By S. Ahmed, R. Jayakumar, A. Salih
This booklet comprises the consequences and findings of complex study conducted in a pilot region with an intensive research of the constitution and functioning of the aquifer in a granitic formation. some of the chapters commence from a really common state of affairs of the water assets administration, then follows a technical contribution at the demanding rock aquifer procedure, its characterization, theoretical component to its homes and behavior. for this reason a short description of assorted studies of learning not easy rock aquifers globally has been incorporated. the remainder of the booklet very systematically contains the geophysical, geological and distant sensing purposes to conceptualize such an aquifer procedure. a tremendous half covers the complicated strategies of geostatistics and aquifer modeling correct from the fundamentals tested by way of compatible case stories. ultimately a couple of examples were incorporated at the demanding rock aquifers from the extraordinary north and likewise from the south of India with case reviews to accomplish the problem.
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Additional resources for Groundwater Dynamics in Hard Rock Aquifers: Sustainable Management and Optimal Monitoring Network Design
Singhal where a is the shape factor parameter depending on fracture and matrix geometry and rw is well radius. Equivalent Porous Medium Model This is also known as equivalent continuum model. Here it is assumed that flow in a large volume of fractured medium can be similar to that of a porous medium especially when fracture density is high. In such cases conventional pumping test methods can be used. Discrete Fracture Network Models Network models use fracture characteristics and heterogeneity of rocks mass based on field data.
Several processes such as cooling stresses in the magma, subsequent tectonic activity or lithostatic decompression were invoked to explain the origin of these fissures. , 2004). Swelling of certain minerals results in a local increase of volume that favours cracks and fissuring. In granitic rocks, the most sensitive mineral to swelling is biotite. Where the rock texture is relatively isotropic (in granite for example), the generated fissures are orthogonal to the lower constraint vector (V3), and thus subparallel to the topographic surface contemporaneous with the weathering process (Fig.
5 mg/l), which is mainly due to the presence of fluoride-bearing mineral, viz apatite, fluorite, biotite and hornblende in rocks. Among other trace elements, iron and manganese are common as a result of weathering of biotite and hornblende bearing rocks. In mafic and ultramafic rocks, chromium is quite prominent. A vertical zonation in the water quality has also been reported from several crystalline rock terrains. Shallow groundwaters are usually of CaHCO3 type. , 2003). Nature of Hard Rock Aquifers: Hydrogeological Uncertainties and Ambiguities 37 The quality of groundwater in deep-seated crystalline rocks is not only of geochemical interest but is also of importance for the disposal of radioactive waste and tapping of geothermal power.