Showing posts with label powerhouse. Show all posts
Showing posts with label powerhouse. Show all posts

Logan Martin Dam near Alpine, AL

(Satellite)

Photo from TooneCycling
[It amazes me that fish can go through the pentstock, scroll and turbine and still have enough energy to feed off a fisherman's line. Or does the turbulence attract fish from downstream?]
Fishing and Boating Safety Tips
Steve Robinson posted ten photos with the comment:
Alabama-Logan Martin Dam
Construction of Logan Martin Dam began in 1960 and quickly took on the monumental scale of an ancient wonder. Photos from Alabama Power’s Archive show hard-hatted workers dwarfed by gigantic intake pipes and turbine housings. Against the dam’s massive flanking earthworks, trucks and cranes seem like toys in a sandbox. Even a half-century later, these images can inspire awe at what it took to tame a river and turn pent-up water into electricity.
An annual festival and boat show at Pell City’s Lakeside Park. Named for former Alabama Attorney General Logan Martin (brother of longtime Alabama Power President Thomas Martin, for whom Lake Martin is named), the dam created a 48.5-mile-long reservoir 460 feet above sea level (465 in summer), with 275 miles of shoreline and an area of 15,263 acres. The dam is 459 river miles above Mobile. Its concrete section, longer than two football fields [612 feet], houses three turbines powering AC generators that produce more than 400 million kilowatt-hours per year.
Beyond hydropower, the dam provides flood control, economic development, irrigation and drinking water, fish and wildlife habitat, and recreation. Flowing under the Interstate 20 bridge east of Pell City, the lake is a liquid interlude on the drive between Birmingham and Atlanta.
Motorists crossing that causeway have been known to feel a pang of envy at the sight of a fast-moving water-skier or a fisherman angling for bass.
Logan Martin was part of the second great phase of hydroelectric dam-building in Alabama. The first era, starting with Lay Dam (completed in 1914) and ending with Thurlow Dam (1930), gave us Lay, Jordan, Mitchell, and Martin lakes, among others. But after the early dams were built on the Coosa and Tallapoosa rivers, the Great Depression and World War II intervened.
The damming of the entire Coosa River had long been envisioned (in the 1870s, the first of many surveys authorized by Congress recommended no less than 34 dams and locks for the river). Finally, in June 1954, President Eisenhower signed into law legislation the U.S. House and Senate had approved almost unanimously, authorizing the transformation of the upper Coosa as proposed by Alabama Power. Logan Martin Dam was the second dam built under the project, which included the construction of Weiss, Henry, and Bouldin dams and the redevelopment of Lay Dam to increase its generating capacity.
A half-century is a long time, but older locals remember what the area was like before the waters rose. “I had family here and came here as a boy,” said Mike Riley, president of the Logan Martin Lake Protection Association. “This was a largely rural, agricultural community. The Coosa was a fast-moving river, not something you’d just jump into.”
It had flooded for generations, as noted by Native Americans who lived on the Coosa and observed that every 15 or 20 years the Coosa “overflow[s] the banks, and spreads itself for five and six miles in width.” [From “Rivers of History” by Harvey Jackson, p.2]
To clear the way for the lake, Alabama Power had to compensate people for property, cut down thousands of trees, and relocate more than 2,000 graves. The lake inundated the village of Easonville, established in 1821.
“I was a teenager when the lake came,” said Pell City resident Vicki Davis Mize. “We lived in Easonville, on what is now Harmons Island. My mother’s store was covered by the water but my father’s church was moved to higher ground.” This structure, Coosa Valley Baptist Church, now stands beside Highway 231.
“A lot of us were very sad to lose our homes,” Mize said. “But farmers who were struggling were better off after selling land to the power company.”
“From a P.R. standpoint, Logan Martin was a much easier sell than the earlier lakes,” said Harvey Jackson, a professor emeritus of history at Jacksonville State University who has written extensively on Alabama waterways. “By then, Alabama Power knew how to hash out the problems. People knew lakefront property was valuable and the lake benefited from its proximity to Birmingham. Because of the dams, the Coosa today is really more of an elongated lake than a river. They were built for electricity but have turned out to be one of the greatest recreational assets the state has.”
Pell City resident Carol Pappas has lived on Logan Martin for about 30 years. “The lake had the effect of growing the surrounding towns — Pell City, Talladega, Lincoln, Riverside, and others — and improving the local economy and housing. We have a lot of people in Georgia with lake homes here,” she said.
“I never pitched the community without highlighting the lake,” noted former Pell City Mayor Guin Robinson. “I can’t tell you how many lake cruises we’ve had with visitors thinking of relocating. You’re not just relocating a business, you’re moving families.”
Robinson and others say the higher quality of life and lower electrical rates fostered by the lake and dam helped attract the Honda plant to Lincoln. “People recognize that the town and the region would not be what they are today without Lake Logan Martin,” he said.
Pappas agrees. “The quality of life of lakeside living is extremely positive — it’s like being on vacation all the time.”
“If you’ve spent time on a lake, you know it’s therapy,” Robinson said. “It has a way of calling you home.”

