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Piece 2 - Hydrodynamic properties


How does water actually move through the fractured layer?


A fractured aquifer is not simply a porous medium with a few fractures.

At Maheshwaram, hydraulic tests at different scales were used to characterize the fractured-weathered layer. Slug tests, injection tests and pumping tests were interpreted using analytical approaches including double-porosity, anisotropic and fractional-flow models.

Key findings

  • Strong vertical anisotropy of hydraulic conductivity, with an average ratio close to 10.
  • Horizontal fractures play a major role in groundwater flow.
  • Fracture-network conductivity was estimated at approximately
    2.1×10−52.1\times10^{-5} m/s.
  • Block conductivity was approximately
    5.1×10−85.1\times10^{-8} m/s.
  • Thus, the fracture network is roughly 400 times more conductive than the blocks.
  • Effective porosity was estimated at 6.3×10−36.3\times10^{-3}.
  • Approximately 90% of storage was associated with the primary fracture network affecting the rock blocks, while the larger-scale secondary fracture network contributed about 10%.

Fractures control transmissivity, while smaller-scale fracture networks contribute substantially to groundwater storage.

Key publications



An Observatory of Groundwater in Crystalline Rock Aquifers Exposed to a changing Environment : Hyderabad, India


Jean-Christophe Marechal, Adrien Selles, Benoit Dewandel, Alexandre Boisson, Jerome Perrin, Shakeel Ahmed

Vadose Zone Journal, vol. 17, 2018 Nov




Determining the vertical evolution of hydrodynamic parameters in weathered and fractured south Indian crystalline-rock aquifers: insights from a study on an instrumented site


Alexandre Boisson, Nicolas Guihéneuf, Jérôme Perrin, Olivier Bour, Benoit Dewandel, Amélie Dausse, Mathieu Viossanges, Shakeel Ahmed, Jean-Christophe Maréchal

Hydrogeology Journal, vol. 23, 2015 Jun, pp. 757--773




Groundwater flows in weathered crystalline rocks: Impact of piezometric variations and depth-dependent fracture connectivity


Nicolas Guihéneuf, Alexandre Boisson, Olivier Bour, Benoit Dewandel, Jerome Perrin, A.mélie Dausse, Matthieu Viossanges, Shandra Chandra, Shakeel Ahmed, Jean-Christophe Maréchal

Journal of Hydrology, vol. 511, 2014, pp. 320-334




Estimating aquifer thickness using multiple pumping tests


Jean-Christophe Maréchal, Jean-Michel Vouillamoz, M S Mohan Kumar, Benoit Dewandel

Hydrogeology Journal, vol. 18, 2010, pp. 1787--1796




A generalized 3D geological and hydrogeological conceptual model of granite aquifers controlled by single or multiphase weathering


Benoit Dewandel, Patrick Lachassagne, Robert Wyns, Jean-Christophe Maréchal, N.S. S. Krishnamurthy

Journal of Hydrology, vol. 330, 2006 Oct, pp. 260--284




Vertical anisotropy of hydraulic conductivity in the fissured layer of hard-rock aquifers due to the geological patterns of weathering profiles


Jean-Christophe Maréchal, Robert Wyns, Patrick Lachassagne, K Subrahmanyam

Journal of the Geological Society of India, vol. 63, 2004, pp. 545--550




Use of hydraulic tests at different scales to characterize fracture network properties in the weathered-fractured layer of a hard rock aquifer


Jean-Christophe Marechal, Benoit Dewandel, K Subrahmanyam

Water Resources Research, vol. 40, 2004 Nov




Vertical anisotropy of hydraulic conductivity in fissured layer of hard-rock aquifers due to the geological structure of weathering profiles


Jean-Christophe Maréchal, Robert Wyns, Patrick Lachassagne, K Subrahmanyam, Frédéric Touchard

Comptes Rendus Geoscience, vol. 335, 2003, pp. 451--460

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