Robin Rowland | Northwest Coast Energy News

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

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

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, 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

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)

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

The 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: Chevron statement

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

Here is the text of a statement Chevron spokesperson Gillian Robinson Riddell sent to Northwest Coast Energy News

The Clio Bay Restoration Project proposed by Chevron, is planned to get underway sometime in early 2014. The proposal is fully supported by the Federal Department of Fisheries and Oceans and the Haisla First Nation Council. The project has been put forward as the best option for removal of the marine clay that is being excavated from the Kitimat LNG site at Bish Cove. Chevron hired Stantec, an independent engineering and environmental consulting firm with extensive experience in many major habitat restoration projects that involve public safety and environmental conservation. The Haisla, along with Stantec’s local marine biologists, identified Clio Bay as a site that has undergone significant environmental degradation over years of accumulation of underwater wood debris caused by historic log-booming operations. The proposal put forward by the marine biologists was that restoration of the marine ecosystem in the Bay could be achieved if marine clay from Chevron’s facility site, was used to cover the woody debris at the bottom of the Bay. The process outlined by the project proposal is designed to restore the Clio Bay seafloor to its original soft substrate that could sustain a recovery of biological diversity.

In preparing this restoration project proposal for Chevron, Stantec conducted independent field studies carried out by their own marine biologists who are registered with BC College of Applied Biology. Two of the studies used in the development of the proposed project were previously published scientific studies on the effects of log-boom activity and log boom activity in Clio Bay that determined log boom and storage activity has had a negative impact on marine diversity. There are previous case studies where capping activity has been used in marine environments.

Stantec’s, and previous studies, have determined that Clio Bay has changed from a once highly productive marine bay characterized by plentiful predatory species such as Dungeness Crab and sunflower stars to a less productive environment hosting more opportunistic and resilient species such as squat lobster and sea anemones. One such study found that compared to Eagle Bay, which has not been affected by logging activity had five times the Dungeness Crab population of Clio Bay. Independent studies conducted before Chevron began working at Bish Cove found that if Clio Bay is left in its current degraded condition, the woody debris will continue to foster and abnormal, species-deficient habitat for several decades. Extensive fieldwork carried out by Stantec’s marine biologists used SCUBA and Remote Operated Vehicle surveys to observe and record all flora and fauna in the bay and its levels of abundance. Stantec’s observations echoed the previous studies which determined that the massive amount of wood has harmed Clio Bay’s habitat and ecosystem.

Most importantly, when considering the work Chevron is proposing to carry out in Clio Bay, it is important to note that a primary objective of all Chevron’s operations is to protect people and the environment. A good example of how we have done that on other projects can be seen in the construction of Chevron’s Gorgon LNG plant in Australia on Barrow Island, which is a Class A nature reserve. Although identified as one of the most important wildlife refuges in the world, and the site was chosen only after a thorough assessment of the viability of other potential locations, and after the implementation of extensive mitigation measures, including a vigorous quarantine program for all equipment and materials brought on to the Barrow island site to prevent the introduction of potentially harmful alien species. Those same high environmental standards are being applied to the Kitimat LNG project and the proposed Clio Bay Restoration project. The proposed work would be carried out with a stringent DFO approved operational plan in place and would be overseen by qualified environmental specialists on-site.

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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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Clio Bay: Links and Documents

Links and documents relating to sunken logs and site remediation

Note many, not all, external links are to pdf files.

Canada

DFO study of sunken log sites in Douglas Channel

DFO Study Dissolved oxygen cycle in Minette Bay

Impact of Wood debris in British Columbia estuaries

Chris Picard’s study of Clio and Eagle Bays as posted on the University of Laval website

United States

Links

Alaska Department of Environmental Conservation

Environmental Protection Agency

Ketchikan Paper Company
This is the EPA Web site on the Ward Cove cleanup and remediation with numerous documents.

