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The global energy demandRenewable energy continuesWave Energy Converter (WEC) to escalate, driven by enhanced living standards associated with technological advancements and breakthroughs. Concurrently, the challenges inherent in the energy system persist; therefore, assessing differences in the Curie isotherm of a region yields valuable insights into the temperature distribution of the region and the energy of the source ensemble. Airborne magnetic data have been effectively utilized to ascertain the renewable energyRenewable energy concentration across the region. Slope depth methods of analysis estimate depth to the centroid and the top boundary to range approximately from 5 to 6 km and 0.61 to 1.9 km, respectively. Estimation of the Curie isotherm reveals an average point depth of about 10.2 km throughout the study area. The energy gradient in the region was estimated to be an average of 56.1 °Ckm−1. Subsurface heat energy flow revealed a mean approximation of about 140.3 mW/m2. This difference in subsurface heat energy flow within the Earth is attributable to the lithological differences observed across diverse regions. Consequently, the findings regarding the renewable energy systemRenewable energy systems will enable essential technological advancement required for the development of a hybrid geo-wave energy converterWave Energy Converter (WEC) system.

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Renewable Energy Sources: An Insight from Geothermal and Wave Energy Converter Systems

  • 章节

  • 发表日期：

    2026年

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  • T. K. Alasi,
  • C. O. Ogunkoya,
  • D. E. Adeleke,
  • M. A. Fakunle,
  • L. O. Olawale

摘要

The global energy demandRenewable energy continuesWave Energy Converter (WEC) to escalate, driven by enhanced living standards associated with technological advancements and breakthroughs. Concurrently, the challenges inherent in the energy system persist; therefore, assessing differences in the Curie isotherm of a region yields valuable insights into the temperature distribution of the region and the energy of the source ensemble. Airborne magnetic data have been effectively utilized to ascertain the renewable energyRenewable energy concentration across the region. Slope depth methods of analysis estimate depth to the centroid and the top boundary to range approximately from 5 to 6 km and 0.61 to 1.9 km, respectively. Estimation of the Curie isotherm reveals an average point depth of about 10.2 km throughout the study area. The energy gradient in the region was estimated to be an average of 56.1 °Ckm−1. Subsurface heat energy flow revealed a mean approximation of about 140.3 mW/m2. This difference in subsurface heat energy flow within the Earth is attributable to the lithological differences observed across diverse regions. Consequently, the findings regarding the renewable energy systemRenewable energy systems will enable essential technological advancement required for the development of a hybrid geo-wave energy converterWave Energy Converter (WEC) system.