American Journal of Water Resources
ISSN (Print): 2333-4797 ISSN (Online): 2333-4819 Website: https://www.sciepub.com/journal/ajwr Editor-in-chief: Apply for this position
Open Access
Journal Browser
Go
American Journal of Water Resources. 2024, 12(3), 77-85
DOI: 10.12691/ajwr-12-3-2
Open AccessArticle

Ground Water Potential Zone Estimation Using Vertical Electrical Sounding (VES) in Some Parts of Bundelkhand Region of Jhansi District of Uttar Pradesh, India

Som Nath1, 2, Jayant Nath Tripathi1, , V.K. Upadhyay3 and Harsh Kumar Verma4

1Department of Earth Sciences, University of Allahabad, Uttar Pradesh, India – 211002

2Department of Earth Sciences, Indian Institute of Technology, Roorkee, Uttarakhand, India- 247667

3Former Director, Ground Water Department, Government of Uttar Pradesh, Lucknow, Uttar Pradesh India – 226021

4CSIR-Central Institute of Mining and Fuel Research, Regional Research Centre, Bilaspur (CG) India – 495001

Pub. Date: August 02, 2024

Cite this paper:
Som Nath, Jayant Nath Tripathi, V.K. Upadhyay and Harsh Kumar Verma. Ground Water Potential Zone Estimation Using Vertical Electrical Sounding (VES) in Some Parts of Bundelkhand Region of Jhansi District of Uttar Pradesh, India. American Journal of Water Resources. 2024; 12(3):77-85. doi: 10.12691/ajwr-12-3-2

Abstract

This study employed Vertical Electrical Sounding (VES) surveys with the Schlumberger array configuration to identify groundwater potential zones in the Moth block of Jhansi district. Schlumberger soundings offer high resolution, depth probing, and field efficiency, which were particularly beneficial in hard rock terrains for studying weathering, fractures, and geomorphological features. Using a DDR-2 resistivity meter, the study successfully discerns water-bearing layers and assessed groundwater properties such as depth, quality, and thickness. The resistivity survey explores up to 60 m, and resistivity value ranges from 2.31 Ω.m. to 99 Ω.m within the surveyed region. The interpreted VES curves revealed that the subsurface lithology consisted of four to five resistive layers. And the results obtained from the distribution of potential zone with their lateral and vertical distribution in lithology signify the suitable depth of ground water well to fulfill demand agriculture needs. These findings are crucial for sustainable groundwater development in the moth block region for agricultural planning, as it helps in identifying suitable areas for groundwater extraction and inform the management borewell depth. Consequently, this plays a key role in sustainable agricultural development in regions with varying geological characteristics. Keywords: Groundwater potential, Vertical Electrical Sounding (VES), Resistivity, Jhansi.

Keywords:
Groundwater potential Vertical Electrical Sounding (VES) Resistivity Jhansi Bundelkhand region

Creative CommonsThis work is licensed under a Creative Commons Attribution 4.0 International License. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/

References:

[1]  Agarwal, R., & Garg, P. K. (2016). Remote Sensing and GIS Based Groundwater Potential & Recharge Zones Mapping Using Multi-Criteria Decision Making Technique. Water Resources Management, 30(1), 243–260.
 
[2]  Mondal, P., & Dalai, A. K. (2017). Sustainable Utilization of Natural Resources (Prasenjit Mondal & A. K. Dalai (eds.)). CRC Press.
 
[3]  Bhattarai, N., Pollack, A., Lobell, D. B., Fishman, R., Singh, B., Dar, A., & Jain, M. (2021). The impact of groundwater depletion on agricultural production in India. Environmental Research Letters, 16(8), 085003.
 
[4]  Kuchimanchi, B. R., Ripoll-Bosch, R., Steenstra, F. A., Thomas, R., & Oosting, S. J. (2023). The impact of intensive farming systems on groundwater availability in dryland environments: A watershed level study from Telangana, India. Current Research in Environmental Sustainability, 5, 100198.
 
[5]  Singh, A. K., Raj, B., Tiwari, A. K., & Mahato, M. K. (2013). Evaluation of hydrogeochemical processes and groundwater quality in the Jhansi district of Bundelkhand region, India. Environmental Earth Sciences, 70(3), 1225–1247.
 
