Vanni v. Depart. Water Resources CA3

CourtCalifornia Court of Appeal
DecidedOctober 30, 2014
DocketC072383
StatusUnpublished

This text of Vanni v. Depart. Water Resources CA3 (Vanni v. Depart. Water Resources CA3) is published on Counsel Stack Legal Research, covering California Court of Appeal primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Vanni v. Depart. Water Resources CA3, (Cal. Ct. App. 2014).

Opinion

Filed 10/30/14 Vanni v. Depart. Water Resources CA3 NOT TO BE PUBLISHED California Rules of Court, rule 8.1115(a), prohibits courts and parties from citing or relying on opinions not certified for publication or ordered published, except as specified by rule 8.1115(b). This opinion has not been certified for publication or ordered published for purposes of rule 8.1115.

IN THE COURT OF APPEAL OF THE STATE OF CALIFORNIA THIRD APPELLATE DISTRICT (San Joaquin) ----

ARMANDO P. VANNI, as Trustee, etc., et al., C072383

Plaintiffs and Appellants, (Super. Ct. Nos. CV025820, CV026726, CV028072) v.

DEPARTMENT OF WATER RESOURCES,

Defendant and Respondent.

On June 3, 2004, a levee on the Middle River in the California Delta failed, damaging farms and property of BNSF Railway Company (BNSF) and East Bay Municipal Utility District. Plaintiffs, area farmers, BNSF, and insurers, brought separate suits (later consolidated) for inverse condemnation against the Department of Water Resources (DWR), contending the operation of the California State Water Project (SWP) caused scour (erosion) which in turn caused the levee to fail. After a court trial, the court determined that plaintiffs had failed to prove their case and entered judgment for DWR.

1 On appeal, the farmers (the Vanni plaintiffs) and BNSF offer a new legal theory of DWR’s liability.1 They contend the levee that failed is indisputably part of the SWP, as planned and constructed, and therefore DWR is liable for its failure. They assert this new theory may be considered on appeal because it is based on undisputed facts. They further contend that the trial court’s decision was predicated on its finding the absence of scour at the failure site and substantial evidence does not support this finding. As we explain, we find plaintiffs’ new theory of liability is not simply a question of law based on undisputed facts established at trial; thus plaintiffs may not raise this new theory for the first time on appeal. We reject plaintiffs’ contention that the judgment was based on factual premise not supported by the evidence. Substantial evidence supports the trial court’s judgment. Accordingly, we shall affirm. FACTUAL AND PROCEDURAL BACKGROUND The Delta and Nonproject Levees The Delta covers 738,000 acres, ranging from Sacramento in the north to just past the City of Tracy in the south. From its western edge at the salinity gates of the Suisan Marsh (just west of Pittsburgh), it extends to east of Walnut Grove. The water in the Delta is influenced by the tides; indeed, the tides are the primary force on Delta waters. In each 25-hour period, there are two flood tides (coming in) and two ebb tides (going out). Originally, the Delta was a tidal marsh, but farmers reclaimed the land and controlled the tides by building levees. The levees in the Delta were built by dredging the channels. Upper and Lower Jones Tract were excavated out of the marshlands. Land in the Delta contains a large amount of peat. Farming introduces oxygen into the peat, which breaks it down. The land then blows away, called subsidence. As a result, much of the land in the Delta is below sea level. Lower Jones Tract is 15 feet below sea level;

1 Only the Vanni plaintiffs and BNSF appealed. The insurers are not parties on appeal. 2 Upper Jones Tract, where the levee breach occurred, is 11 feet below sea level. Subsidence increases the pressure on the levees. The levees on Upper Jones Tract are “non-project” levees under Water Code section 12980, meaning they were constructed by private interests, not by the government. Most were built by agricultural interests from the 1860’s to 1930’s. Project levees are maintained by the Corps of Engineers, but nonproject levees are owned and maintained by local reclamation districts. The state has no authority to maintain or take over nonproject levees. The state’s involvement with nonproject levees is through the subventions program, under which the state provides some reimbursement to reclamation districts for work on nonproject levees. The reclamation districts, not the state, are responsible for the work. DWR conducts inspections to determine only if the work was done, not to determine if the work was done properly. The state cannot require reclamation districts to perform work on nonproject levees. The Water Projects: the SWP and the CVP The SWP was designed and constructed in the 1960’s to transport water to various parts of California. Water from the Feather River flows into Lake Oroville, the initial storage facility and highest nonfederal dam ever built. Water is released from Lake Oroville into the natural channel of the Feather River which connects with the Sacramento River; the water then flows naturally into the Delta. The Sacramento River provides 80 percent of the fresh water in the Delta; the San Joaquin, Mokelumne, Cosumnes, and Calaveras Rivers provide the rest. Most of the water, 76 percent, flows out of the Delta to the ocean with the tides; six percent is used in the Delta; and 18 percent is exported to the Bay Area, and Central and Southern California. The North Bay Aqueduct takes water from the upper Delta and feeds the North Bay. There are water facilities in the Delta, including the Clifton Court Forebay and the Harvey Banks Pumping Plant. The Clifton Court Forebay is a man-made reservoir, known as “Mile Point Zero” of the California Aqueduct. Water from the Delta flows into the forebay through five intake gates. These gates do not have pumps; the water flows by 3 gravity due to the elevation difference. The Harvey Banks Pumping Plant is located off a canal of the Clifton Court Forebay. Water is pumped from this plant to the South Bay Aqueduct to supply the South Bay and to the California Aqueduct, a concrete lined channel flowing to Southern California. The Old River and the Middle River are the main channels that conduct water from the Delta into the Clifton Court Forebay. Thus, the channels of the Delta are part of the SWP’s water conveyance system. The Central Valley Project (CVP) is a federal project, funded during the 1930’s as part of the New Deal Program. It, like the SWP, is a water project, designed to transport water from Northern to Southern California. The two water projects transport like amounts of water. The 20-year average is 2.5 million acre-feet pumped from the SWP and 2.3 million acre-feet pumped from the CVP per year. The CVP pumps water out of the Delta at the Tracy Pumping Plant (now the Jones Pumping Plant) into the Delta- Mendota Canal. It does not have a forebay, but pumps directly from the Delta. Unlike the SWP, the CVP pumps constantly. Scour Monitoring Program Scour is erosion or the removal of soil caused by running water. In 1969, in connection with the SWP, DWR started a scour monitoring program in the south Delta. There was concern that the SWP and the CVP could have an impact on the Delta relative to scour. The number of monitoring sites began at 26 and increased as time went by. Monitoring is done by bathymetry, the practice of taking soundings to map underwater surfaces. Originally, DWR used single-beam bathymetry, but switched to multi-beam after 2003. Multibeam bathymetry covers a wider area by using multiple sound waves to gather depths. The levee breach was between two monitoring sites on the Middle River, MR-105R and MR-115R. The Levee Failure On the morning of June 3, 2004, the levee on Upper Jones Tract that holds back the Middle River failed, and water rushed onto the land. The force of the water

4 overturned farm equipment. It took until December 2004 to pump all the water out. There were at least two eyewitnesses to the levee failure. One, Dennis Lass, flew over the Middle River every morning in an ultralight experimental aircraft. On June 3, 2004, he flew over at about 7:30 a.m. Flying at 12 feet above the river, he saw a levee breach across the Middle River from Woodward Island.

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