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<br />,,~ . '=! ,~ <br />-' _'... v.... J <br /> <br />.. <br /> <br />Precipitation-Chemistry Data at Selected Sites in <br />Northwestern Colorado, 1980-94 <br /> <br />By Anthony J, Ranalli <br /> <br />Abstract <br /> <br />The chemical content of precipitation was <br />monitored during the period 1980--94 at three <br />sites at altitudes above 2,400 meters near the <br />Piceance Basin in northwestern Colorado, Daily <br />precipitation volumes, specific conductance, pH <br />(in this report pH is expressed as hydrogen-ion <br />concentration), concentrations of major cations <br />and anions, calculated charge balance between <br />cations and anions, and summary statistics of <br />chemical concentrations are tabulated, Sampling <br />sites are plotted on a map of the area, Seasonal <br />variabilities of major cation and anion concentra- <br />tions are presented graphically, <br /> <br />INTRODUCTION <br /> <br />Knowledge of the chemistry of precipitation is <br />needed in the preparation of permit requests for new <br />sources of emissions to the atmosphere and for review <br />of these requests, One area in which data may be <br />needed is northwestern Colorado. Energy resources, <br />such as oil shale and coal, are upwind from the <br />federally protected Flat Tops Wilderness Area, which <br />is sensitive to acid rain (Turk and Adams. 1983). The <br />lack of precipitation-chemistry data in northwestern <br />Colorado partially was addressed by establishment of <br />a network of monitoring sites as part of a study done <br />by the U,S. Geological Survey, in cooperation with <br />Delta, Mesa, and Rio Blanco Counties, and assisted by <br />the Rocky Mountain Oil and Gas Association. The <br />network is located near the oil shale reserves of the <br />Piceance Basin. Data collected from these sites <br />provide a baseline for ambient atmospheric deposition <br />that could be compared to any future measurements, <br />The data also are suitable for making estimates of <br /> <br />natural variability in precipitation chemistry. This <br />report presents data collected at the monitoring sites <br />from 1980 to 1994 and includes site location, <br />sampling and laboratory analytical methods, precipita- <br />tion volume and summary statistics, and seasonal <br />variability,of major chemical constituents. <br /> <br />Site Description <br /> <br />The three precipitation-monitoring sites <br />(fig. I) are located at Douglas Pass at an altitude of <br />2,710 meters in a treeless area of sage; at Grand Mesa, <br />at an altitude of3,I21 meters in a clearing; and at <br />Marvine Ranch, at an altitude of 2,414 meters in a <br />clearing. <br /> <br />'I <br /> <br />:1 <br /> <br />Methods <br /> <br />Precipitation volume and chemistry have been <br />monitored at Douglas Pass since November 1980, at <br />Grand Mesa since August 1981, and at Marvine Ranch <br />since April 1981. Data collection was discontinued at <br />Douglas Pass and Grand Mesa in October 1991 but is <br />ongoing at Marvine Ranch, The sampling equipment <br />and analytical methods are the same at each site. The <br />sampling intervals, however, varied at each site. The <br />sampling equipment consisted of a Belfort weighing- <br />bucket rain gage for the measurement of precipitation <br />volume and an Aerochem Metrics Model 301 wet/dry <br />collector for the monitoring of wet deposition, The <br />samples collected at each site are a combination of <br />single storms and two or more storms collected into a <br />single sample, Unfiltered precipitation samples were <br />analyzed for specific conductance, pH, dissolved <br />calcium, magnesium, sodium, potassium, ammonium, <br />chloride, nitrate, and sulfate by the U,S, Geological <br />Survey National Water-Quality Laboratory in Arvada, <br /> <br />;1 <br /> <br />I <br />" <br /> <br />;"i <br /> <br /><:, <br /> <br />..' <br />I <br /> <br />INTRODUCTION 1 <br />