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 |