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Jonas & Associates Inc <br /> ' screened portion of the well was then backfilled with filter pack As the filter pack <br /> was placed, the augers were withdrawn from the hole so the sand would flow out of <br /> the augers and fill the annular space of the borehole The filter pack extended to <br /> approximately 1 foot above the top of the well screen A I-foot seal of bentonite <br /> pellets was placed in the annular space above the filter pack Since the bentonite <br /> seal was above the water table, approximately 3 gallons of potable water were added <br /> ' to allow swelling of the bentonite After sufficient time had passed for the bentonite <br /> to swell (at least 1 hour), the remaining annular space was backfilled to the surface <br /> ' with a cement-bentonite grout Representatives of the San Joaquin County <br /> Environmental Health Department were onsite to inspect and approve the grouting <br /> of each well (PG&E, 1988) <br /> ' Each well was finished with a tamper-resistant, watertight street box set into <br /> concrete The street boxes were set slightly above the existing ground surface to <br /> provide additional protection against infiltration of surface water A threaded water- <br /> tight cap with a cork liner (2-inch wells) or rubber clamp-on cap (4-inch wells) was <br /> placed over the end of each well casing inside the street box (PG&E, 1988) <br /> ' Each well was developed by surging with a surge block and pumping with a <br /> centrifugal pump Due to the fine texture of the soil material surrounding the wells, <br /> none of the wells produced clear water, even after extensive developing However, <br /> turbidity was reduced significantly in all wells With the exception of well OW-2, all <br /> wells produced water continuously throughout the development process Well OW-2 <br /> t was pumped dry twice during development Development water from each well was <br /> retained in labeled drums pending chemical analysis and appropriate disposal <br /> (PG&E, 1988) <br /> ' Wells were located a sufficient distance from one another to allow determination of <br /> the groundwater gradient and flow direction through analysis of water level data <br /> ' collected from these wells The top of casing of each well was surveyed to the <br /> nearest 0 01 foot to allow comparison of water elevations The depth to water from <br /> the top of the well casing was measured with an electronic emersion probe The <br /> ' water elevation in each well was computed by subtracting the depth to water from <br /> the elevation at the top of the well casing This procedure was repeated on several <br /> occasions from January 1988 to November 1995, in an effort to observe any <br /> fluctuations in groundwater flow direction and gradient (PG&E, 1988) <br /> 2 3 2 Groundwater Sampling Methodology <br /> ' Prior to purging and sampling each well, the depth to water was measured and <br /> recorded An acrylic bailer was then used to collect a sample from the water surface <br /> 5 <br /> t <br />