An Introduction to Mine Hydrogeology by Pradipta Kumar Deb PDF

By Pradipta Kumar Deb

ISBN-10: 3319029878

ISBN-13: 9783319029870

ISBN-10: 3319029886

ISBN-13: 9783319029887

An creation to Mine Hydrogeology briefly describes the topic of hydrogeology in order that this information may be built-in into mine improvement making plans. It emphasizes not just the hydrochemical but additionally the actual affects of the hydrogeological surroundings at the mine and its atmosphere. additional, it discusses the methodologies utilized in mine hydrogeological reviews, showcased by means of chosen reports on Indian mines.

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Hydrogeology of Karstic limestone differs widely from the alluvium deposits and the sedimentary rocks on the one hand and the igneous and metamorphic rocks on the other, as it has neither primary porosity of sediments nor the fracture porosity of the effusive rocks. It has thus only secondary porosity and permeability developed essentially as a result of Karstification. Karstification is, therefore responsible for location and movement of both the confined and unconfined ground water bodies. In the unconfined aquifer naturally the first bench of Karstification is one involved below water table.

Hydrogeology of Karstic limestone differs widely from the alluvium deposits and the sedimentary rocks on the one hand and the igneous and metamorphic rocks on the other, as it has neither primary porosity of sediments nor the fracture porosity of the effusive rocks. It has thus only secondary porosity and permeability developed essentially as a result of Karstification. Karstification is, therefore responsible for location and movement of both the confined and unconfined ground water bodies. In the unconfined aquifer naturally the first bench of Karstification is one involved below water table.

Bench height and number of working benches are also required to be known. Thus, if possible, bench-wise quantum of groundwater seepages should be computed in advance, which calls for integration of hydrogeological study with the mine development planning (Deb 1987). In order to fulfill water demand of the mining colonies and process plant/s, groundwater exploration is carried out through pumping tests (APT) on the exploratory wells so that aquifer parameters like coefficient of Transmissibility (T), Storage Co-efficient (s) and coefficient of permeability can be determined.

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