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SU0004126
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SU0004126
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Entry Properties
Last modified
6/27/2024 9:08:38 AM
Creation date
9/4/2019 10:27:44 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
RECORD_ID
SU0004126
FACILITY_NAME
QX-91-0005
STREET_NUMBER
35656
Direction
S
STREET_NAME
BIRD
STREET_TYPE
RD
City
TRACY
ENTERED_DATE
5/12/2004 12:00:00 AM
SITE_LOCATION
35656 S BIRD RD
RECEIVED_DATE
11/18/1997 12:00:00 AM
QC Status
Approved
Scanner
SJGOV\gmartinez
Supplemental fields
FilePath
\MIGRATIONS\B\BIRD\35656\QX-91-05\SU0004126\PUB REC REL APPL.PDF
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EHD - Public
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8 <br /> ground-water levels have declined gradually across the area such that the ground-water conditions <br /> have returned to the southeasterly flow direction observed during 1994 (Figures 8 and 9, <br /> respectively). <br /> The contour maps were prepared without including the observed water levels from the deep South <br /> Tracy#1 or Brown's #1 wells because they are representative of the deep ground water zone. Also, <br /> the observed water levels from the Petz well, which is completed in both shallow and deep zones of <br /> the underlying aquifer, were not used in preparing the contour maps. Until mid-1998, the Petz well <br /> water levels had been in an intermediate elevation range between those measured in wells solely <br /> completed in the shallow or deep zones; those measurements have typically represented a <br /> "composite" of shallow and deep zone water levels and thus are invalid for use in contouring the <br /> shallow or deep ground-water levels exclusively. <br /> Ground-Water Quality <br /> General mineral analyses of ground-water samples conducted during the last six years indicated that <br /> the ground water beneath the area is hard to very hard with intermediate electrical conductivity (EC) <br /> and total dissolved solids (TDS) values (Tchobanoglous, 1985), as shown in Table 2. Hardness <br /> values ranged from 230 to 360 mg/1 (Figure 10), and EC values ranged from 790 to 1,100 umho/cm <br /> with the highest EC values in samples from the shallow wells (Figure 11). Samples from all wells <br /> were of a similar sodium/calcium quality, but the proportions of major anions varied with aquifer <br /> depth. The shallow ground water appeared to be of a bicarbonate/chloride quality, such as shown by <br /> the Hall well analyses (Figure 12), while deep ground water appeared to be of a bicarbonate/sulfate <br /> quality as shown by the Brown's#1 well analyses (Collins, 1928; Piper, 1953; Hem, 1959) <br /> (Figure 13). <br /> HA 9 f > .. <br /> 111 <br /> In regard to other notable ground-water constituents, nitrate levels were elevated in both shallow and <br /> deep well samples, with concentrations in the South Tracy#1 production well fluctuating alternately <br /> slightly above and below the drinking water maximum contaminant level (MCL) of 45 mg/1 during <br /> © LUHL)ORFF & SCALMANINI <br /> A CIMNSULTING ENGINEERS <br />
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