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West Elk Mine 2011 Annual Hydrology Report 40 <br />in the well is measured to the nearest 0.01 -foot, using a Solinst or Heron brand electronic <br />well sounder. The static water level is always recorded as the distance below the top of <br />the inside well casing (btoc), unless otherwise specified. Water samples are collected <br />from the groundwater monitoring wells with a point source bailer. A point source bailer <br />is lowered to a selected depth in the well (usually the center of the screened interval) in <br />order to collect an undisturbed sample from that zone. The monitored wells are not <br />bailed prior to sampling because of their very slow recharge rates. Field water quality <br />parameters are recorded and water samples are processed and sent to the certified <br />laboratory for analysis, as described above. <br />The underdrain monitoring program protocols include measuring and recording <br />flow and field water quality (pH, EC, and temperature), and collecting laboratory samples <br />for analysis. Flow rates are measured using the timed volumetric method described <br />above. The protocols for recording field water quality and processing the underdrain <br />samples for laboratory analysis are the same as described above for surface water <br />monitoring. <br />The temperature monitoring program protocols include monthly visits to the data <br />logger monitoring stations to verify that the loggers are functioning properly, to <br />download data, and to ensure that the loggers are submerged and in the shade when <br />possible. The temperature data loggers are downloaded to a laptop computer on a <br />monthly basis, except when access is prevented by excessive ice or by dangerously high <br />flows. <br />June 2012 HydroGeo, Inc. <br />