Sources of Salinity Near a Coal Mine Spoil Pile, North-Central Colorado
Robert A. Zielinski*,a,
James K. Ottonb and
Craig A. Johnsonc
a U.S. Geological Survey, Mail Stop 973, Denver Federal Center, Denver, CO 80225
b USGS, Mail Stop 939, Denver Federal Center, Denver, CO 80225
c USGS, Mail Stop 963, Denver Federal Center, Denver, CO 80225

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Fig. 2. Map of the study site showing locations of water (W) and auger (A) samples.
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Fig. 3. Triangular plots showing the relative proportions of the major cations and anions in surface waters, mine spoil leachates, and saline soil leachates.
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Fig. 4. Calculated saturation indices of selected mineral phases in nine samples of surface water (W1W9) collected at progressive distances downstream from the cattail wetland below the coal spoil pile. Positive values of saturation index (log of ion activity product/equilibrium constant) indicate oversaturation with respect to a particular phase.
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Fig. 5. Dissolved concentrations of selected elements in surface waters W1W9, plotted as a function of distance downstream from the cattail wetland below the coal spoil pile.
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Fig. 6. Sulfur isotopic composition of total sulfur in core samples and of soluble sulfate in the spoil pile, nearby saline soil, regional soils, and surface waters W1W9.
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Copyright © 2001 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.