled while more tests were done to determine how to deposit the sand on the sunken logs.

Sand bucket at Ward Cove
Dredging bucket modified to deposit sand during capping operations at Ward Cove, Alaska. (EPA)

Sand was placed on a smaller barge and taken to the deposit site. Initial tests were done with a mechanical dredge equipped with a clamshell bucket. The operator deposited the sand using “swaths” released from the bucket. To make it work properly, the bucket, as supplied by a manufacturer had to be modified by welding baffle plates to the bucket and lengthening the chains to insure consistent deposition of the sand. Two computers with special software called WINOPS, designed for dredging operations  “provided the operator and deck engineer the precise locations of the derrick barge position” in order to ensure precise deposition of the sand. WINOPS dredge positioning and guidance software. The WINOPS system made use of three differential global positioning receivers. One GPS receiver was located at the top of the derrick and provided the center positioning of the dredge bucket. Two fixed receivers, one near the starboard center spud and one near the center aft, provided the barge position and heading.

Although using marine clay is likely to produce different engineering challenges at Clio Bay, it is not currently clear that the project has contemplated the level of precision that was used at Ward Cove.

While KM LNG must find a way to dispose of the marine clay from the Bish Cove excavation site, there is a silver lining for the Haisla Nation’s aim of restoring both Clio Bay and the other 50 sites in their traditional territory, since the Kitimat Sand Hill would likely be a ready resource for any future projects.
Monitoring

The EPA considered the project finished in September 2001, and long term monitoring began, with major updates every five years in 2004 and 2009.

An EPA report on the 2004 review showed that the three sand-capped areas and one shallow natural recovery area (not sand-capped) had achieved biological recovery; three other natural recovery areas tested had not achieved biological recovery but were making significant progress.

The  2004 studies showed that benethic (sea bottom) communities in uncapped areas showed “species commonly found in areas where organic enrichment is low or declining.” adding “In three other natural recovery areas, benthic communities have not progressed as far toward recovery but are making significant progress.

By the time of the 2009 update, most of the old industrial infrastucture on land at Ward Cove had been demolished and the land area was slated for redevelopment. Many of the companies that had been there had either gone out of business or had declared bankruptcy and the land was taken over by the Ketchikan Gateway Borough,mostly through foreclosure.

The EPA declared that “The remedial action construction is complete, and the remedial action is an operating or ongoing remedial action.”

The 2009 report says that the project was successful in eliminating sediment toxicity. The area was then quickly being recolonized by a diverse bottom dwelling macroinvertebrate species and those species were spreading beyond the specific study areas, so recovery of Ward Cove is expected to continue.

However the 2004 report went on to say that “the achievement of stable benthic biological communities with balanced species composition in more than 75 percent of the area with documented coverage by wood residues on the bottom of Ward Cove” would happen within 40 years from the 2004 study.

The next review of Ward Cove is slated for August 2015.

 

Sand capping
Diagram of a sand capping operation from a barge. (US Army Corps of Engineers)

 

Diagram of a sediment capping operation knowing as diffusion (US Army Corps of Engineers)
Diagram of a sediment capping operation knowing as diffusion (US Army Corps of Engineers)

 

 

Termie
Diagram of a Japanese system called tremie that uses a hose system to deposit capping material on the seabed. (US Army Corps of Engineers)

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Clio Bay: What happens to sunken logs?

Special report: Clio Bay cleanup: Controversial, complicated and costly

Logs at Clio Bay
Floating logs at Clio Bay, September 14, 2013. (Robin Rowland/Northwest Coast Energy News)

The forest industry has been operating on the Pacific coast from Oregon to Alaska for more than a century. Over that time, it is likely that millions of logs from booms and other operations have sunk to the bottom of bays, cove, estuaries and inlets along the coast.

During that century, scientists in both Canada and the United States have been studying the effects of the those sunken logs on the sea bottom. It is only in recent years that the cumulative effect of all those logs has become an environmental concern.