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What struck me about this dam is the height of the Tainter gates. They are about half the height of the dam itself.

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NYC water supply: Cannonsville Dam sprung a leak

(Satellite, the spillway is a text book example of a tumble bay)

Cannonsville Dam is the westernmost dam in NYC's water supply, and it captures water from the Delaware River, which flows through Trenton, NJ and Philadelphia, PA. "Placed into service in 1964, Cannonsville Reservoir was the last of New York City’s 19 reservoirs to be built. Water diverted from Cannonsville Reservoir for drinking water enters the West Delaware Tunnel and travels 44 miles to the upper end of Rondout Reservoir. From there, it is carried in the 85-mile-long Delaware Aqueduct. Water is released downstream from Cannonsville Reservoir under the terms of the 1954 U.S. Supreme Court Decree, and a flow program, known as the Flexible Flow Management Program, agreed upon by New York City and the states of Delaware, New Jersey, New York and Pennsylvania. All other reservoirs in the city’s Delaware System have continued to meet their downstream release requirements under the Flexible Flow Management Program while the condition at Cannonsville is repaired."  [Aug 2] It holds an eighth of the system's water supply. [NYtimes]

Cannonsville Public Meeting, page 3
New York City Department of Environmental Protection
It is a 175' tall earthen dam that can store 95.6 billion gallons with a two-stage emergency spillway that is 800' long.

(When this photo was taken, I wonder if the river release was kept low to deliberately fill the reservoir to test the spillway or if there was a spring season wet enough to cause the overflow.)

Cannonsville Public Meeting, page 4
If I'm reading the diagram below correctly, water will start going over the spillway at an elevation of 1150'; and, at the maximum expected spillway flow, the water level would be 1155'. So the water should remain 20' below the height of the dam.

Cannonsville Public Meeting, page 5
Soil sample bore holes were drilled as part of a study to build a 14Mw power plant next to the existing release chamber. (It is interesting that the above diagram of the dam doesn't include the intake for, and location of, the discharge pipe to runs to the release chamber. This pipe the normal way of releasing water so that the reservoir level should seldom reach the emergency spillway.)

Cannonsville Public Meeting, page 8
If you look at the dam diagram, you see by the "Assumed rock surface" graphic that they don't even know where the bedrock is for this dam. It is built on glacial till. So before they build the hydro-power plant, they need to understand what type of soil+rock mixture is under it so that they can design the pilings needed for the foundation. They do this by boring holes to sample what is underneath. One of the holes created an artisan spring under the rock drainage at the tow of the dam. What I can't tell is if that was expected and they normally then plug the rock drainage with Bentonite or if this spring was a surprise and their efforts to plug it with Bentonite failed. Now they have Bentonite and bore hole material flowing with the water through the rock and into the river.