EPA capping guidance
EPA contaminated sediment capping guidance

US Army Corps of Engineers

US Army Corps of Engineers capping guidance

Documents

Alaska log site remediation guide (pdf)

EPA study of dissolved oxygen in Ward Cove (pdf)

Marine Log Transfer Facilities and Wood Waste (pdf)

Academic paper by Ward Cove consultants Geramano & Associates on sediments in Ward Cove and Thorne Bay, Alaska.

Ward Cove Sediment Remediation Project Revisited

Academic paper by Ward Cove consultants Integral Consulting

Other Links

Kitimat LNG (KM LNG)

Stantec

Stantec remediation project page

Integral Consulting

Integral Consulting Ward Cove web page

Exponent

Exponent Ward Cove web page

Exponent LNG Safety web page

Germano & Associates

(Note not all documents used in this report are available online. Some sent to NWCEN are too large to upload)

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Chevron announces open house on Clio Bay, seeks input from stakeholders

Updates with open house location

Chevron, the partner with Apache in the KM LNG (also known as Kitimat LNG) project at Bish Cove, said Sunday that the company will hold an open house in Kitimat on the controversial Clio Bay reclamation project.

Chevron says there will be a public open house at Riverlodge Tuesday, October 8 from 4 pm to 8 pm.

In an e-mail to politicians and local groups, including Douglas Channel Watch, Marc Douglas, a senior advisor for Chevron, based in Calgary, invited local stakeholders for a series of one hour meetings the same day at the KM LNG offices in City Centre.

Chevron Canada invites you to a meeting to discuss the Clio Bay Marine Life Restoration Project.
This proposed project would see Chevron excavate marine clay from the Kitimat LNG construction site at Bish Cove and work closely with the Federal Department of Fisheries and Oceans to deposit this natural material in specific locations in Clio Bay. The clay will cap-off decaying wood debris left by historic log booming operations that has accumulated on the bottom of Clio Bay, damaging the Bay’s natural ecosystem. A key goal of the project is to restore natural marine life populations in Clio Bay. Come and share your thoughts and ideas with us and learn more about this innovative restoration project.

There has been growing controversy over the Clio Bay project in recent weeks. Members of the Haisla Nation and residents of Kitimat were initially told that due to the large number of sunken logs at Clio Bay, that the area was deprived of oxygen, with limited sealife and that capping the logs with clay from Bish Cove would restore the ecosystem. However, beginning with a discussion at District of Kitimat Council on September 3, more people have been challenging the idea that Clio Bay needs restoration, with fishers posting photographs of recent catches on Facebook pages.

On Sept.3, Councillor Phil Germuth told Council: “Those logs have actually created a woody reef, where like any other reef, an ecosystem is being sustained. So to say that those logs are suffocating the life out of Clio Bay doesn’t seem to have a lot of merit.”

At the time, Chevron told the media that they had consulted with the Department of Fisheries and Oceans and concluded that carefully placed clay would improve the ecosystem.

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

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Has Enbridge “moved to the dark side?”

So far, Enbridge’s public and community relations efforts on issues like Northern Gateway and Kalamazoo, have for, the most part, been a disaster. In BC, since the Joint Review hearings wrapped in June, Enbridge has been on a full out campaign to convince British Columbians to support Northern Gateway.

Now, at least to me and my geeky sense of humour, it appears, that Enbridge has another PR fiasco in the making.

A few minutes ago, as I was scanning my Tweetdeck feed, a Tweet from Enbridge popped up. Given that the default background for Tweetdeck is black, I thought, that Enbridge logo looks very dark.

Now since I’ve been monitoring Enbridge tweets since I started this site, normally the company logo is white and stands out against the black of the Tweetdeck feed.

Is it a mistake I wondered?

Or is it a new logo and therefore has Enbridge, I wondered, “moved to the dark side?”

So I checked the company webpage. It’s a new logo and new web design. In the lead picture, the old logo is clearly visible under the new logo on top.

For the record here is the new logo and the old one.

So I can’t resist reporting, Enbridge has moved to the dark side. 🙂