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San Benito County Water District San Benito County Water District

San Benito County Water District San Benito County Water District

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RECOMMENDATIONS<br />

This annual report is required under Section 70-7.6 of the State <strong>Water</strong> Code to include<br />

recommendations regarding groundwater production, groundwater replenishment, CVP<br />

imports, and water charges in water year 2009.<br />

In 2009, the <strong>District</strong> continues to face an uncertain imported water supply as the ramifications<br />

of the May 2007 Court decision on Delta smelt and the July 2008 Court decision on the Delta<br />

salmonoids are materialized over the upcoming months. While CVP allocations are expected to<br />

remain similar to those observed in water year 2008, groundwater use is expected to increase as<br />

groundwater infrastructure is put in place to meet growing demand and users adjust their<br />

cropping and irrigation practices to rely more heavily on groundwater. However, in past years<br />

the <strong>District</strong> has accumulated substantial reserves in the groundwater basin that can now be<br />

relied upon for water supply.<br />

GROUNDWATER PRODUCTION AND REPLENISHMENT<br />

Groundwater levels increased slightly over the past year and groundwater storage in most<br />

subbasins is near historic highs. Groundwater storage is adequate to meet water demands in<br />

2009 and years thereafter. As a matter of perspective, groundwater pumping over the four<br />

drought years of 1988 through 1991 averaged 34,456 afy, similar to the amount estimated for<br />

2009. These pumping rates resulted—as expected—in temporary groundwater level declines<br />

(see Figure 17). The recommended amount of groundwater production for 2009 is the<br />

amount—in conjunction with available CVP water—that meets agricultural, M&I, and<br />

domestic water demands, assuming efficient water management practices.<br />

Historically, the <strong>District</strong> conducted extensive percolation operations that ultimately reversed<br />

overdraft and then accumulated a substantial water supply reserve. <strong>District</strong> management of<br />

groundwater storage in conjunction with surface water is currently being refined to avoid<br />

excessively high or low water levels both on a temporal and geographic basis. In 2009, storage<br />

in Hernandez Reservoir should be replenished and percolation of available local water supplies<br />

should be focused on areas exhibiting declines in response to drought and increased pumping.<br />

In the longer term, the <strong>District</strong> should consider the ramifications for groundwater management<br />

of increasingly unreliable CVP supply. While overall groundwater storage is substantial,<br />

increasing use of groundwater is likely to result in localized declines. Such potential problems<br />

can be minimized with groundwater management planning that addresses the distribution of<br />

groundwater pumping relative to areas of historical high groundwater and to areas of historical<br />

and existing percolation activities. The percolation capabilities of the latter areas (including<br />

<strong>District</strong> access, permeable surficial sediments, and flat channel area for water spreading) may<br />

need protection in light of intensifying and potentially competing land uses.<br />

Annual Groundwater Report for <strong>Water</strong> Year 2008 December 2008<br />

<strong>San</strong> <strong>Benito</strong> <strong>County</strong> <strong>Water</strong> <strong>District</strong> 46

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