Cannonsville Public Meeting, page 10
Evidently the booboo was on July 8 and the presentation to the public was July 23. While they are working on repairs, they have maximized the release to the NYC water supply at 970 MGD and maximized the river diversion at 470 MGD. They are also "stockpiling materials and equipment for emergency on-call repairs." [Cannonsville Public Meeting] This is lowering the water level about 8 or 9 inches a day. It has raised the Delaware River about a foot and reduced the water temperature, which is good for the trout. [WaterShedPost]
They have also released the inundation map to the public even though it is marked "FOR OFFICIAL USE ONLY - NOT FOR DISTRIBUTION." This map indicates the impact of the worse case scenario of a breech with a full reservoir. It is not surprising that the whole town of Deposit would be under water. It is surprising that several blocks and bridges in Philadelphia would also be under water.

The photo below shows the water turbulence in the release chamber caused by the maximum release flow and the turbid water to the left caused by the aquifer puncture by the boring hole. You can see a relief-well drilling rig on the upstream side of the road at the base of the dam.

The repair has two stages. The first is to drill relief wells upstream with proper screens and casings so that clean water will flow through the rock embankment. These clean holes will relieve the pressure on the dirty holes and stop the release of sediment into the river. The second stage is to grout the soil sample holes and then drill grout holes around the dirty holes to create a grout curtain with pressurized grout. [July 23]

nyc.gov Flickr

nyc.gov Flickr
One of the two rigs drilling the relief wells.
By July 29, a sediment analysis was complete. It determined that the sediments are coming from the bore hole site and not from the dam. When the first relief well started flowing, the turbidity in the river was reduced. So the relief plan was working. "Engineers are prepared to install as many as 8-10 relief wells, but they expect it may take fewer to end the turbid discharge." [July 29]

Four relief wells were enough to stop the turbid flow, and outflow rates started to shift to normal rates on July 29. In this case, normal was zero for drinking water because they switched to other reservoirs for drinking water to reduce the rate this reservoir was being drained. The river flow was reduced from 1500cfs to 500cfs between Aug 2 and Aug 5 per the advice of fisheries biologists. Inflow was 300cfs. At the time of the July 23 presentation, the water level was 1141.97' with 47.2 billion gallons of warm water and 37.5 BG of cold water. As of Aug 2, 25 BG of cold water remained. (I never found information on how much warm water was left. Nor if the water intake has inlets at different levels to control the temperature of the water that is released.) [Aug 2]

The second stage of repairs was finished Aug 21. Now they will gradually close the relief wells and verify that the dam's instrumentation shows values returning to levels comparable to what they were before the test bore holes were drilled. [Aug 26]

After two weeks of monitoring the instrumentation and the flow in the river, the repairs have been declared successful. The reservoir is expected to fill to normal capacity by late Spring, 2019. [Sep 17]

nyc.gov Flickr
"This photo shows the cloudy discharge downstream of the dam just a few days after it was discovered."
[It also shows the turbulence in the release chamber with a high release rate. In hindsight, the dam was not in danger and they did not need to release the water. But it makes sense that when there is a sign of trouble that they would drain first and think second. Nonetheless, it did take a week before they decided to start draining the reservoir even though it was close to capacity because of a wet June. [NYtimes]]

nyc.gov Flickr
"This photo shows the cloudy discharge after one relief well was installed and pumping. The discharge was reduced, but some remained along the grass and the stone abutment near the middle of the photo."

nyc.gov Flickr
"This photo shows the same area downstream of the dam on Aug. 7, after the cloudy discharge was successfully halted by the relief wells. Notice the water is so clear that rocks on the river bottom can be seen easily."
The 14MW ($2M per year) capacity of the proposed hydro-power plant is impressively small. Modern coal plants and nuclear plants are over 1000MW. 14MW is just a few windmills in a windmill farm. At an estimated cost of $72M, it was estimated that it would barely pay for itself assuming a 50-year lifespan. After this repair bill, it strikes me as a looser because of the risk of building a foundation over a pressurized aquifer.

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WE Energies Dam on Pine River and Hydro Dams

(Satellite)  Note the long inlet channel to the powerhouse penstocks. It must have been rainy because the dam is spilling a lot more water than is going through the powerhouse.

