2009
DOI: 10.1016/j.egypro.2009.01.293
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Monitoring at the CO2 SINK site: A concept integrating geophysics, geochemistry and microbiology

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Cited by 103 publications
(43 citation statements)
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“…The CO 2 arrival in the observation well was detected by the downhole measurements of the amount and nature of the dissolved gases in the fluid samples by GMS (Gas Membrane Sensor) and the increase of the well head pressure (Giese et al, 2009). The CO 2 arrival resulted in a significant decrease in pH and the number of bacteria (Fig.…”
Section: Discussionmentioning
confidence: 99%
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“…The CO 2 arrival in the observation well was detected by the downhole measurements of the amount and nature of the dissolved gases in the fluid samples by GMS (Gas Membrane Sensor) and the increase of the well head pressure (Giese et al, 2009). The CO 2 arrival resulted in a significant decrease in pH and the number of bacteria (Fig.…”
Section: Discussionmentioning
confidence: 99%
“…The CO 2 arrival in the observation well 1 (Ktzi 200) was detected by the downhole measurements of the amount and nature of the dissolved gases in the fluid samples. Notably, detailed physical, geochemical and microbiological monitoring was performed in all three wells (Giese et al, 2009). However, this study concentrates on the results obtained from the observation well 1 (Ktzi 200), where it was possible to monitor the effects of the CO 2 exposure during the five months.…”
Section: Study Sitementioning
confidence: 99%
“…For monitoring of CO 2 , the injection well and the two observation wells were equipped with geophysical sensors including e.g. a fiber-optic-sensor cable loop for Distributed Temperature Sensing (DTS; all wells) and a Vertical Electrical Resistivity Array (VERA) consisting of fifteen toroidal steel electrodes per well and 15-line surface connection cables (Prevedel et al, 2009;Giese et al, 2009). In recent studies, Electrical Resistivity Tomography (ERT) based on cross-hole measurements has been evaluated as a suitable method to detect the resistivity changes caused by CO 2 injection and migration in geological reservoirs (Ramirez et al, 2003;Christensen et al, 2006).…”
Section: Introductionmentioning
confidence: 99%
“…This distributed temperature sensing system was applied to the CO2SINK project in Germany where CO2 was injected into a saline aquifer with an anticlinal structure [Forster, 2006]. Although the definite cause observed in temperature signal is still being investigated, the distributed temperature sensing system successfully measured the largest temperature increase (Δ25 °C) close to the injection wellhead during the injection period [Giese et al, 2009 ] while the temperature increase within the injection zone was about Δ5-10°C. In summary, CO 2 injection into the Arbuckle formation are expected to disturb the temperature regimes in the target formations, and such temperature changes could be detected by installation of temperature sensors in injection and observation wells.…”
Section: Thermal Disequilibrium Processesmentioning
confidence: 99%