A methodology for regionalizing 3‐D effective porosity at watershed scale in crystalline aquifers. Issue 12 (9th May 2017)

• Record Type: Journal Article
• Authors: Dewandel, Benoît; Caballero, Yvan; Perrin, Jérôme; Boisson, Alexandre; Dazin, Fabrice; Ferrant, Sylvain; Chandra, Subash; Maréchal, Jean‐Christophe
• Is Part Of: Hydrological processes. Volume 31:Issue 12(2017)
• Page Start: 2277
• Page End: 2295
• Publication Date: 2017-05-09
• Subjects: crystalline aquifer -- effective porosity -- hard rock aquifer -- regionalization of aquifer parameters -- upscaling; Hydrology -- Periodicals; Hydrology -- Research -- Periodicals; Hydrologic models -- Periodicals; Hydrological forecasting -- Periodicals; 631.432
• DOI: 10.1002/hyp.11187
• Languages: English
• ISSNs: 0885-6087

Abstract

Abstract: An innovative approach for regionalizing the 3‐D effective porosity field is presented and applied to two large, overexploited, and deeply weathered crystalline aquifers located in southern India. The method derives from earlier work on regionalizing a 2‐D effective porosity field in that part of an aquifer where the water table fluctuates, which is now extended over the entire aquifer using a 3‐D approach. A method based on geological and geophysical surveys has also been developed for mapping the weathering profile layers (saprolite and fractured layers). The method for regionalizing 3‐D effective porosity combines water table fluctuation and groundwater budget techniques at various cell sizes with the use of satellite‐based data (for groundwater abstraction), the structure of the weathering profile, and geostatistical techniques. The approach is presented in detail for the Kudaliar watershed (983 km 2 ) and tested on the 730 km 2 Anantapur watershed. At watershed scale, the effective porosity of the aquifer ranges from 0.5% to 2% in Kudaliar and between 0.3% and 1% in Anantapur, which agrees with earlier works. Results show that (a) depending on the geology and on the structure of the weathering profile, the vertical distribution of effective porosity can be very different and that the fractured layers in crystalline aquifers are not necessarily characterized by a rapid decrease in effective porosity and (b) that the lateral variations in effective porosity can be larger than the vertical ones. These variations suggest that within a same weathering profile, the density of open fractures and/or degree of weathering in the fractured zone may significantly vary from a place to another. The proposed method provides information on the spatial distribution of effective porosity that is of prime interest in terms of flux and contaminant transport in crystalline aquifers. Implications for mapping groundwater storage and scarcity are also discussed, which should help in improving groundwater resource management strategies.