Doug Kearney posted three photos with the comment:
Grove RT875E working on the Pine river dam for WE Energies in Florence, WI. A lot goes into setting it up. They had to haul the barge sections down the hill, launch them, then roll the crane on board. You can see the ramps on far shore. Driving the crane down the hill was probably a bit of an adventure.
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"Near Florence" is relative. It struck me as being rather far away until I saw how few towns were in the area. I noticed that there are some bigger, closer powerhouses. And they also are spilling a lot of water.

Satellite
Satellite
I almost missed the powerhouse for this one because it is downstream, and I do not see an intake structure for the penstocks.

Satellite
Satellite
This reservoir needed some "helper" side dams.
So the Pine River Dam is one of WE Energies smaller reservoirs.




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Lake St. Lawrence and its Dams

(Moses-Saunders Power Dam Satellite, Long Sault Dam Satellite)

Long Sault Dam is effectively the emergency spillway for the Moses-Saunders Power Dam. Normally, the entire flow of the St. Lawrence River would go through the power dam to maximize the production of electricity. For simplicity, I'm going to refer to these two dams as the Cornwall Dam. I've seen the "Cornwall Dam" reference in news articles. The slack pool created by these dams is called Lake St. Lawrence.

ijc.org
Moses-Saunders Power Dam
May 22, 2017, file photo from the International Lake Ontario - St. Lawrence River Board (source)
Facebook, lots of gates are open because gates are closed at the power dam for routine turbine maintenance. Seeing this significant flow gives us great insight as to how big the flow is through the power dam. The river flow is more than the flow going over Niagara Falls because some of the flow of the Niagara River is diverted through powerhouses. Furthermore, the watershed for these dams is greater than the watershed for the Niagara Falls.
When they built a 9' navigation channel in an American river such as the Upper Mississippi, Ohio, Illinois, Tennessee, etc., they didn't dig down 9', they built a lock & dam to raise the level of the water to create a series of slack pools. To create the 26'+ navigation channel in the St. Lawrence river, these "slack pools" are big enough to be called lakes. Lake St. Lawrence is created by the Cornwall Dam and creates a pool 26'+ deep at the foot of the Iroquois Lock and Dam.

Unlike a 9' rise in water level, a 26' rise is significant enough that it flooded some of the towns that were on the original shores of the St. Lawrence River. I have already described how the entire town of Iroquois was moved up a hill.

Peter Joseph posted
As a result of the tanker Chem Norma becoming stuck on an embankment, I learned that Morrisburg, ON was another town that was partially flooded when they closed the gates of the Cornwall Dam. The ship strayed off course because it had an issue with its rudder. As with all tankers on the St. Lawrence Seaway, it is double hauled. There were no pollution issues. [GreatLakes-Seaway] (After they freed it and inspected it, not even the outer haul was damaged.) I've already described how they first tried to use a lot of horsepower (three tugboats and the ship) to free it. They ended up raising the level of Lake St. Lawrence a little and then all of that horsepower was able to pull the ship free.

This image is part of an analysis of what the tanker got stuck on. It shows us that the part of Morrisburg that got flooded included some old locks. Specifically it was Lock 23 built in the 1800s.
OttawaRewind (source)
Not only did Lake St. Lawrence require that 6,500 people be moved to higher ground, the native Mohawk people of Akwesasne, who lived in this traditional territory for centuries, lost much of their land including islands, fishing sites, and both burial and sacred sites. [OntarioPowerGeneration]


Satellite
The power dam is more than a half-mile long and contains 32 turbines. Note how the border goes right through the middle. The 16 turbines on the Canadian side are operated as the Robert H. Saunders Generating Station. The 16 turbines on the American side is the Robert Moses Power Dam, and it can produce 800,000 kilowatts of electricity for the New York Power Authority. The cheap electricity supports the regional economy by supporting aluminum, zinc, and glass companies.

