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NARROW
GeoRef Subject
-
all geography including DSDP/ODP Sites and Legs
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Africa
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West Africa
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Ghana (1)
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Animas River basin (1)
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Arctic region (1)
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Asia
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Japan
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metals
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Invertebrata
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Plantae
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Spermatophyta
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Gymnospermae
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Coniferales
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geochronology methods
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geologic age
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Cenozoic
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upper Pleistocene
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Tertiary
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Miocene
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Paleogene
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Oligocene
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Laurentide ice sheet (1)
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Mesozoic
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Cretaceous
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Lower Cretaceous
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Upper Cretaceous
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Jurassic
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Middle Jurassic (2)
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Triassic (2)
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Paleozoic
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lower Paleozoic
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Precambrian
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upper Precambrian
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Proterozoic
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Mesoproterozoic (1)
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igneous rocks
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volcanic ash (1)
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metamorphic rocks
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metamorphic rocks
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framework silicates
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Primary terms
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Africa
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Ghana (1)
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Antarctica
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Victoria Land
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Arctic region (1)
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Asia
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Far East
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China
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Inner Mongolia China (1)
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Japan
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Hokkaido (1)
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Honshu
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Kanto Plain (1)
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Tono Japan (1)
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Yamaguchi Japan (1)
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Phaeozems (3)
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Podzols (2)
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Red soils (1)
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Regosols (2)
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saline soils (2)
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Ultisols (2)
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volcanic soils (5)
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Spodosols (2)
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solute transport
Autonomous time-lapse electrical imaging for real-time management of subsurface systems
Influence of hydrostratigraphy on the distribution of groundwater arsenic in the transboundary Ganges River delta aquifer system, India and Bangladesh
The effect of filtration size on the geochemistry of groundwater samples from a massive sulfide deposit at the Bathurst Mining Camp, New Brunswick, Canada
Geochemistry of natural acid rock drainage in the Mt Evans area, Anaconda–Pintler Range, Montana, USA
Influence of Shear Displacement on Fluid Flow and Solute Transport in a 3D Rough Fracture
Experimental and Numerical Simulation Study of Flow and Solute Transport in Pore-Fractured Media Based on High-Density Resistivity Method
Abstract Mining operations disturb the natural hydrological cycle at a local scale by creating new pathways for water flow and conveying large amounts of water, both for use in ore beneficiation and through the dewatering of mining workings. Sulfide minerals exposed to water and oxygen are oxidized through chemical and microbial-enhanced reactions, significantly altering the quality of water (acid mine drainage). Stable isotopes may reveal important information concerning water origin and transfer, as well as chemical processes and solute fluxes within the aqueous environment. Several case studies illustrate the use of stable isotope techniques for clarifying aspects related to water circulation in mining areas within Romania and Finland. Hydrogen and oxygen stable isotopes coupled with total dissolved solids have been used to characterize mine water and for assessing water sources, flow paths and mixing processes at some Romanian mining sites. At Talvivaara mine in Finland, water isotopes and chemical composition were used to determine the extent of waste water contamination in groundwater systems after a leakage at gypsum ponds.