Serious water critique from LA ...

...which has much drinking water to lose if things go wrong in Northern California. On the one hand, these are very sober, penetrating articles that reveal major issues in the state's water-development policies. On the other hand, they don't ask more fundamental questions: Is the size of California's population good? Has population growth brought more happiness to more people" Has it created better citizens? Is California a safer place to live than it was when the Oroville Dam was built in 1968 when we had half as many people, 20 million, than we do today at 40 million? -- blj
Los Angeles Times
Capitol Journal 
Does California really need more dams? We're running out of places to put them
George Skelton
You hear this every time there’s a drought or deluge in California: “Why haven’t they built more dams?” Truth is, they’ve built a bunch. And they’re about done with it.
Tally them up. There are more than 1,400 dams in the state. At least 1,000 are major and 55 can hold 100,000 acre-feet or more of water.
One acre-foot is enough to supply two average households for a year.
There are 36 reservoirs that can contain at least 200,000 acre-feet. Eleven can hold 1 million or more.
The biggest is Shasta on the Sacramento River at 4.5 million acre-feet. Then comes Oroville with its broken spillways on the Feather River at 3.5 million.
The largest reservoir in Southern California is Diamond Valley in Riverside County at 810,000 acre feet. For perspective, Castaic Lake off Interstate 5 heading over the Grapevine is about 324,000 acre-feet.
So there’s already a heap of storage capacity in California — or what’s called “surface storage” in water talk, in contrast to underground aquifers. The largest 200 reservoirs alone have a combined capacity of 41 million acre-feet.
There’s at least one dam on every river running off the west slope of the Sierra except for the Cosumnes, just south of Sacramento, says Jeffrey Mount, a water expert at the Public Policy Institute of California. “And that doesn’t have enough water in it to make a dam worthwhile,” he adds.
Thankfully. The Cosumnes frequently spills over its banks, flooding roads and barns. But just before it enters the Sacramento-San Joaquin River Delta, the natural-flowing Cosumnes forms a popular nature preserve that annually hosts thousands of migratory waterfowl, including giant sandhill cranes.
California has lost 95% of its wetlands since 1900. So pardon if talk of “balancing” what’s left isn’t really appealing.
Anyway, dams don’t make it rain and end droughts. And lack of rain was our principal drought problem, regardless of corporate agriculture’s squawking about governments and judges coddling salmon.
“You can build more dams, but there isn’t more water flowing into California,” says Jay Lund, a water expert and professor of civil and environmental engineering at UC Davis.
“This year, there’s more water than reservoirs. But if you can only fill them every 10 years, they make less sense economically.”
There aren’t many sensible dam sites left in California.
“We’ve already built the cheap dams,” Lund says. “The remaining sites mostly are pretty expensive and are not going to give you that much water. Economically, you’re not going to find a lot of people volunteering to pay for those dams. They’d be happy if someone else paid for one.”
For environmental and cost reasons, Gov. Ronald Reagan killed dam proposals on the Eel River and the Middle Fork of the Feather nearly 50 years ago. An earthquake scare later scuttled a proposed dam on the American River above Folsom Lake.
There are earthquake faults all over California that unnerve dam builders. “There’s nothing simple about water in California,” Lund notes.
The best bet for the next major dam in California is called Sites, named after an old settlement in the low foothills of the Coast Range 14 miles west of the Sacramento River near Colusa.
This would be an “off-stream” reservoir that didn’t dam a river, so there’s much less opposition from environmentalists. Water would be piped into the reservoir from the Sacramento when it was running high.
It would have a capacity of 1.8 million acre-feet and be the seventh-largest reservoir in California. It’s estimated that 500,000 acre-feet could be delivered a year, split between agriculture, domestic and environmental use. But there’d be only minor flood-control value, experts say.
The cost? About $5 billion. Proponents are preparing to seek money from the $7.5-billion water bond issue that voters approved in 2014. Of that, $2.7 billion was set aside for water storage.
Under the measure, up to half a project’s cost could be paid for by the bond money. The rest would need to be footed by the water users on their monthly bills.
But before water districts in the San Joaquin Valley and Southern California commit to pitching in, they’d need assurance the water could be moved through the troubled delta. And that’s anything but certain.
