کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
4576079 1629944 2013 10 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Hydrogeochemical characteristics of streams with and without acid mine drainage impacts: A paired catchment study in karst geology, SW China
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات فرآیندهای سطح زمین
پیش نمایش صفحه اول مقاله
Hydrogeochemical characteristics of streams with and without acid mine drainage impacts: A paired catchment study in karst geology, SW China
چکیده انگلیسی


• A paired catchment study was used to assess karst hydrogeochemistry of two streams.
• Chemistry of streams with and without acid mine drainage (AMD) was very different.
• The observation was supported by PHREEQC modeling of equilibrium conditions.
• Ionic fluxes of AMD-impacted water were higher than that of non-AMD-impacted water.
• The higher ionic fluxes were predominantly controlled by the oxidation of pyrite.

SummaryA paired catchment study was used to assess hydrochemical characteristics of streams in AMD (acid mine drainage)-impacted and non-AMD-impacted catchments in a karstic region, SW China. The catchments shared similar geology, slope, aspect, area and climate, but different land use since one encompassed mining activities. As a result, hydrogeochemical characteristics of the AMD-impacted water were dominantly controlled by oxidation of pyrite, while that of non-AMD-impacted were influenced by water–rock reactions. It is also coincident with the source of δ34SSO4 in both waters. Upstream, unit ion fluxes of the AMD-impacted catchment for Ca, Mg, H, Fe and SO4 were 17 g/(m2 yr), 2 g/(m2 yr), 0.0002 g/(m2 yr), 17 g/(m2 yr) and 136 g/(m2 yr), respectively, while unit ion fluxes of the non-AMD-impacted catchment were much lower than that of the AMD-impacted catchment. Along the flow, fluxes of H, Ca, Mg, Fe and SO4 decreased in the AMD-impacted water, but increased in the non-AMD-impacted water. The observation was coincident with variations of ion concentrations in both waters along the flow, supported by PHREEQC modeling of minerals such as goethite, jarosite(ss), melanterite, scorodite, calcite, and dolomite. It suggests that the transport of constituents of interest (except for Ca and Mg) is dramatically different in these catchments. Results provide important information on karst system response to AMD, together with the baseline data to understand the degree and type of impairment.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Journal of Hydrology - Volume 504, 11 November 2013, Pages 115–124
نویسندگان
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