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Renewable Energy & Power Sector25 Essential Exam Concepts

Geothermal Energy in India: Potential, Exploration Sites & Utilization Guide

Geothermal energy utilizes the immense natural heat stored within the Earth's sub-surface crust, extracted through hot subterranean aquifers, pressurized hydrothermal steam, and dry radiogenic rock formations. Unlike intermittent renewable energy sources such as solar photovoltaics and wind turbines—which depend strictly upon diurnal cycles and atmospheric meteorological conditions—geothermal energy represents a continuous, weather-independent source of baseload electric power. Possessing an exceptional Capacity Utilisation Factor (CUF) routinely exceeding eighty to ninety percent, geothermal resources provide stable grid inertia, minimal land footprint requirements, and near-zero greenhouse gas emissions during sustained power generation.

India's exploration of its geothermal potential is driven by its international climate commitments under the COP26 Glasgow Panchamrit goals, specifically achieving five hundred gigawatts of non-fossil installed electric capacity by 2030 and Net Zero carbon emissions by 2070. Extensive geological investigations conducted by the Geological Survey of India (GSI) and the Ministry of New and Renewable Energy (MNRE) have cataloged approximately three hundred and forty distinct hot spring systems distributed across seven major geothermal provinces. These include the Himalayan Geothermal Belt (notably Puga Valley and Chumathang in Ladakh, Manikaran in Himachal Pradesh, and Tapovan in Uttarakhand), the Cambay Graben in Gujarat, the West Coast geothermal lineament in Maharashtra, and the Son-Narmada-Tapi (SONATA) rift zone in central India.

The utilization of geothermal energy is partitioned into indirect power generation and direct thermal applications. For electricity generation, medium-to-high enthalpy geothermal reservoirs (100circextC100^circ ext{C} to >200circextC>200^circ ext{C}) are harnessed using binary cycle power plants (operating on the Organic Rankine Cycle), where geothermal fluids vaporize low-boiling-point working fluids to spin turbines. Simultaneously, direct thermal applications offer transformative developmental benefits in remote, sub-zero Himalayan altitudes. In regions like Ladakh, geothermal fluid is routed directly for residential district space heating, operating winter agricultural greenhouses, hot-spring tourism balneology, aquaculture, and cold-storage refrigeration, displacing diesel generator consumption and bolstering regional energy self-reliance. Moreover, enhanced geothermal systems (EGS) and sub-surface reinjection techniques ensure that mineralized geothermal brines are recycled into deep aquifers without contaminating surface hydrological systems, preserving fragile Himalayan ecosystems while securing clean thermal power.

Essential Concepts & Key Facts

High-yield conceptual summaries for competitive exams and rapid revision.

  • Geothermal energy is renewable thermal energy generated from radioactive decay of minerals and original primordial heat in Earth's core.
  • Unlike solar and wind power, geothermal is a continuous baseload power source with a Capacity Utilisation Factor (CUF) above 80–90%.
  • The Ministry of New and Renewable Energy (MNRE) estimates India's aggregate geothermal power potential at approximately 10,000 MW (10 GW).
  • The Geological Survey of India (GSI) has identified roughly 340 hot springs across seven recognized geothermal provinces in India.
  • The seven geothermal provinces are: Himalayan, Cambay, West Coast, SONATA lineament, Godavari, Mahanadi, and Bakreswar.
  • Puga Valley in the Ladakh region is recognized as India's most promising geothermal field, with surface temperatures exceeding 84°C.
  • Puga lies at the collision boundary of the Indian and Eurasian tectonic plates, creating high geothermal heat gradients.
  • India's first commercial-scale geothermal power project is being developed at Puga Valley by the Oil and Natural Gas Corporation (ONGC).
  • Chumathang in Ladakh is another high-enthalpy Himalayan geothermal field located along the Indus suture zone.
  • Manikaran in the Parbati Valley of Himachal Pradesh is famous for high-temperature hot springs containing radioactive radon and minerals.
  • Tatapani in the Balrampur district of Chhattisgarh represents the prime geothermal field within the Son-Narmada-Tapi (SONATA) lineament.
  • Cambay geothermal province in Gujarat features deep sedimentary aquifers heated by high heat-flow granitic basement rocks.
  • The West Coast geothermal belt includes hot spring clusters at Unhavre, Tural, and Rajapur along coastal tectonic fault fractures in Maharashtra.
  • Direct use of geothermal energy involves utilizing hot water directly for space heating, greenhouses, aquaculture, and crop drying.
  • Direct geothermal heating eliminates the need for burning high-emission fossil fuels or diesel in sub-zero Himalayan winter months.
  • Indirect geothermal utilization converts high-pressure geothermal steam or hot brine into electricity via turbine generators.
  • Binary Cycle power plants use the Organic Rankine Cycle (ORC) to generate power from moderate-temperature geothermal brines (100°C–180°C).
  • Enhanced Geothermal Systems (EGS) inject pressurized water into deep, impermeable hot dry rock (HDR) to create artificial geothermal reservoirs.
  • Geothermal exploration involves geochemical geothermometry, magnetotelluric (MT) geophysical surveys, and deep exploratory drilling.
  • Geothermal power plants occupy the smallest land area per megawatt-hour produced among all renewable energy sources.
  • The main environmental considerations in geothermal development include managing dissolved hydrogen sulfide gas and mineral reinjection.
  • Developing geothermal energy aligns with India's Glasgow COP26 target to expand non-fossil energy capacity to 500 GW by 2030.

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