Chemistry of Groundwater from Two Aquifers in Liuyi Coal Mine, Northern Anhui Province, China: a Comparative Study

Lin Hua Sun; He Rong Gui

doi:10.4028/www.scientific.net/AMM.212-213.362

Paper Titles

Uncertainty Improvement in a Simulation of Channel Evolution
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High-Resolution Integrated Detection of Underwater Topography and Geomorphology Based on Multibeam Interferometric Echo Sounder
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Study on Dynamic Equilibrium of Sediment Transport by Qingshuigou Course of the Yellow River
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An Analysis on Water-Saving Potential in Central and Northern Part of Ningxia
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Chemistry of Groundwater from Two Aquifers in Liuyi Coal Mine, Northern Anhui Province, China: a Comparative Study
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Experimental Study of Sand Sediments Effects on Submerged Hydraulic Jump Properties
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Study and Application of Tidal River Flow-Sediment Mathematical Model
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Laboratory Study of Unsaturated Flow in a Single Fracture-Matrix System: A Conceptual Model
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Evaluation on the River Seepage under Groundwater Pumping near Riverside
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HomeApplied Mechanics and MaterialsApplied Mechanics and Materials Vols. 212-213Chemistry of Groundwater from Two Aquifers in...

Chemistry of Groundwater from Two Aquifers in Liuyi Coal Mine, Northern Anhui Province, China: a Comparative Study

Abstract:

Major ion concentrations of twenty groundwater samples from two deep seated aquifers (coal bearing-GC and limestone-LC) are analyzed for identify the differences between them and the source of ions. The results suggest that they are moderate to highly mineralized water with their average TDS values are 2444 (GC) and 1178 (LC) mg/L. LCs show lower Na but much higher Ca and Mg concentrations relative to GCs. Saturation indexes and principle component analysis, as well as mole ratios between Na and Cl, Ca and SO4, Ca and HCO3 indicate that they have multi sources with incorporation of halite and albite for Na, calcite, dolomite and gypsum for Ca, pyrite and gypsum for SO4.