Method of calculation of water intakes in the weathering zone of fractured rocks
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Abstract
Until recently, when calculating water intakes laid in the weathering zone, the filtration homogeneity of fractured rock massifs was assumed; the decrease of their water permeability with depth was not taken into account, which led to inevitable errors. L.V. Borevsky proposed a method of calculating the water inflow to the well, based on the condition that the rock filtration coefficient in the weathering zone decreases with depth according to a linear law. It has allowed to specify considerably calculations of water intakes.
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References
- Borevsky L. V. Determination of calculated hydrogeologic parameters of aquifers of the weathering zone. Exploration and Protection of Subsoil, No. 3, 1966.
- Chernyshev S. N. About water permeability of fractured rocks in the zone of unloading and weathering. Bulletin. Moscow Society for Nature Research, Geol. department, vol. 40, No. 4, 1965.
- Yarpev N.A. About fracturing and karst formation of carbonate strata of the Saksagan area. Proc.. Lengidroproekt, vol. 4. 1966.
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