Abstract

Among the distinguished zones of geothermal potential in India, the Puga Valley is identified as one of the potential sites for tapping geothermal energy at industrial scale. The hydrogeological properties and the temperature variations with depth have been examined under the Geological Society of India by drilling borewells at a few locations. The temperature distribution is one of the most essential parameters in quantifying the energy potential of a geothermal reservoir in its life time. Such temperature distribution has not been mapped for the Puga Valley. 2D Kriging technique is adopted in this study to assess temperature distribution for thermal manifestation zone at various depths and these are further used to estimate the thermal gradients at ungauged locations of the valley. From the results obtained, it is observed that the thermal gradient in the eastern zone of the valley is relatively higher. This indicates a possible bottom heat source in the eastern zone of the valley. The results of this study could be helpful in identifying the distinctive conceivable locations of injection and production wells for the extraction of entrapped heat within the rock strata. Also, a priority order is drawn in terms of thermal gradients at gauged and ungauged locations which may be helpful in deciding the zones of high and low heat sources in the reservoir.

Highlights

  • After decades of research carried out in India by several government organizations, a decision has been taken to generate 1000 MW of electricity using geothermal energy by 2022

  • In this study, ordinary Kriging is used to map temperature by using the field data from gauged well locations which is spread over an area of 3 km2 representing the thermal manifestation zone of the Puga Valley

  • This study aims to predict 2D temperature distribution in thermal manifestation zone of the Puga Valley and thermal gradients at ungauged well locations

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Summary

Introduction

After decades of research carried out in India by several government organizations, a decision has been taken to generate 1000 MW of electricity using geothermal energy by 2022. Geothermal energy is perceived as a hidden potential in the earth’s crust. Research efforts in India on geothermal energy date back to year of 1862 (Guha 1986). As a part of this effort, the Geological Survey of India explored 340 hot springs and a few potential geothermal provinces with an overall potential of 10,600 MW. These springs are grouped into seven geothermal provinces namely Himalayan (Puga–Chumathang), Sahara Valley, Cambay Basin, Son-Narmada-Tapi Lineament Belt, West Coast, Godavari Basin and Mahanadi Basin. Subsequent research in exploring and tapping this energy resource remains inadequate and no remarkable progress has been achieved in the production of electricity on an industrial scale

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