As well as logs on the sea bottom, ranging, depending on location, from a couple of hundred to the tens of thousands of logs, there are wood chips, wood fibre and discarded log parts and bark. Often metal cables, bolts, ropes, and other manufactured material either dropped accidentally or deliberately discarded are also found among the old logs, further contaminating the seabed. Compounding the problem of the sea bottom is organic material that would occur naturally on the seabed, including tree trunks, roots, branches, conifer needles, deciduous leaves and other material from terrestrial plants.

Anyone who sails Douglas Channel after a storm can see with all the floating tree trunks in the Channe. That means that storms and spring run off ads debris to the natural pile up of old logs and debris. At logging sites, this natural material, brought in by creeks and rivers, piles up on the already sunken logs.

Over the years, depending on the salinity, teredos, more popularly known as ship worms  eat the wood, often leaving a tube of bark that eventually collapses. The rotting wood, bark and other material is often, depending on conditions, pounded into fragments by the action of waves, currents and outflow from rivers. Some species of teredo can live in brackish water, but since teredos are not a fresh water species, that means that logs in fresh or mostly fresh water last longer.

A DFO report on sunken log sites on Douglas Channel, published in 2000, noted:

very few comprehensive, quantitative field studies describing the effects of wood and bark have been published and those that did focused on log handling and storage sites which handled high volumes of more than one million cubic metres.

The DFO report said that thick bark and wood debris deposits resulting from log handling can cause substantial, long-term negative impacts to benthic (sea bottom) ecosystems. Under the worst conditions, the cumulative debris can deprive an area of oxygen and, according to DFO, “virtually eliminate aerobic” sea bottom animal life.

The report noted that studies had shown that “negative biological impacts were localized,” but added that “the cumulative effect of several hundred sites located on the B.C. coast is currently unknown.”

Studying the problem has been a low priority for DFO and other agencies and that meant a limited budget and few studies. Other problems is that, according to the DFO, parts of BC fjords are steep and “much of the likely impacted habitat is beyond diver range.” There is also pressure to study the effect on “economically or socially important species.” Although the use of remotely operated vehicles has increased since the 2000 report, using an ROV can also be a budget buster for a low priority project.

As the ready timber supply in British Columbia particularly old growth forest declined in the last part of the twentieth century, the DFO report says “forest companies have harvested areas where access is more difficult and cut-blocks are smaller.” That meant many smaller dump sites were developed that were used for only one to five years. Plans for log handling at the time, DFO said, were evolving to ensure ensure that fisheries resources and overall fish production capability were not adversely affected by development of log handling facilities and planning was focused on ensuring that sites for log handling facilities did “not have sensitive fish habitats or fisheries resources (such as eel grass beds or shellfish resources) which may be affected by the log handling,”

One of the reasons for the disagreements over Clio Bay is that while some people call it “dead” saying there are no halibut and fewer cod, others say that Clio Bay is very much alive, pointing out that it is easy to catch crab and rock cod.

The studies that have looked at life on the bottom of log dumps sites have shown that it can be highly variable even within one bay or cove, with many factors creating small local ecosystems, including depth, nature of the sea bottom, for example sand, mud, clay or a mixture, whether or not the sea bottom sediment is “enriched,” the flow of currents, fresh water flow into the site, the percentage of wood on the bottom, the percentage of bark on the bottom, whether the wood and/or bark debris is “continuous’ or “discontinuous,” whether or not the seabed is contaminated as was the case with the cleanup of pulp mill sites at Ward Cove and Sitka, Alaska.