Delta farmers and environmentalists are fighting Gov. Jerry Brown’s $15.5-billion plan to dig two monstrous tunnels to siphon off fresh Sacramento River water before it ever reaches the estuary. And Brown hasn’t shown any interest in trying to fix the fish-chomping water transfer system that exists.
One other major dam is being promoted, but its economics are less promising and its environmental impact more controversial. It’s Temperance Flat near Fresno on the San Joaquin River above Friant Dam. Its backers also are eyeing a piece of the 2014 bond issue.
“The default reaction when we’re faced with a water emergency is the 20th century notion that large investments in concrete will somehow solve our problem,” Mount says.
“But if you’ve already tapped out that, the alternative is to look more closely at whether we can do a better job with what we have. And to date we haven’t done that.”
Operate the dams more efficiently. Recharge the aquifers. Expedite groundwater regulation. Capture storm runoff. Recycle. Desalinate.
Build Sites. Compromise and fix the delta.
One thing is not the answer: continuing to plant thirsty nut orchards in the arid San Joaquin Valley.






Los Angeles Times
Government severely misjudged strength of Oroville emergency spillway, sparking a crisis  
Bettina Boxall
Bill Croyle stood in front of an aerial photo of Lake Oroville and swept his hand across the top of the emergency spillway that was helping drain water out of the brimming reservoir.
“Solid rock. All this is rock,” Croyle, acting director of the Department of Water Resources, said with an air of confidence at the Feb. 11 briefing.
The flows over the concrete lip of the unpaved spillway were tiny compared with what it was designed to handle. Oroville’s first-ever emergency spill was going smoothly.
Some 27 hours later, state officials told Butte County Sheriff Kory Honea that erosion was chewing away at the base of the spillway’s concrete lip. It was on the verge of collapse, threatening to send a towering wall of flood water surging through downstream communities, endangering tens of thousands of people. Honea ordered a mass evacuation.
The erosion slowed and dam managers succeeded in getting enough water out of the reservoir to stop the emergency spill late Feb. 12. California narrowly averted what could have been one of the worst dam disasters in state history.
Interviews and records suggest that the near-catastrophe grew out of fundamental problems with the original design of the emergency spillway that were never corrected despite questions about its adequacy.
The “solid” bedrock that Croyle thought would stand up to the force of the spill was soft and easily eroded. The long concrete lip of the spillway was not anchored into the rock. Critical power lines were strung across the spillway, which consists of nothing more than an earthen hillside covered with trees and brush.
“There is no way to rationalize running water down a hillslope with deep soils and a forest on it and weak bedrock,” said Jeffrey Mount, a UC Davis emeritus professor of geology and expert on California water.
Federal and state officials said the cause of the spillway’s near-failure was under investigation.  
The key reservoir in the State Water Project that typically provides Southern California with roughly a third of its supplies, Oroville started operation in 1968. Routine water releases are made through the powerhouse at the base of the dam, which is the nation’s tallest.
Higher releases go down the main spillway, a long, gated concrete chute off to the side of the dam. The emergency spillway — which until Feb. 11 had never been used — is to the side of the main spillway.
After a hole big enough to swallow a small house appeared in the main spillway, chunks of concrete and dirt tumbled into the channel at the base of the dam, raising water levels and forcing managers to stop the powerhouse discharges.
Operators reduced flows down the main spillway to avoid further damage, leaving them with limited discharge abilities just as storm runoff was pouring into the lake. Oroville — which at the same date a few years ago was less than 40% full — was suddenly full to the brim.
The morning of Feb. 11, what Croyle called “a little water” started spilling over the concrete lip like an overflowing bathtub. At the peak of the spill, roughly 1 ½ feet of water was sheeting out of the reservoir, spreading over the top of the hill and forming a stream as it followed a ravine down to the Feather River.
The 1,700-foot long lip, known as a weir, was supposed to handle up to a 16-foot flow over its top.
Beneath it was mostly schist, metamorphic rock that Mount described as weathered and fractured. It started to erode under the force of the spill.
“There are unlined spillways elsewhere that perform well,” Mount said. “But they tend to be in resistant rock, and this rock is not very resistant. That is one of the design errors, not fully considering how soft and erodible that bedrock is. This stuff is all busted.”