The International Lake Ontario - St. Lawrence River Board (River Board) is responsible for controlling the flows through the Iroquois Dam and these dams. The power dam should have been designed so that the ideal river flow is the capacity of the powerhouse with no water going over the spillway dam. The effect of these dams on the river is significant enough that upstream is considered the "upper St. Lawrence River" and downstream is considered the "lower St. Lawrence River."  The "upper St. Lawrence River" is basically Lake St. Lawrence. To determine the outflow of the dams, the River Board considers the need of the powerhouse, maintaining a minimum depth in the navigation channel, and water levels for Lake Ontario and the upper and lower St. Lawrence River. If water levels are too high, it increases erosion of the shoreline and it can flood property. If it is too low, then the water intakes for towns along the river provide an inadequate flow to the town. And people's boats can't reach their piers. When determining the outflow rate, the River Board must also consider precipitation in the watershed and evaporation from Lake Ontario. Water flow through the locks is negligible. If outflows are high, then commercial shipping is stopped because the river currents are too dangerous.

Three plans as to how to determine the river flow had been written: 1952, 1956, and 1958D. In 2014, work began a new plan "to improve ecosystem health and diversity on Lake Ontario and the upper St. Lawrence River....Allowing for more natural variations of water levels, the plan aims to foster the conditions needed to restore Lake Ontario and upper St. Lawrence River coastal wetlands and improve habitat for fish and wildlife. The plan will also frequently extend the Lake Ontario recreational boating season in the fall, better maintain system-wide levels for navigation and allow for a modest increase in hydropower production compared to the previous plan." Plan 2014 became effective Dec. 8, 2016. [ijc]

An additional issue the River Board must consider is the formation of a stable ice cover. When ice starts to form, the outflows are reduced to allow an ice cover to form. After a stable ice cover forms, the flows can be increased. Furthermore, if the Ottawa River is causing flooding in the Montreal area, outflows are reduced to reduce the extent of the flooding in the Montreal area. [ijc]

But in 2017, Mother Nature dumped a record amount of precipitation into Ontario Lake causing flooding.
InternationalLakeOntarioStLawrenceRiverBoatd
Unfortunately, Mother Nature also dumped a lot of precipitation in the Ottawa River watershed and flooded Montreal. People living on the shores of Ontario Lake were calling for higher outflows.
Letting out enough water to lower Lake Ontario by 1 inch would raise the level of the river at Montreal by nearly a foot, says the International Joint Commission, which controls water levels. Letting less water out of the lake until the Ottawa River peaks "can prevent several feet of flooding in the Montreal area," said commission spokesman Frank Bevacqua. During nine days in April and May when the Ottawa River was high, the commission let less water out of Lake Ontario, Bevacqua said. The commission plans to start discharging more water from the lake as the water levels near Montreal begin to recede, Bevacqua said. [NewYorkUpstate-flooding]
Below the above article is this drought information. But I think the flooding was May 10, 2017 and this drought article is current (Sep 7, 2018). I still get the printed Chicago Tribune delivered to my house, so I'm not experienced with reading "web news." But the juxtaposition of old and new articles does demonstrate that Mother Nature can have significant "mood swings."
A severe drought (orange) is now affecting parts of the Adirondacks, while 20 percent of New York remains in a moderate drought (tan) or is considered abnormally dry (yellow). (U.S. Drought Monitor)
New York's Gov. Andrew Cuomo demonstrated that he is another politician that makes statements before consulting with his experts because he joined the Ontario Lake residents asking for more water to be released downstream. [NorthCountryPublicRadio]

Evidently the water level in the lower St. Lawrence River is now low enough that they have been able to use the spillway and powerhouse to increase the outflow. But this creates another problem, low river levels on the downstream end of Lake St. Lawrence. An organizer of a Sep 11, 2018 meeting to complain about the low levels claims parts of the river are now down to the bare minimum needed to support commercial shipping --- something not seen since at least 1998.
NationValleyNews
I found the NationValleyNews link in a Facebook posting.

Dennis DeBruler Why don't they open the gates at the Iroquois Dam as well to match the flow being spilled by the Cornwall Dam to maintain the traditional height of Lake St. Lawrence? Especially since they want to get water out of Lake Ontario?