Ward Cove had been so polluted for decades by pulp mill effluent that it was eligible for US Superfund clean up funding and was estimated to hold 16,000 sunken logs. At the same time, an EPA report on Ward Cove noted that at the point Ward Creek emptied into Ward Cove was “a popular sport fishing location during salmon season, including commercially guided fishing. Some sport fishing and personal-use crab pot fishing has taken place in the past and may continue in the waters of the cove.” At the same time of the cleanup, the EPA identified that the degradation of Ward Cove put at risk eight species of salmon, 75 “non-salmonid esturine and marine fish species and benthic invertebrate fauna.”  (The EPA says Ward Cove is recovering after the reclamation and fishing is continuing)

In other words, those say Clio Bay is in danger and those who say Clio Bay is a rich source of life are likely both right.

For example, while Chris Picard’s (then with the University of Victoria, now with the Gitga’at First Nation) study of Clio Bay said: “Dungeness crabs were observed five times more often in the unimpacted Eagle Bay than in Clio Bay,” and tied that to log dumping and low oxygen.
Picard’s study noted that both Dungeness crabs and sunflower seastars, while more abundant in Eagle Bay, in Clio Bay “both species were several-fold less abundant in wood-dominated habitats in Clio Bay than in non-wood habitats in that bay.”

Several people have pointed out that since Clio Bay is one of the closest crabbing spots to both Kitimat and Kitamaat Village, while Eagle Bay is further down Douglas Channel, overfishing at Clio may be a factor in the reported species decline.

The DFO study noted

The dumping of logs into water down skids can result in the generation of a considerable amount of bark and wood debris. The abrasive action of boom boats and waves during the sorting and storage of bundles can also generate quantities of wood debris. Bark and wood lost during dumping often forms thick, continuous, anoxic fibre mats extended from the base of the dump skids. The debris mat tends to dissipate with distance from the entry point; however, wood debris can often be observed substantial.” distances from the dump skids as seen at all four of the sites sampled. Debris deposits can also be generated as logs resting on the sea floor decay. Wood boring organisms (e.g., Toredo) quickly reduce the wood fibre content of logs, but the bark of some species (e.g., western red cedar (Thuja plicata) which has a high lignin content) is left relatively untouched. The amount of wood debris generated during handling and storage can be different depending on tree species, tidal levels, and dumping methods. Debris accumulation, distribution, and the resulting biological impacts are affected by physical factors including depth, sea floor slope, dump site aspect, water currents, and wind or wave exposure.

One of the main problems with log dumping is that it has the potential to deplete vital oxygen, especially at deeper levels. Seasonal variations can mean that, even if there are thousands of logs at the bottom, the levels of dissolved oxygen can vary. Years of studies at the cleanup site at Ward Cove, Alaska showed how the oxygen levels can vary by season. In Minette Bay, near Kitimat, a DFO study showed that the Minette is somewhat stagnant and therefore has naturally occurring low oxygen levels, but also that the low levels usually last from May to November and are worst in July.

The DFO study went on to say that oxygen poor thick anoxic bark or wood fibre deposits are likely to cause damage to bottom dwelling species, although in the short term, logs may not cause any impacts. It says that some studies have indicated that large pieces of wood debris can, for a time, increase diversity by providing suitable base for some filter feeders as well as food and cover for epifauna and wood boring organisms. Several species not normally found in sand-bed have occasionally been found in log and rock debris.

(Studies have shown that salmon the ability to detect low oxygen areas and avoid them and some active  invertebrate species can migrate away from a low oxygen area.)

In the long term, logs do decay and the wood and bark left behind can contribute to the wood debris accumulation. One study cited by the DFO survey of Douglas Channel found found that crabs avoided bark deposits when given a choice but when they were forced to live among bark deposits, they were had fewer offspring, had lower feeding rates, and had a decreased survivorship.

One theory is that the decaying organic material produces hydrogen sulphide in combination with ammonia and other unmeasured toxicants. One study of Dungeness crabs, living at a log dump in southeast Alaska with elevated hydrogen sulphide and ammonia concentrations in the bark debris, shows the colony had less than half as many reproducing females as a control population.

