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Geothermal Scope in Bangladesh

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dc.contributor.author Tarekul Islam
dc.contributor.author Sabbir Ahmed
dc.date.accessioned 2020-10-22T05:54:25Z
dc.date.available 2020-10-22T05:54:25Z
dc.date.issued 2020-01-12
dc.identifier.uri http://dspace.daffodilvarsity.edu.bd:8080/handle/123456789/4805
dc.description Heated fluid begins to rise above the surface of the earth under the pressure of intense pressure in the centre of the earth. Upon reaching the earth's surface, a pipe line will enter a cylinder where heated liquid and high pressure vapour will be separated. Through the pipe line, the extracted fluid is pumped into another cylinder where the normal pressure vapour (proof pressure vapour) is removed from that fluid and the separated fluid is re-entered into a cylinder where the fluid is low pressure vapour is split. Subsequently, steam is introduced into a turbine in these three categories of high- pressure, standard and low-pressure steam, rotating the turbine, connecting the turbine to a generator, generating electric charge. Such power is transmitted through copper wire to a step-up transformer, where it is transformed by increasing the voltage into a usable power for commercial and domestic use. On the other hand, heated liquid is re-filtered through another tube to the centre of the earth, so that the fluid is balanced. en_US
dc.description.abstract With only 510 kWh per capita of electricity generation, Bangladesh is one of the world's energy-affected countries and only 94 percent of its population has access to that electricity. Bangladesh is still very early in the sense of geothermal water use. To date, there has been no systematic study to assess Bangladesh's geothermal potential. However, authors in a few articles have highlighted the potential of Bangladesh's geothermal energy resources. Exploration of geothermal energy involves early exploration cash incentives, Yet good planning reduces risks and saves money. Many deep abandoned wells were used in Bangladesh, initially drilled for oil and gas exploration, to collect valuable information on the underground geology and temperature of interesting areas. Analysis of the temperature data for these wells shows that the average geothermal gradient along the south-eastern part of Bengal Foredeep varies from 19.8 ° C to 29.5 ° C / km and from 20.8 ° C to 48.7 ° C / km along the stable north-western shelf. An attempt was made to recalculate different temperatures of the geothermometer using the geochemical data from water samples from the basement aquifer of the Madhyapara hard rock mine region and using the knowledge gained from this training program. The predicted temperature ranges from 67 to 153 ° C, which can relate to a potential low-temperature geothermal field in the region of Madhyapara. After geophysical investigations (resistivity (MT), seismic, gravity, etc.) preliminary geological and geochemical surface studies are recommended, Drilling of shallow gradient wells to create a conceptual model of any geothermal system before continuing with the most expensive and hazardous part, i.e. deep well drilling. en_US
dc.language.iso en en_US
dc.publisher Daffodil International University en_US
dc.subject Geothermal Power Plants en_US
dc.subject Geothermal Resources en_US
dc.title Geothermal Scope in Bangladesh en_US
dc.type Other en_US


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