More than a decade ago, several environmental groups asked federal regulators to require the state to armor the hillside that forms the emergency spillway. The dam’s operating rules called for use of the spillway as part of flood-control operations, they argued, so the slope needed to be armored to prevent damaging — and potentially dangerous — erosion.
In filings with the agency that oversees the dam — the Federal Energy Regulatory Commission — the groups cited a 2002 technical memo prepared for the Yuba County Water Agency that concluded emergency spills would cause extensive erosion on the hillside, potentially destroying high-voltage transmission towers and a road. Soil, rocks and debris would clog the Feather River.
 “We had real concerns that even if the spillway itself didn’t fail, moving all that erosion of topsoil down the river would cause major damage to a very important fishery,” said Allan Eberhart of the Sierra Club.
The 2005 filing by Friends of the River, the Sierra Club and the South Yuba River Citizens League also warned of “a loss of crest control” — which would have happened if the top of the spillway had collapsed, as it almost did Feb. 12.
A crumbling weir would have taken a dangerous bite out of the side of the reservoir, unleashing catastrophic torrents that Robert Bea, a UC Berkeley professor emeritus of engineering, said could have rushed more than 100 miles down the Feather and Sacramento rivers, breaching levees all the way to the Sacramento-San Joaquin River Delta.
In a May 2006 filing with FERC, the Department of Water Resources insisted that the emergency spillway was sound.
“DWR recently reviewed the geologic conditions at the emergency spillway and concluded that the spillway is a safe and stable structure founded on solid bedrock that will not erode,” the department stated. “The Project Geology Section determined that there are only one to four feet of erodible top soil in the downstream area and that erosion would not compromise the stability of the emergency spillway.”
A few months later, an internal FERC memo echoed Water Resources,  saying the spillway had been reviewed as part of a 2004 safety analysis: “It is important to emphasize that during a rare event with the emergency spillway flowing at its design capacity, spillway operations would not affect reservoir control or endanger the dam,” states the memo by a FERC senior civil engineer.
“FERC patted us on the head and said it’s all good, don’t worry about it,” said Ron Stork, a senior staffer at Friends of the River.
Stork is not an engineer, but his decades of river work have made him a dam geek. “I tried and failed” to get the state to upgrade the spillway, he said. “Maybe nature gave us a wake-up call that what I suggested is needed.”
FERC spokeswoman Celeste Miller said the agency could not comment on the 2006 memo or the basis of it because the Oroville events were under review. The memo was written during a periodic review of the dam’s operating license.
DWR spokeswoman Nancy Vogel said, “We don’t know the cause of the spillway erosion and we won’t know the cause until we get experts in there to do a full investigation and analysis.”
John France, a veteran dam safety consultant with Aecom, noted, “In 1968, quite frankly, there weren’t probably a lot of methodologies available to evaluate how rock erodes if you had flowing water on it.”
“Certainly we have to acknowledge that the performance we saw on that spillway was not consistent with [the DWR] conclusion,” he added. “We saw a significant erosion occur in that formation with far less than the design amount of water that would go over that structure.”
When the spillway issue came up during relicensing, Mount said, the state could have dug test pits and conducted lab analysis of rock corings to determine if the bedrock was as strong as they thought it was.
“They operated with an assumption that turned out to be incorrect,” he said.
Soft bedrock is not the only problem, he added. The concrete weir at the top of the emergency spillway was “just plopped on top of that ridge. It’s a design area that will probably get a lot of scrutiny and had to be a major concern as [the spillway] was eroding up the hill.”
Vogel confirmed that the weir, which she said ranges in height from 25 feet to 45 feet, was not anchored.
As to why the state never moved transmission lines that cross both spillways and connect the dam powerhouse to the electrical grid, Vogel said, “The main spillway performed well for the past 50 years, so there was no perceived need to relocate.”
State contractors worked around the clock last week to strengthen the top of the emergency spillway with thousands of tons of rock sealed in place with concrete slurry as dam operators shoved as much water down the broken main spillway as they safely could.
By late Friday afternoon, reservoir levels had fallen more than 40 feet below the trigger point for emergency spills.