The EPA and Alaska reports from Ward Cove show that sand capping does help restore the seabed environment.
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Clio Bay: DFO declines invitation to appear before Kitimat Council

Special report: Clio Bay cleanup: Controversial, complicated and costly

DFO logoThe Department of Fisheries and Oceans has declined an invitation from District of Kitimat Council to appear at a special meeting on Monday, September 30 to discuss the Clio Bay remediation project.  A representative of Chevron will be in the council chambers at the Kitimat branch of Northwest Community College to make a presentation and answer questions.

The letter from DFO to the council  from Dave Pehl works at DFO office in Kamloops says:

Thank you for the invitation to attend District of Kitimat Council meeting on September 30, 2013 to address plans by Chevron Canada and Apache Canada(Kitimat LNG) to remediate habitat conditions in Clio Bay. Regretfully, Fisheries and Oceans Canada (DFO) is unable to attend the scheduled council meeting.

Fisheries and Oceans Canada has reviewed a proposal to dispose of soil materials, generated at the Kitimat LNG plant, in Clio Bay, Clio Bay has been used as a log handling site for decades which has resulted in areas of degraded habitat from accumulations of woody debris materials on the sea floor. The project intends to cap impacted areas with inert materials and restore soft substrate seafloor. The remediation of the seafloor is predicted to enhance natural biodiverstiy and improve the productivity of the local fishery for Dungeness crab. The project area does support a variety of life that will be impact and therefore the project will require authorization from Fisheries and Oceans Canada for the Harmful Alteration, Disruption or Destruction (HADD) of fish and fish habitat.

Mapping of the seafloor in Clio Bay has been completed and the project plans prioritizes capping on areas of dense woody debris, followed by areas of soft substrate with woody debris distributed throughout. Mapped areas that are avoided include hard substrates and sensitive habitats such as freshwater streams and eelgrass beds. Buffers have been allocated around sensitive areas and no capping will be conducted in areas of less 10m in depth. Proposed mitigation to avoid potential impacts to areas outside Clio Bay includes avoiding deposition of material within 500m of the confluence of Clio Bay and kitimat Arm. Some areas of degraded or partially degraded habitat will not be capped to serve as reference areas.

Chevron will be required to conduct a pre-construction, construction and post construction monitoring program. Pre-construction monitoring will include collection of baseline information that will be used to assess effectiveness monitoring during and at the completion of the project. Water quality monitoring for turbidity and total suspended solids will be undertaken during construction to determine if established performance criteria are met. The monitoring plan for the project will evaluate

1. Water quality near the sea floor.
2. Fish habitat quality and quantity
3. Biodiversity of the seafloor ecosystem and
4. Distribution of a fishery resource (Dungeness crab)

Reference sites will be used to make comparison between capped and uncapped habitats. Monitoring will continue for a period of five years following the completion of the works. The proponent will be required to report the follow-up monitoring program to DFO in years 1,3 and 5 following construction.

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Clio Bay Editorial:Hire the experts. This is not the time to be learning on the job

Special report: Clio Bay cleanup: Controversial, complicated and costly

Editorial:

Hire the experts. This is not the time to be learning on the job.

Everyone in the Kitimat and Kitamaat Village are facing a dilemma, a dilemma that should have been solved a year ago, when it was first known that the KM LNG project at Bish Cove had grossly underestimated the amount of marine clay and other material that has to be removed for the liquified natural gas terminal, a total of about 3.5 million metric tonnes.

The Haisla and Chevron are proposing that much of the clay be deposited over sunken logs in Clio Bay.

Chevron, which only took over operations at KM LNG in December 2012, is still learning on the job.

When the Clio Bay capping plan became public, far too late in the process, only then did Chevron begin to take a serious look public worries about the environmental problems that might result from depositing all that marine clay in Clio Bay.

