RESERVOIR CHARACTERIZATION AND STORAGE CAPACITY OF CO2 ESTIMATION AT RK FIELD, BEKASAP FORMATION, CENTRAL SUMATERA BASIN
Many countries commited to reducing CO2 emission which is a current environmental issue because it is really rises every year. Carbon Capture, Utilization and Storage (CCUS) is essential tool to unlock the full potential decarbonization where the CO2 is captured from atmosphere directly or fro...
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Format: | Final Project |
Language: | Indonesia |
Subjects: | |
Online Access: | https://digilib.itb.ac.id/gdl/view/78489 |
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Institution: | Institut Teknologi Bandung |
Language: | Indonesia |
Summary: | Many countries commited to reducing CO2 emission which is a current
environmental issue because it is really rises every year. Carbon Capture,
Utilization and Storage (CCUS) is essential tool to unlock the full potential
decarbonization where the CO2 is captured from atmosphere directly or from
refinery & petrochemical plant and geothermal power plant. One of CO2 geological
storage is depleted oil and gas field. RK Field is a gas field located in Central
Sumatera Basin which has a recovery factor of gas about 48,13% and 14 inactive
wells from 18 total wells. Characterization of reservoir and estimation of CO2
storage capacity are needed to identify CCUS potential in interval of study at RK
field. This study conducted within SB 1 – SB 5 interval of Early Miocene age in
Bekasap Formation. This study aims to understand RK Field’s geological
configuration especially in study’s interval, do facies analysis and determine
depositional environment of study’s interval, identify and correlate sequence of
stratigraphy of study’s interval, determine petrophysics property value in every
parasequence of study’s interval, and estimate storage capacity of CO2 of RK Field.
Data used in this study came consists of wireline logs from 16 wells, core
descriptions, pressure and temperature of reservoir reports, and three-dimension
seismic that covers all wells.
Seismic of the study area shows several faults of inversion faults with northwest–
southeast relative directions. Facies and depositional environment yielded four
lithofacies. Lithofacies analysis is then matched with log pattern in electrofacies
analysis resulting SB 1 – SB 5 interval shows two facies association which are
heterolithic mouthbars and tidally influence channel deposited in delta-front and
lower delta plain environment respectively. Sequence stratigraphy analysis shows
study’s interval is dominated by progradation and retrogradation parasequence
set, transgressive system tract, and highstand system tract. Petrophysics analysis
shows the average property value of shale volumes, effective porosity, and water
saturation of reservoir is 0.33, 0.12, and 0.33. Reservoir cut-off property values of
shale volume at 0.48, effective porosity at 0.1, and water saturation at 0.52. Storage
capacity of CO2 in reservoir estimation results is 7.24 MMT CO2 in vapor phase. |
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