24.06.2015 Views

San Benito County Water District San Benito County Water District

San Benito County Water District San Benito County Water District

San Benito County Water District San Benito County Water District

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

Table 5. Change in Storage during <strong>Water</strong> Year 2008 for Zone 6<br />

Subbasin<br />

Area<br />

(acres)<br />

Average Change in<br />

Groundwater Height<br />

(feet)<br />

Average<br />

Subbasin<br />

Storativity<br />

<strong>San</strong> Juan 11,708 0.30 0.05 174<br />

Hollister West 6,059 3.33 0.05 1,009<br />

Tres Pinos 4,735 -0.67 0.05 -158<br />

Pacheco 7,290 -1.36 0.03 -298<br />

Hollister East 15,367 -0.87 0.03 -403<br />

Bolsa SE 2,690 11.54 0.08 2,483<br />

TOTAL ZONE 6 2,807<br />

Change in<br />

Storage (af)<br />

In recent years, the volume of managed percolation has been decreased in response to high<br />

water levels. The recent annual quantities of managed percolation are very small in comparison<br />

to the peak volumes from the late 1990s. Because managed recharge has been greatly reduced,<br />

storage fluctuations caused by pumping and other sources of recharge can be seen more clearly.<br />

When groundwater levels are high, upward fluctuations in storage are limited because excess<br />

groundwater tends to leak into streams rather than accumulate in storage. Conversely, when<br />

groundwater levels decline, groundwater discharge into streams is affected almost immediately.<br />

Figure 17 illustrates long term changes in groundwater levels in the basin. <strong>Water</strong> elevations in<br />

key wells from each subbasin for each monitoring event were averaged to produce<br />

representative hydrographs for each subbasin. These key wells are shown on the map in Figure<br />

17. It should be noted that these subbasin hydrographs represent average conditions in each<br />

subbasin and illustrate long term trends, but do not show localized variations in water levels.<br />

Over the past five years, water levels have remained fairly constant in most subbasins. This<br />

includes an interruption in the long-term rising trends seen from 1994 to 2006 in the Hollister<br />

East and Bolsa Southeast (SE) subbasins, where average water levels remained fairly stable<br />

between 2007 and 2008. The increasing trend was related to reduced groundwater pumping and<br />

increased CVP delivery for both agricultural and M&I uses. <strong>Water</strong> levels in all subbasins show<br />

a seasonal variation with the lowest water levels occurring in the fall and the highest in the<br />

spring. The Bolsa subbasin shows the most variation: 20 to 50 feet of elevation change between<br />

seasons.<br />

<strong>Water</strong> levels continue to remain generally near their historic highs in most parts of the basin.<br />

Based on these water levels and the stable management of the basin, there was no overdraft in<br />

2008 and overdraft is unlikely to occur in 2009.<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> 32

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!