Chevron hired Stantec, a well-known international  consulting firm with close ties to the energy industry and some experience in remediation to evaluate Clio Bay. Although Chevron said in a statement that Stantec is a company  “with extensive experience in many major habitat restoration projects,” it appears that Stantec, in the case of Clio Bay, is a jack of all environmental trades and master of none, just learning on the job.

In answer to questions by Northwest Coast Energy News, Chevron cited two studies supplied to them by Stantec. One was Chris Picard’s (now with the Gitga’at First Nation) study of Clio Bay which anyone can find by using a Google Search. The second was an overview chapter of west coast North American logging practices from a book published 22 years ago.

Any of the web saavy undergraduate journalism students I once taught at Ryerson University could have done better. This semi-retired reporter, without the resources he once had in a major newsroom, easily found the studies of the log filled Ward Cove, the State of Alaska’s recommended remediation practices, the capping procedures recommended by the US Army Corps of Engineers and more. Chevron did not mention Stantec citing the 1995 DFO study of nearby Minette Bay which can easily be found on the DFO website.

A letter from Fisheries and Oceans to District of Kitimat Council only mentions Dungeness crab and not the Haisla desire to restore halibut and cod to Clio Bay. That can only raise suspicions that the DFO is also depending solely on Chris Picard’s limited survey of Clio Bay.

In Alaska, at Ward Cove, there were almost five years of studies on the ocean environment before part of the cove was dredged and parts of the cove with thousands of logs there were capped with fine sand.

The people of Kitimat and Kitamaat want the LNG project to proceed. Everyone wants a clean and sustainable ocean enviroment, whether in Clio Bay, Minette Bay or down Douglas Channel. The problem of that 3.5 million cubic metres of marine clay must be handled in a timely fashion so the LNG terminal can move to the next step in the coming months. There is no time for five years of studies before proceeding.

This site would not normally endorse one large corporation over another.

There isn’t time for Chevron and Stantec to be learning on the job, its technicians racing in their boats between Clio Bay and Bish Cove trying to figure out what is going on and casually asking people what they think. No time at all.

The clock is ticking. Chevron and Apache, in partnership with both the Haisla and the District of Kitimat, should immediately hire the companies that do have the expertise in remediating a northwest Pacific coast bay filled with sunken logs, the companies that cleaned up Ward Cove in Alaska. Integral Consulting was the main environmental consulting contractor at Ward Cove, assisted by another large firm, Exponent  and by Germano and Associates, a company that  according to its website specializes in “rapid seafloor reconnaissance”. Both Integral and Exponent are, like Stantec, giant international consulting firms.  In this case, experience has to count. While Stantec’s website does list remediation projects, none are similar to Clio Bay.

A letter from Fisheries and Oceans to the District of Kitimat says that:

Chevron will be required to conduct a pre-construction, construction and post construction monitoring program. Pre-construction monitoring will include collection of baseline information that will be used to assess effectiveness monitoring during and at the completion of the project. Water quality monitoring for turbidity and total suspended solids will be undertaken during construction to determine if established performance criteria are met.

From the reports available from both the EPA and the State of Alaska it appears that the companies that cleaned up Ward Cove did just what DFO is asking, assess and monitor.  Another reason to hire the experts rather than the newbies.

Why a three way partnership? Chevron/Apache and the Haisla Nation are already partners in the Clio Bay plan. Adding the District of Kitimat would establish trust and make sure that the results of any scientific and engineering studies, plans and operations would be available to the people of Kitimat (as well as some Haisla members who feel they were excluded) as part of the ongoing process. The partnership would make up for the lack of transparency up until now, make sure the public is kept up-to-date and not just by Chevron’s and DFO’s communications people since reports to the District could be reviewed by the engineering staff and members of council.

It is likely that those companies that worked at Ward Cove could quickly let everyone know whether the idea of capping at Clio Bay with marine clay is a viable option and if it is viable how to do it properly rather than just dumping the clay from a barge using a hose. If marine clay is not viable for Clio Bay, it is likely that those firms could advise whether one of the original plans, to dump the clay in the deep ocean, is a better solution, or if there is another alternative that no one has thought of.