Dennis DeBruler I think I now understand. I'm looking at a photo at the downstream part of Lake St. Lawrence. As the flow increases, the "lake" turns back into a river and the water slopes downstream from Iroquois to Cornwall causing the water level to be significantly lower at the Cornwall end. Basically, the water management people have done such a good job for so many decades that people think they bought land on a lake instead of a river. At least they have the advantage that the exception is that the water goes down instead of up. Most people that live on a river get flooded, not drained, by abnormal weather. For example the Mid-Continental Railway Museum got hit this summer by the Baraboo River. They were still trying to recover from a 2008 flood. https://www.facebook.com/.../a.22924.../2293066620709671/...

Dennis DeBruler Even a true lake can be at the mercy of Mother Nature's precipitation moods. Lake Michigan varies by about six feet. When Lake Michigan went down after Chicago reversed the flow of their river, Wisconsin sued the sanitary district to reduce the flow. Water Treatment Plants were invented and a lock was installed at the mouth of the river to reduce the flow out of the lake. Later, when the lake went back up, Chicago was asked to open the locks and allow big flows again. Chicago refused because the outflow was a drop in the bucket compared to what Mother Nature was adding and because a heavy river flow would disrupt barge traffic.



Update Oct 2, 2018: the flow will be reduced so the water level near the Cornwall Dam should go up about 2 feet.
The international board said this week that it will temporarily decrease outflows significantly over two 45-hour periods during the first two weekends of October to provide an opportunity for residents of Lake St. Lawrence and upstream of that area to remove their boats and other equipment while the river level rises.
“These flow decreases will temporarily raise Lake St. Lawrence levels, which will assist marinas, yacht clubs and other recreational boaters in the area in removal of their boats prior to winter,” according to the organization’s statement. “The board acknowledges the concerns identified at recent meetings with the public in the area, and the board takes each concern very seriously. The exact amounts of the water level rises will vary depending on a number of factors, including location, winds and other secondary factors.”
[WaterTownDailyTimes]
CHRISTOPHER LENNEY / WATERTOWN DAILY TIMES
Boaters are complaining that low river levels  at the Patterson Street access site make it difficult to remove their vessels.
Satellite
I notice there is are bins, piles of materials, a crane and conveyor belts in the background of the above photo. But there is none of this infrastructure in a satellite image.

After studying a satellite image, I noticed that the levels at Ogdensburg are controlled by the Iroquois Dam instead of the Cornwall Dam. The article says the flow reduction will raise the water level at Ogdensburg just three inches instead of the two feet expected near the Cornwall Dam.

South Stormont is another town near the Cornwall Dams that is complaining about the low water levels. It is not just a matter of the people along the shore refusing to convert to floating docks, the exceptionally low water levels is exposing hazards to navigation. They claim it is impacting commercial as well as recreational boats. “What if an oil ship gets punctured? It could be a disaster and that’s the point I’ve tried to get across to the IJC.” But I can't believe the River Board would jeopardize the 26'+ draft of the Seaway navigation channel. [CornwallSeawayNews] Of note, all tankers on the Seaway are required to be double hulled.



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Saint Croix Falls Hydro Dam

Satellite
John A Weeks III
The gated spillway used to be a log sluice. But it obviously has a Tainter gate now.

I learned of this dam while studying the Nevers Dam. I had planned on skipping yet another hydro dam until I saw this image. That is the steepest, highest hydro jump I have ever seen.
Ben Hanson Photo, July 2016
After the storm
Evidently Ben had access to the powerhouse and was able to get a shot from the corner of the powerhouse next to the spillway. Looking at the satellite image, there is a gated spillway at the north end of the dam. The overview below shows that spillway can pass a lot of water so the storm that created the above flow over the fixed spillway must have been really impressive. I wonder if some of the boards on top of the spillway were removed in anticipation of the storm or if the gaps are a sign of lax maintenance. The high, sharp hydraulic jump is caused by the water level being so high. The water level is so high because a wide fixed spillway is filling a narrow discharge channel.
Kyle Ahlborn Photo, July 2017
The 59' high dam creates a reservoir that covers the 55' drop in the river.
John A Weeks III, 1.5x and cropped


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Copper River & Northwestern Railway and its bridges

Mile 27, Flag Point Bridge: ( Satellite ; Blog ; more below) Mile 28: the bridge no longer exists; Blog Mile 34, Hot Cake Bridge: the bridge...