Formation of chemical composition of drainage waters of Korshunovskoye iron ore deposit
Abstract
One of the main reasons for changes in the chemical composition of groundwater during drainage of developed deposits is the intensification of the overflow of pressure, more mineralized water of deep horizons, or squeezing (due to the growth of intra-class stresses) pore water from weakly permeable layers and blocks with a general decrease in head in the upper aquifers.
Область исследования:
(Archived) Without section
References
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