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<br />2.05-78 Rev. 11/96- PR07; 04/06-PR10; 12/14- TR136, 04/24 – TR153 <br />aerated spring flow. Care is taken to minimize any increases in turbidity. Sample bottles are <br />capped, labelled, placed on ice, and transported to the laboratory for analysis. <br /> <br /> Typical Hydrologic Sampling Methods-Ground Water <br /> <br />Ground water monitoring wells are measured seasonally as described on page 2.05-75. Monitoring <br />measurements include field and laboratory parameters as identified in Table 5. Static water levels <br />are measured first at each well. In obtaining samples from ground water wells, the field technician <br />samples each well the same way each time. In general, the ground water wells at West Elk do not <br />exhibit recovery within the time necessary to complete sampling. For this reason, as explained <br />during the 1993 permit renewal, three casing volumes of water are not removed from the wells. A <br />PVC thief with a brass foot valve is used to obtain samples. The bailer is rinsed with distilled water <br />before and after each sample. After rinsing, the bailer is gently lowered into the water column in the <br />well. The sample is obtained, striving to disturb the well water column as little as possible during <br />sampling and retrieval. Prior to measurement, instruments and equipment (filters and instruments) <br />are rinsed with distilled water. Field parameters are measured (Table 5) and the water sample is <br />filtered, divided into the proper sample bottles, sealed, cooled as appropriate, boxed, and delivered <br />to the laboratory for analysis. In some cases, samples may not be available since there is <br />insufficient water for sampling. This means that there is not enough water to fill the sample bottles <br />and an additional 300 to 500 ml of sample for rinsing and field parameter measurement. <br /> <br /> Typical Hydrologic Sampling Methods-Mine Inflows <br /> <br />Flow measurements, field parameters and a water quality sample will be collected from mine inflow <br />locations as close to the inflow source as safely possible. Flow estimates will be recorded for the <br />inflows that are expressed as roof drippers, seeps, or dispersed flow that are less than 5 gpm. Field <br />parameters and a water quality sample will be obtained if the inflow is of sufficient, discernable <br />flow (>5 gpm) and/or lasts longer than 7 days. If the inflow is continuous, an initial sample will be <br />obtained, and then sampled at least annually thereafter. Because the location and conditions of the <br />inflows will vary, as they will originate from the roof, floor, or ribs and may be flowing at a very <br />low or high rate, it is difficult to describe how information on each inflow will be collected. To the <br />extent possible, flow measurements will be taken through the use of a timed volume approach as <br />close to the source of the inflow as possible. The sampler will time the flow into a specific measured <br />volume container to establish flow rate. Several measurements will be taken and averaged prior to <br />reporting. Field parameters of temperature, pH, and conductivity will be procured as close to the <br />inflow source as possible by selecting a sample volume from the inflow and measuring the sample <br />for the parameters using standard instruments which have been calibrated. Samples for analysis of <br />laboratory parameters per Table 5 will be collected by filling a clean, pre-fixed sample bottle from <br />non-aerated flow. Sample bottles will be capped, labeled, placed on ice, and transported to the <br />laboratory for analysis. If the sampler is unable to obtain a sample following the above described <br />methods due to conditions in the mine or if the inflow is of very high volume and/or flow, the <br />sampler will attempt to obtain the most accurate measurement of flow and as representative water <br />quality sample, as safely possible. <br /> <br /> Monitoring Mining Impacts-Surface Water <br />