CHANGE OF THE RESERVOIR FLUID CHARACTERISTICS IN WEST SILERI SECTION, DIENG GEOTHERMAL FIELD
Dieng geothermal field is a volcanic hydrothermal water dominance, lies at Wonoboso, Banjarnegara and Pekalongan District, Central Java. The study was conducted on four wells, those are RH-1, RH-2, RH-3 and RH-4 on Sileri reservoir. Change in reservoir charcteristics is indicated by comparing the...
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id-itb.:633122022-01-28T15:19:41ZCHANGE OF THE RESERVOIR FLUID CHARACTERISTICS IN WEST SILERI SECTION, DIENG GEOTHERMAL FIELD Hidayat, Ryan Indonesia Theses Alteration, Dieng, Activity Diagram, Evolution. INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/63312 Dieng geothermal field is a volcanic hydrothermal water dominance, lies at Wonoboso, Banjarnegara and Pekalongan District, Central Java. The study was conducted on four wells, those are RH-1, RH-2, RH-3 and RH-4 on Sileri reservoir. Change in reservoir charcteristics is indicated by comparing the condition of the past and the present conditions. The past condition is show by the occurrence of alteration minerals analyzed by megaskopis, petrographic and XRD. The present condition obtained from measurement of temperature and pressure curve and water chemistry discharge from RH-1 and RH-3 wells. Reservoir fluid evolution started with water rock interaction at temperatur 300°C. Afterwards, boiling process took place which led to the formation of the vapour reservoir at temperature 300-335°C. text |
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Dieng geothermal field is a volcanic hydrothermal water dominance, lies at
Wonoboso, Banjarnegara and Pekalongan District, Central Java. The study was
conducted on four wells, those are RH-1, RH-2, RH-3 and RH-4 on Sileri reservoir.
Change in reservoir charcteristics is indicated by comparing the condition of the past
and the present conditions. The past condition is show by the occurrence of alteration
minerals analyzed by megaskopis, petrographic and XRD. The present condition
obtained from measurement of temperature and pressure curve and water chemistry
discharge from RH-1 and RH-3 wells.
Reservoir fluid evolution started with water rock interaction at temperatur 300°C.
Afterwards, boiling process took place which led to the formation of the vapour
reservoir at temperature 300-335°C. |
| format |
Theses |
| author |
Hidayat, Ryan |
| spellingShingle |
Hidayat, Ryan CHANGE OF THE RESERVOIR FLUID CHARACTERISTICS IN WEST SILERI SECTION, DIENG GEOTHERMAL FIELD |
| author_facet |
Hidayat, Ryan |
| author_sort |
Hidayat, Ryan |
| title |
CHANGE OF THE RESERVOIR FLUID CHARACTERISTICS IN WEST SILERI SECTION, DIENG GEOTHERMAL FIELD |
| title_short |
CHANGE OF THE RESERVOIR FLUID CHARACTERISTICS IN WEST SILERI SECTION, DIENG GEOTHERMAL FIELD |
| title_full |
CHANGE OF THE RESERVOIR FLUID CHARACTERISTICS IN WEST SILERI SECTION, DIENG GEOTHERMAL FIELD |
| title_fullStr |
CHANGE OF THE RESERVOIR FLUID CHARACTERISTICS IN WEST SILERI SECTION, DIENG GEOTHERMAL FIELD |
| title_full_unstemmed |
CHANGE OF THE RESERVOIR FLUID CHARACTERISTICS IN WEST SILERI SECTION, DIENG GEOTHERMAL FIELD |
| title_sort |
change of the reservoir fluid characteristics in west sileri section, dieng geothermal field |
| url |
https://digilib.itb.ac.id/gdl/view/63312 |
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