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Abstract
Samples of flowback water from a 4.3 km deep geothermal borehole in granite (Pohang, South Korea) were collected following a period of hydraulic stimulation by injection of surface water. Electrical conductivity, temperature and water chemistry of the flowback water were measured. To a first approximation, the data conform closely to a simple 'mixing tank' model, with an exponential trend between two end members: an initial injected surface water to a more brackish 'resident groundwater' composition. Significant deviation from the 'mixing tank' trend would be an indication of significant recent water-rock interaction or other anomalous factors. Such a deviation can tentatively be seen in Na/Cl data, especially between 88 and 200 m3 flowback (2.8 to 8.8 hr).
Original language | English |
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Article number | 08001 |
Number of pages | 5 |
Journal | E3S Web of Conferences |
Volume | 98 |
DOIs | |
Publication status | Published - 7 Jun 2019 |
Event | 16th International Symposium on Water-Rock Interaction, WRI 2019 and 13th International Symposium on Applied Isotope Geochemistry, 1st IAGC International Conference - Tomsk, Russian Federation Duration: 21 Jul 2019 → 26 Jul 2019 |
Keywords
- geothermal borehole
- granite
- mixing tank model
- resident groundwater
- injected surface water
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Dive into the research topics of 'Exponential trends in flowback chemistry from a hydraulically stimulated deep geothermal borehole in granite; Pohang, South Korea'. Together they form a unique fingerprint.Projects
- 1 Finished
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DESTRESS: Demonstration of soft stimulation treatments of geothermal reservoirs
1/03/16 → 1/05/21
Project: Projects from Previous Employment