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ARCHIVED REPORTS_XR0012570
EnvironmentalHealth
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EHD Program Facility Records by Street Name
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M
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MACARTHUR
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29099
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3500 - Local Oversight Program
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PR0545462
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ARCHIVED REPORTS_XR0012570
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Entry Properties
Last modified
3/10/2020 9:14:05 AM
Creation date
3/10/2020 8:24:23 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0012570
RECORD_ID
PR0545462
PE
3528
FACILITY_ID
FA0005525
FACILITY_NAME
TEICHERT - TRACY ROCK PLANT
STREET_NUMBER
29099
Direction
S
STREET_NAME
MACARTHUR
STREET_TYPE
DR
City
TRACY
Zip
95377
APN
25312012
CURRENT_STATUS
02
SITE_LOCATION
29099 S MACARTHUR DR
P_LOCATION
99
P_DISTRICT
005
QC Status
Approved
Scanner
SJGOV\sballwahn
标签
EHD - Public
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� 3 <br /> 2 <br /> s <br /> GEOLOGY <br /> l f' <br /> The geology of the region-area is sedimentary in nature, a <br /> combination of fluvial-marine strata consisting of silts and clay <br /> facies with lenses of sand and gravelly silts and clays. <br /> S01L TYPES <br /> Soil to a depth of 28 feet was generally silt-clay with <br /> sands dispersed throughout the silt-clay matrix. Sand and gravel <br /> strata are to be found at deeper depths of 30 to 60 feet and over <br /> silty clay at 56 to 60 feet. Drilling logs were attached to the <br /> preliminary report in September 1987. <br /> GROUND WATER <br /> Ground water in the area is approximately 90+ feet deep per <br /> San Joaquin County Department of Public Works. Seasonal fluctua- <br /> tions are unknown at this time. Monitor Well No. I has a depth <br /> to ground water of 83 feet. <br /> GROUND WATER GRADIENT <br /> The ground water gradient was measured on November 8, 1987, <br /> as shown on Plate No. 4. Two existing wells, 500 gpm and 2000 <br /> _ gpm, are used daily, Monday through Friday, in aggregate and <br /> asphalt production. Measurements were made late Sunday to permit <br /> 48 hours for stabilization. Plate 3 shows the ground water <br /> gradient to be northwest at a rate of 1 foot/400 feet. <br /> The gradient as determined using these three wells generally <br /> agrees with the region ground water gradient. The local ground <br /> water gradient is probably influenced by both the 2000 gpm and <br /> the 500 gpm wells. <br /> {x <br /> E <br /> WELLS <br /> There are three (3) in3ustrial water supply wells and one <br /> domestic well on the site (se. Plate No. 3) . One is located to <br /> the northwest at a distance of approximately 900'+ feet with a <br /> capacity of 500+ G.P.M. One is located to the northeast at a <br /> distance of approximately 7501+ feet with a capacity of 2000+ <br /> G.P. F. ; draw down, for this well is one foot/100 gallons. A third <br /> 8" domestic well is located about 2301+ east of the 2000 G.P.M. <br /> well. The fourth well is located 980' northwest, has a 6" <br /> diameter, and has not been used for many years. The pump motor <br /> - - - --- has -been---removed--but -the-pump--impellers- are _wedged_ in_place__and___ <br /> can't be pulled. Ground water gradient is to the northwest at a <br /> rate of one foot/400 feet. <br /> -2- <br />
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