Kitimat and Kitamaat are lucky. The recommended practice for capping sunken logs is using sand. There is here a ready source at the Kitimat Sand Hill. If marine clay is not a viable option, or for future projects, the Sand Hill can easily be used to fulfill the aims of both the Haisla Nation and the residents of Kitimat to clean up Clio Bay, Minette Bay and eventually all 50 other sites identified along Douglas Channel by DFO in 1997. Those consulting firms have the expertise in this area and that expertise should be utilized.

Learning from the job

Even though sand has a track a record in capping, using marine clay from Bish Cove  to cap the logs at Clio Bay is probably a good idea, after all that marine clay was once at the bottom of the Ice Age Douglas Channel.

The use of sand for capping sites is well-known, there are established engineering parameters. At Ward Cove, there were studies of the angle of the slopes and how much weight of sand that the debris could hold.  Sand is very different from marine clay. At the moment, there are no engineering parameters for marine clay. It appears that no one has thought of doing slope analysis and load bearing engineering studies at Clio Bay.

Marine clay is a potential cap for all the sunken log sites on Douglas Channel and on the whole Pacific coast from Oregon to Alaska.  That means that Clio Bay is a pilot project that should be planned as carefully as possible, within the time constraints needed for construction of the LNG terminal, but not regarded as a rush job to get rid of that clay.  That means taking the time needed to do all the necessary scientific and engineering studies before the first drop of clay heads to the bottom. That is another reason to hire experts who actually know what they are doing so everyone can learn from the job.

 

Standards

No matter how the cleanup of Clio Bay proceeds, KM LNG, the Haisla and the District of Kitimat are facing another dilemma. What standards and benchmarks should be applied to the project?

By law, the Department of Fisheries and Oceans is responsible and will, of course, be monitoring the cleanup.

Despite assurances in a letter to the District of Kitimat, it is clear that DFO too is learning on the job.

At the moment, DFO has no standards for remediation, because the Conservative omnibus bills have gutted environmental standards in Canada. Even before the omnibus bills and the LNG rush, cleaning up log dumps was on the DFO low low priority list.

The letter from DFO to District of Kitimat council shows what knowledgeable sources have told us, DFO will be navigating Clio Bay from a desk in Kamloops (of all places). The same sources say that the Prince Rupert office of DFO, which has the expertise on the northwest coast is out of the loop on this project. The residents of the northwest coast already know there are not enough fisheries officers to properly monitor the coast. DFO “estimates” the annual recreational halibut catch (perhaps by using fish entrails rather than the traditional chicken?). DFO has retired or laid off many scientists who have studied the coast. Others have left on their own. The remaining scientists are muzzled by the Harper government, with anything they could say filtered by the Prime Minister’s Office, so it is likely that no one in the northwest will actually trust what they say.

Normally in a free and democratic society, the government tells local residents when a major operation like the remediation of Clio Bay is going to occur.  In this case, Fisheries and Oceans did not tell anyone in Kitimat anything until the District of Kitimat Council requested information.

On Monday, Sept. 30, a representative of Chevron will make a presentation to District Council. DFO did nothing more than send a letter that said: “Regretfully, Fisheries and Oceans Canada is unable to attend the scheduled council meeting.” Nobody, in the whole department? One is tempted to say, “That’s not good enough.” Then you remember that if DFO appeared before Council, the presenter would have to face possibly awkward questions from both members of Council and the media. That just doesn’t happen in Stephen Harper’s Canada, not in Ottawa and certainly not in Kitimat.

Despite what DFO has said in its letter, this regulatory vacuum leaves the Kitimat region no choice. Since Canada has no standards, when the Clio Bay project proceeds, the best available standards are those set by Alaska, which has the same type of coast and climate. The Clio Bay clean up should therefore be measured against those Alaska standards.
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