Lower Pilarcitos Creek Groundwater Basin Study - Coastside ...
Lower Pilarcitos Creek Groundwater Basin Study - Coastside ...
Lower Pilarcitos Creek Groundwater Basin Study - Coastside ...
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aquifer. The S-value ranges between 0.00071 and 0.0013, indicating that the marine<br />
terrace aquifer is confined near the Balboa wellfield.<br />
The informal pumping tests performed by drilling contractors are usually recorded<br />
on the DWR Water Well Drillers reports and provide basic hydraulic information including<br />
static water level (SWL), pumping water level (PWL), length of pumping test, and the<br />
approximate discharge. These are reported in Appendix 2, well inventory information.<br />
The well inventory lists 380 wells (62 percent) with hydraulic information.<br />
Because the T-value (and, by inference, the specific capacity) varies with geologic<br />
materials, the well inventory was sorted by aquifer type (alluvium, marine terrace, and<br />
bedrock) and summarized to determine the minimum, maximum, and average specific<br />
capacities. The specific capacity for these wells varies by at least three orders of<br />
magnitude and ranges between 0.006 (bedrock) to 7.06 gpm/ft of drawdown (alluvium<br />
and marine terrace). The alluvium and marine terrace aquifers are similar in hydraulic<br />
properties, averaging 2.82 and 2.64 gpm/ft of drawdown, respectively; the average for<br />
bedrock is 0.66 gpm/ft of drawdown. This suggests that the T-values of the geologic<br />
units range between 1,000 gpd/ft for bedrock and 5,500 gpd/ft for the alluvium and<br />
marine terrace units.<br />
In summary, the marine terrace aquifer near the proposed <strong>Lower</strong> <strong>Pilarcitos</strong> <strong>Creek</strong><br />
wellfield has a T-value of about 16,000 gpd/ft, an aquifer thickness of about 32 feet, a K-<br />
value of 500 gpd/ft 2 , and is a confined aquifer. The marine terrace aquifer near the<br />
Balboa wellfield has a T-value of about 9,400 gpd/ft, an aquifer thickness of about 42<br />
feet, a K-value of about 224 gpd/ft 2 , and an S-value of 0.0011 (confined aquifer). In<br />
regions south of the proposed <strong>Lower</strong> <strong>Pilarcitos</strong> <strong>Creek</strong> wellfield, the T-value is lower<br />
ranging between 1,500 and 7,000 gpd/ft. Regional informal pumping tests and empirical<br />
analysis of the data suggest that the T-value may range between 1,000 and 5,500 gpd/ft<br />
for bedrock and marine terrace aquifers, respectively. In general, the informal pumping<br />
test data are consistent with formal aquifer and well testing.<br />
<strong>Groundwater</strong> Elevation Maps<br />
Geoconsultants (June 1987, August 1991, and September 1993) constructed<br />
four groundwater elevation or potentiometric maps for the <strong>Lower</strong> <strong>Pilarcitos</strong> <strong>Creek</strong> coastal<br />
plain between Arroyo de en Medio and Cañada Verde. The four maps include (1) a<br />
composite map for 1978 to 1987, (2) winter 1990-91, (3) summer 1991, and (4) summer<br />
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