Water Productivity Journal (WPJ) Quarterly Publication

Document Type : Original Research Paper


Assistant Professor, Academy of CSIR, Scientist, CSIR-National Geophysical Research Institute, Uppal Road, Hyderabad 500 007, India



Introduction: The faults and fractures of the granite are, according to their position in relation to the plane of deformation, hypothetically interpreted as tension and shear faults. The faults in shear position are supposed to be tight and have very little groundwater. The tension faults, on the other hand, are supposed to be open and to be capable of a high yield of groundwate. The electrical conductivities of rocks and soils are highly dependent of the water saturation. Variations in electrical resistivity are monitored by time lapse electrical resistivity tomography (TLERT) during a long duration pumping test.
Rocks such as granite and schist are generally poor aquifers because they have a very low porosity. However, if these rocks are highly fractured, they make good aquifers. A well is a hole drilled into the ground to penetrate an aquifer. Normally such water must be pumped to the surface.
Material and methods: Climate of South India is mostly tropical. The study of climate is very important from many aspects. It is predominantly important for crops, tours, vegetation etc. Henceforth necessary to understand the working and eating habits, also. In fact the study of climate is correlated to Topography and Temperature of the region. In fact the region has a tropical climate and depends on monsoons for rainfall. This region includes Karnataka, inland Tamil Nadu and western Andhra Pradesh.
Most importantly it gets between 400 and 750 millimetres (15.7 and 29.5 in) of rainfall annually . The summers are hot and dry . But the winters are cool with temperatures around 20-24°C (68-75°F).
This experiment is carried out in the Experimental Hydrogeological Park (EHP) located in Choutuppal, 45 km south-east of Hyderabad. Vadose zone of EHP comprises an uppermost thin layer of red soil (<1m), sandy regolith (1m-3m), saprolite (3m-15m), and then the fissured granite. The pumping test lasts for 5 days and the piezometric variations are between 13 m and 18 m during pumping in CH03 borehole. This fissured granite is characterized by an important horizontal fracture density controlling the flow. An East West profile was laid with 48 electrodes and 3 m spacing interval. CH03, pumping well, was in the center of the profile covering 8 observation wells in both directions. 27 time-lapse datasets were inverted using Res2Dinv adopting least square inversions. The inverted resistivity datasets seem to be correlated with weathered profile and the variations of resistivity may be correlated with variation of hydraulic head. The variations of resistivity are more important close to CH03 and decreases with distance away from it. This behavior is coherent with the depression cone created by the pumping. Moreover, resistivity variations in the vadose zone highlight an influence of the pumping on the water content evolution of this zone. The observed heterogeneous response seems to be correlated with the geological media heterogeneity. TLERT appears to be a powerful tool to follow dynamic behavior of both saturated level and vadose zone for a given event. Grounwater punping monitoring helps to the water content evolution and groundwater productivity.
Results: The different distribution pattern of resistivity during and after the pumping are noticed. There is no occurrence of rainfall event during the experiment and the watershed. However, there is a temporary storage tank towards the eastern end of the profile, constructed for storing the water. This tank has no effect on the percolation, but the saturation effect is observed the surficial level. A very sharp breakup is seen after almost 40hr of pumping. This sharp boundary or may be fracture is strongly observed upto 20m depth.
Conclusion: Subsurface hydrology of the granitic terrene is studied, monitored and analyzed by a simpler approach of TLERT. The inverted resistivity datasets successfully correlates with the hydraulic head data measured at the water table at the same timings. This research, intended to examine the validity of time-lapse electrical imaging has been extremely successful, showing that repeat measurements of resistivity recorded at the surface can accurately delineate changes in saturation in the subsurface. The observed heterogeneous response seems to be correlated with the geological media heterogeneity. The precise location of a fracture can be determined with this non-invasive and quick method in the presence of significant vertical flow. Vadose zone connectivity in terms of pathways in both horizontal as well as vertical directions. It helps in reducing the uncertainty in the model parameters.


Main Subjects

Alamry Abdulmohsen, S. & et al. (2017). Spatial and temporal monitoring of soil moisture using surface electrical resistivity tomography in Mediterranean soils. Catena, 157: 388-396.
Al-Gamal, S.A. (2021). The potential impacts of climate change on groundwater management in west Africa. Water Productivity Journal, 1(3): 65-78.
Arora, T. & Shakeel, A. (2011). Characterization of recharge through complex vadose zone of a granitic aquifer by time lapse electrical resistivity tomography. Journal of Applied Geophysics, 73: 35-44.
Arora, T., Alexandre, B. & Shakeel, A. (2016). Non-intrusive Hydro-geophysical Characterization of the Unsaturated Zone of South India-A case study. Special Issue: Contributions of the Global Earth Sciences Integration. Journal of African Earth Sciences, 12(2): 88-97.
Binley, A. (2015). Tools and Techniques: Electrical Methods. Treatise on Geophysics, 11: 233-59. DOI: https://doi.org/10.1016/B978-0-444-53802-4.00192-5.
Daily, W., Ramirez, A., Labrecque, D. & Nitao, J. (1992). Electrical Resistivity Tomography Of Vadose Water Movement. Water Resources Research, 28:
Dutta, S., Krishnamurthy, N.S., Arora, T., Rao, V.A. & Shakeel, A. (2006). Localization of water bearing fractured zones in a hard rock area using integrated geophysical techniques in Andhra Pradesh, India. Hydrogeology Journal, 14(5): 760-766.
LaBrecque, D.J. & Yang, X. (2000). Difference inversion of ERT data; a fast inversion method for 3-D in-situ monitoring. Paper presented at Symposium on the Application of Geophysics to Engineering and Environmental Problems (SAGEEP), Environ. and Eng. Geophys. Soc., Arlington, Va, USA.
Seaton, W.J. & Burbey, T.J. (2002). Evaluation of two-dimensional resistivity methods in a fractured crystalline-rock terrain. Journal of Appl. Geophys, 51: 21-41.
Singha, K.F., Day-Lewis, D., Johnson, T. & Slater, L.D. (2015). Advances in interpretation of subsurface processes withtime-lapse electrical imaging. Hydrol. Process, 29: 1549-1576.
Ward, S.H. (1990). Resistivity and induced polarisation methods. In: Geotechnical and Environmental Geophysics. Vol.1, Edited by S.H. Ward, Soc. of Exp. Geophys:147-189, Tulsa, Okla, USA.
Ward, S.H. & Hohmann, G.W. (2002). Electromagnetic theory for geophysical applications. Nabighian M.N. (Ed.), Electromagnetic methods in Applied Geophysics - Theory, 1, Society of Exploration Geophysicists, 1987: 130-311.
Zhou, Q.Y., Shimada, J. & Sato, A. (2001). Three-dimensional spatial and temporal monitoring of soil water content using electrical resistivity tomography. Water Resour. Res, 37: 273-285.