印度古吉拉特邦甘达尔地热田开发前景

Kelvy P. Dalsania , Anirbid Sircar , Vaishnavi Pandey , Kriti Yadav , Namrata Bist , Tejaswini Gautam
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摘要

油田开发是自然资源利用和勘探的重要组成部分,因为它涉及对特定区域的系统评估和优化。本研究探讨了印度古吉拉特邦犍陀罗地区的地热田开发。过去几十年来,犍陀罗一直是油气开采的旺地。然而,由于全球都在应对环境问题,并需要转向更清洁、更可持续的能源,地热能源已成为一种可行且无害生态的选择。本研究旨在了解甘达尔及其周边地区作为印度西海岸大陆边缘潜在地热田的潜力。在地表采用了地质、地球化学和地球物理勘测三个主要学科来评估犍陀罗地热资源的潜力。地质评估提供了有关底层地质构造的信息,这可能有助于找到可能的地热资源。德干岩基底是岩浆热的主要来源,热梯度在 1.29 到 1.87 W/K 之间。通过加热地下水和地核中的放射性核素,这增强了犍陀罗的地热潜力。根据吉根巴赫三角法,温度范围为 60 至 80 °C。犍陀罗的水富含碳酸氢盐,与可能的地下含水层相连,这进一步凸显了犍陀罗的地热潜力。地球物理研究证实了这些结果。通过异常现象可以发现潜在的地热储量和四通闭合。重力勘测发现了一个双垂向反斜面,重力高值分别为 5.4 和 5.3 mGa l,58 和 56.2 nT 的磁峰也证实了这一点。电阻率研究确定了导电率较高的区域,这也表明可能存在流体路径和地热储层。本文概述了已确定勘探区的概念性实地开发计划。文件还计算了基本的基础设施和与之相关的开发成本。还强调了生产成本/兆瓦发电量。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

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Prospects of geothermal field development in Gandhar, Gujarat, India

Field development is an important part of natural resource utilization and exploration because it involves a systematic evaluation and optimization of a specific area. This study examines the geothermal field development in the Gandhar region of Gujarat, India. Gandhar for the past several decades has been a flourishing field for hydrocarbon extraction. However, as the world is dealing with environmental issues and the need to shift to cleaner and more sustainable energy sources, geothermal energy has emerged as a feasible and ecologically sound option. This study aims to understand the potential of regions in and around Gandhar as a prospective geothermal field of the west coast continental margin of India. Three primary disciplines namely geological, geochemical, and geophysical surveys are employed on the surface to assess the potential of Gandhar's geothermal resources. Geological assessments provide information about underlying geological formations, which might help to locate possible geothermal resources. The Deccan basement is a prominent source of magmatic heat, with a thermal gradient ranging from 1.29 to 1.87 W/K. This enhances Gandhar's geothermal potential by heating the underlying water in conjunction with radionuclides found in the Earth's core. The temperatures range from 60 to 80 °C according to Giggenbach triangle method. Gandhar's geothermal potential is further highlighted by the fact that its water is bicarbonate-rich, which connects it to possible subterranean aquifers. These results are verified by geophysical studies. Prospective geothermal reserves and four way closures can be found by as anomalies. Gravity survey reveal a doubly plunging antiform, with gravity high value of 5.4 and 5.3 mGa l respectively, which is corroborated by magnetic peaks of 58 and 56.2 nT Areas with higher conductivity are identified by resistivity studies, which also indicate possible fluid paths and geothermal reservoirs. The paper outlines a conceptual field development plan for the identified prospect. The basic infrastructure and the cost associated with it for field development is worked out. The cost of production/MWe of energy generation is also highlighted.

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