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Surface Water Quality Sample Handling, Preservation, and Analysis <br /> Surface water quality samples are collected by grab sampling or using a depth integrated <br /> sampler. Table 15-4 indicates the sample type, preservative, and bottle type necessary <br /> for analysis of the particular constituents shown. Raw and/or raw acidified water samples <br /> are taken from the sampling site and placed into specially prepared sample bottles. <br /> Portions of the raw samples to be field-filtered are forced through a 0.45 micron membrane <br /> using a skougstad type plastic barrel filter. The water samples are chilled by packing in <br /> ice and taken as rapidly as possible to Peabody's present contract laboratory (ACZ <br /> Laboratories, Steamboat Springs, Colorado). Laboratory procedures are consistent with <br /> those outlined in the U.S. Environmental Protection Agency's Manual Methods for Chemical <br /> Analysis of Water and Wastes (1983). <br /> All surface water samples are field tested for pH, temperature, and conductivity at the <br /> time they are collected. On an annual basis field equipment is tested for accuracy. The <br /> field equipment used for sampling conductivity, salinity and temperature at the Nucla Mine <br /> and the Nucla East mining area (YSI conductivity meter) was last tested for accuracy on <br /> December 10, 1987. The testing was performed by comparing the Nucla conductivity meter <br /> against an identical (previously calibrated) meter used for similar measurements at <br /> Peabody's Seneca Mine in northern Colorado. Both meters were used to measure the <br /> conductivity and temperature of tap water. The Seneca meter measured the water as 380 <br /> umhos at 10°C, while the Nucla meter registered readings of 360 umhos at 10°C. <br /> Temperature readings for both meters were identical, and the Nucla conductivity meter <br /> measured the conductivity of the water within 5.3 percent of the Seneca meter. <br /> The Seneca conductivity meter was calibrated on July 31, 1987. The calibration was <br /> performed by measuring the conductivity of a 0.01 demal potassium chloride (KC1) solution <br /> at 210C (YSI, 1979). Based on the conductivity table for this solution at 210C (YSI, <br /> 1979), the theoretical conductivity should be 1300 umhos. The Seneca meter registered a <br /> conductivity of 1300 umhos at 21°C for the prepared solution, which indicated accurate <br /> calibration of the Seneca conductivity meter. <br /> The pH meter used to measure field-determined pH values at the Nucla Mine and Nucla East <br /> mining area is calibrated by performing two point calibrations prior to each daily round <br /> of monitoring activities and one point calibration prior to each measurement using buffer <br /> solutions of known pH values obtained from outside laboratories. Three buffer solutions <br /> 15-7 Revised 04/11/88 <br />