[6]  Panda, D. K., & Wahr, J. (2016). Spatiotemporal evolution of water storage changes in <scp>I</scp> ndia from the updated <scp>GRACE</scp> ‐derived gravity records. Water Resources Research, 52(1), 135–149.
 
[7]  Jahan, A., Khan, M. U., Rai, N., Kumar, S., & Ali Dar, T. (2023). Geochemical characterization, its controlling factors, and comparison between the upstream and downstream segments of the Himalayan Satluj River basin, India. Geochemistry, 83(2), 125974.
 
[8]  Selvam, S., Magesh, N. S., Chidambaram, S., Rajamanickam, M., & Sashikkumar, M. C. (2015). A GIS based identification of groundwater recharge potential zones using RS and IF technique: a case study in Ottapidaram taluk, Tuticorin district, Tamil Nadu. Environmental Earth Sciences, 73(7), 3785–3799.
 
[9]  Kumar, D. V., & Ramadass, G. (2015). Vertical Electrical Soundings for Locating Groundwater Potential Zones in Osmania University Campus, Hyderabad, Telangana State, India. Journal of Experimental Sciences, 6.
 
[10]  Banks, D. (1998). Predicting the Probability Distribution of Yield from Multiple Boreholes in Crystalline Bedrock. Groundwater, 36(2), 269–274.
 
[11]  Barton, C. C. (1994). Characterizing bedrock fractures in outcrop for studies of ground-water hydrology: An example from Mirror Lake, Grafton County, New Hampshire. In In US Geological Survey Toxic Substances Hydrology Program—Proceedings of the Technical Meeting (pp. 81–87).
 
[12]  Majumdar, R. ., Majumdar, N., & Mukherjee, A. . (2000). Geoelectric investigations in Bakreswar geothermal area, West Bengal, India. Journal of Applied Geophysics, 45(3), 187–202.
 
[13]  Pal, S. K., & Majumdar, R. K. (2001). Determination of ground water potential zones using iso-resistivity maps in alluvial areas of Munger district, Bihar. Indian Jour. Earth Sci, 14, 16–26.
 
[14]  Singh, V. B., & Tripathi, J. N. (2009). An investigation of groundwater condition using geoelectrical resistivity method: A case study from some parts of Kaushambi district (UP) India. Journal of Spatial Hydrology, 9(2), 20-28.
 
[15]  Stewart, M., Layton, M., & Lizanec, T. (1983). Application of Resistivity Surveys to Regional Hydrogeologic Reconnaissance. Groundwater, 21(1), 42–48.
 
[16]  Yadav, G. S., & Abolfazli, H. (1998). Geoelectrical soundings and their relationship to hydraulic parameters in semiarid regions of Jalore, northwestern India. Journal of Applied Geophysics, 39(1), 35–51.
 
[17]  Bhattacharya, P. K., & Patra, H. P. (1968). Direct current geoelectric sounding, Elsevier: Amesterdam.
 
[18]  Riwayat, A. I., Ahmad Nazri, M. A., & Zainal Abidin, M. H. (2018). Application of Electrical Resistivity Method (ERM) in Groundwater Exploration. Journal of Physics: Conference Series, 995, 012094.
 
[19]  Vasantrao, B. M., Bhaskarrao, P. J., Mukund, B. A., Baburao, G. R., & Narayan, P. S. (2017). Comparative study of Wenner and Schlumberger electrical resistivity method for groundwater investigation: a case study from Dhule district (M.S.), India. Applied Water Science, 7(8), 4321–4340.
 
[20]  Schwarz, S. D. (1988). Application Of Geophysical Methods To Groundwater Exploration In The Rolt River Basin, Washington State. 1st EEGS Symposium on the Application of Geophysics to Engineering and Environmental Problems, cp-214.
 
[21]  Lucius, J. E., Bisdorf, R. J., & Abraham, J. D. (2001). Results of electrical surveys near Red River, New Mexico. US Department of the Interior, US Geological Survey.
 
[22]  Singh, V. B., & Tripathi, J. N. (2016). Identification of Critical Water Quality Parameters Derived from Principal Component Analysis: Case Study from NOIDA Area in India. American Journal of Water Resources, 2016, Vol. 4, No. 6, 121-129.
 
[23]  Akhtar, N., Syakir Ishak, M. I., Bhawani, S. A., & Umar, K. (2021). Various Natural and Anthropogenic Factors Responsible for Water Quality Degradation: A Review. Water, 13(19), 2660.
 
