2024
DOI: 10.1016/j.geothermics.2024.102983
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Sequentially optimized data acquisition for a geothermal reservoir

Anthony Corso,
Maria Chiotoroiu,
Torsten Clemens
et al.
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Cited by 1 publication
(10 citation statements)
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“…The numerical models consist of approximately 0.82 million cells and cover an area of 8 km from south to north and 6 km from east to west. The average reservoir thickness is approximately 200 m, with the uppermost layer of the reservoir at a depth of 1500 m in the northern region, gradually deepening to 3800 m in the south [70]. The porosity model is governed by well log interpretations, whereas the porosity and permeability distribution is given by geostatistical methods in areas away from the wells.…”
Section: Geological Reservoir Parameterisationmentioning
confidence: 99%
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“…The numerical models consist of approximately 0.82 million cells and cover an area of 8 km from south to north and 6 km from east to west. The average reservoir thickness is approximately 200 m, with the uppermost layer of the reservoir at a depth of 1500 m in the northern region, gradually deepening to 3800 m in the south [70]. The porosity model is governed by well log interpretations, whereas the porosity and permeability distribution is given by geostatistical methods in areas away from the wells.…”
Section: Geological Reservoir Parameterisationmentioning
confidence: 99%
“…Corso et al [70] introduced a POMDP agent designed to address challenges in data acquisition. Below, the POMDP and agent as developed by Corso et al [70] is briefly described.…”
Section: Introduction Of Pomdp and Agentmentioning
confidence: 99%
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