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Kennedy/Jenks Consultants <br /> Mr. Timothy O'Brien <br /> California Regional Water Quality Control Board <br /> 10 March 2005 <br /> Page 3 <br /> the conceptual hydraulic modeling of the river and groundwater system (Darcy flux model)will <br /> be included in the Groundwater Characterization Report. <br /> Item 2 — Pond Level Gauge <br /> Pond level gauges were installed in all four process water ponds several years ago. The water <br /> level readings are reported monthly to the CRWQCB. These level readings will be used for the <br /> Groundwater Characterization Work Plan. <br /> Item 3 — Production Wells <br /> It is important to collect as much readily available data as possible, which is why the production <br /> wells were included. Data from these wells can be used to generate an overall picture of the <br /> groundwater status in the area. Also, some of the production wells may draw from aquifers of <br /> concern. If the data from the production wells does not correlate well with the data from the <br /> monitoring wells, then we will not use the data from the production wells in our analysis of <br /> groundwater monitoring well data. <br /> Item 4 — CPT/HydropunchTM Study <br /> The proposed location of Cone Penetrometer Test 01 (CPT-01) has been moved westward, so <br /> that it is not directly downgradient of the ponds (See Revised Figure 2). The proposed location <br /> of CPT-03 has been moved farther north to move it farther from the ponds. The location of the <br /> ponds and nearby Block A and the East Block limit the degree to which CPT-03 location can be <br /> shifted. <br /> Item 5 — Measurement of Groundwater Elevations <br /> The approximate depth of groundwater can be derived from a pore-pressure dissipation test. <br /> This test is conducted by halting the CPT cone at a specified depth and measuring the variation <br /> of the penetration pore pressure with time. The cone is held at a specific depth and the pore <br /> pressure is monitored until no further change in pore pressure is observed. The depth to <br /> groundwater is a function of this equilibrium pore pressure, the unit weight of water, and the <br /> depth of the cone. <br /> The groundwater depths at the CPT locations will be estimated using this method, and this <br /> information will be used in conjunction with the groundwater elevation data from the monitoring <br /> wells to augment the groundwater gradient analysis. The groundwater depth estimates which <br /> are derived from the CPT data will not be used solely to derive the groundwater gradient. <br /> Item 6 — Mixing of Groundwater <br /> Groundwater samples are collected using a HydropunchTM or equivalent method. In this <br /> method, steel sampling rods with a sacrificial cone at the end are pushed down to the desired <br /> depth. PVC casing and screen are then inserted into the steel rods, the rods are retracted by a <br /> p:cs grmpAad"ntiDbW=0123.W�dmVkoMnd%g"wp Wa fmduml.o <br />