[24]  CGWB. (2017). Aquifer Maps and Ground Water Management Plan of Jhansi District, Uttar Pradesh. NAQUIM District Reports of Uttar Pradesh.
 
[25]  Octova, A., Muji, A. S., Raeis, M., & Putra, R. R. (2019). Identification of Aquifer using Geoelectrical Resistivity Method with Schlumberger Array in Koto Panjang Area, Nagari Tigo Jangko, Lintau Buo Sub-District, Tanah Datar Regency. Journal of Physics: Conference Series, 1185(1), 12009.
 
[26]  Octova, A., & Sule, R. (2018). Seismic Travel Time Tomography in Modeling Low Velocity Anomalies between the Boreholes. IOP Conference Series: Materials Science and Engineering, 335(1), 12056.
 
[27]  Basu, A. K. (1986). Geology of parts of the Bundelkhand Granite Massif, Central India Geological Survey of India Special Publication. 117, 61–124.
 
[28]  Akhtar, N., & Rai, S. P. (2019). Physico-chemical analysis of ground water for irrigation and drinking purposes around moth block of Jhansi District, Uttar Pradesh, India. Indian Journal of Ecology, 46(2), 260–269.
 
[29]  CGWB. (2009). Methodology for assessment of development potential of deeper aquifers, Central Ground Water Board, Ministry of Water Resources. River Development and Ganga Rejuvenation.
 
[30]  CGWB. (2017a). Aquifer mapping and ground water management plan, Jhansi District, Uttar Pradesh, Central Ground Water Board, Ministry of Water Resources, River Development and Ganga Rejuvenation, Government of India, Northern Region, Lucknow.
 
[31]  CGWB. (2017b). Dynamic Groundwater Resources of India, as on 31 March 2013, Central Ground Water Board, Ministry of Water Resources. River Development and Ganga Rejuvenation. Government of India, Faridabad.
 
[32]  Sonar, M. A., Tribhuvan, P. R., & Malik, M. A. (2018). Aquifer Characteristics in Hard Rock Terrain of GP-8 Watershed, Aurangabad District, Maharashtra Using Vertical Electrical Sounding Method. Journal of Geosciences, 3(2), 153–162.
 
[33]  Gupta, G., Erram, V., & Maiti, S. (2015). Geoelectrical investigation for potential groundwater zones in parts of Ratnagiri and Kolhapur districts, Maharashtra. The Journal of Indian Geophysical Union, 19(1), 27–38.
 
[34]  Ratnakumari, Y., Rai, S. N., Thiagarajan, S., & Kumar, D. (2012). 2D Electrical resistivity imaging for delineation of deeper aquifers in a part of the Chandrabhaga river basin, Nagpur District, Maharashtra, India. Current Science, 61–69.
 
[35]  Singhal, B. B. S. (1997). Hydrogeological characteristics of Deccan trap formations of India. IAHS PUBLICATION, 241, 75–80.
 
[36]  Tarawneh, M., & Janardhana, M. R. (2017). Integrated approach of field and geophysical methods for the investigations of subsurface geology and potential sites for the artificial groundwater recharge in the NW part of Jordan. International Journal of Multidisciplinary Research and Development, 4(2), 1–11.
 
[37]  Koefoed, O. (1979). Geosounding principles, 1. Resistivity sounding measurements.
 
[38]  Loke, M. H., Rucker, D. F., Chambers, J. E., Wilkinson, P. B., & Kuras, O. (2020). Electrical resistivity surveys and data interpretation. In Encyclopedia of solid earth geophysics (pp. 1–6). Springer.
 
[39]  Orellana, E., & Mooney, H. M. (1972). Two and three layer master curves and auxiliary point diagrams for vertical electrical sounding using Wenner arrangement. (No Title).
 
[40]  Andrade, R. (2014). Delineation of Fractured Aquifer Using Numerical Analysis (Factor) of Resistivity Data in a Granite Terrain. International Journal of Geophysics, 2014, 1–8.
 
[41]  Roy, I. G. (1999). An efficient non‐linear least‐squares 1D inversion scheme for resistivity and IP sounding data. Geophysical Prospecting, 47(4), 527–550.
 
[42]  GSI. (2023). Bhukosh. https://bhukosh.gsi.gov.in/Bhukosh/Public.