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Title: Inert and Adsorptive Tracer Tests for Field Measurement of Flow-Wetted Surface Area

Abstract

Abstract Field tests in a discrete rock fracture validated a combined inert/adsorbing tracer test method to estimate the contact area between fluids circulating through a fracture and the bulk rock matrix (i.e., flow‐wetted surface area, A). Tracer tests and heat injections occurred at a mesoscale well field in Altona, NY. A subhorizontal bedding plane fracture ∼7.6 m below ground surface connects two wells separated by 14.1 m. Recovery of the adsorbing tracer cesium was roughly 72% less than the inert tracer iodide. Using an advection‐dispersion‐reaction model in one‐dimension, the adsorbing/inert tracer method identified substantial flow channelization. These results are consistent with Ground Penetrating Radar (GPR) and thermal sensors. All characterization methods suggest circulating fluids were concentrated in a narrow, 1–2 m wide channel directly connecting the injection and production well. The inert/adsorbing tracer method identified two flow channels with areas of 28 and 80 m 2 . A one‐dimensional heat transport model predicted production well temperature rises 20.5°C in 6 days, whereas measured temperature rise was 17.6°C. For comparison, two‐dimensional heat transport through a fracture of uniform aperture (i.e., homogeneous permeability) predicted roughly 670 days until production well temperature would rise 17.6°C. This suggests that the use of a fracturemore » of uniform aperture to predict heat transport may drastically overpredict the thermal performance of a geothermal system. In the context of commercial geothermal reservoirs, the results of this study suggest that combined inert/adsorbing tracer tests could predict production well thermal drawdown, leading to improved reservoir monitoring and management.« less

Authors:
ORCiD logo [1]; ORCiD logo [2];  [3]
  1. Stanford Univ., CA (United States)
  2. California State Univ., Long Beach, CA (United States)
  3. Cornell Univ., Ithaca, NY (United States)
Publication Date:
Research Org.:
California State Univ. (CalState), Long Beach, CA (United States); Cornell Univ., Ithaca, NY (United States)
Sponsoring Org.:
USDOE Office of Energy Efficiency and Renewable Energy (EERE)
OSTI Identifier:
1539737
Alternate Identifier(s):
OSTI ID: 1464869
Grant/Contract Number:  
EE0006763; EE0006764; DE EE0006764; DE EE0006763
Resource Type:
Accepted Manuscript
Journal Name:
Water Resources Research
Additional Journal Information:
Journal Volume: 54; Journal Issue: 8; Journal ID: ISSN 0043-1397
Publisher:
American Geophysical Union (AGU)
Country of Publication:
United States
Language:
English
Subject:
54 ENVIRONMENTAL SCIENCES; Environmental Sciences & Ecology; Marine & Freshwater Biology; Water Resources

Citation Formats

Hawkins, Adam J., Becker, Matthew W., and Tester, Jefferson W. Inert and Adsorptive Tracer Tests for Field Measurement of Flow-Wetted Surface Area. United States: N. p., 2018. Web. doi:10.1029/2017wr021910.
Hawkins, Adam J., Becker, Matthew W., & Tester, Jefferson W. Inert and Adsorptive Tracer Tests for Field Measurement of Flow-Wetted Surface Area. United States. https://doi.org/10.1029/2017wr021910
Hawkins, Adam J., Becker, Matthew W., and Tester, Jefferson W. Wed . "Inert and Adsorptive Tracer Tests for Field Measurement of Flow-Wetted Surface Area". United States. https://doi.org/10.1029/2017wr021910. https://www.osti.gov/servlets/purl/1539737.
@article{osti_1539737,
title = {Inert and Adsorptive Tracer Tests for Field Measurement of Flow-Wetted Surface Area},
author = {Hawkins, Adam J. and Becker, Matthew W. and Tester, Jefferson W.},
abstractNote = {Abstract Field tests in a discrete rock fracture validated a combined inert/adsorbing tracer test method to estimate the contact area between fluids circulating through a fracture and the bulk rock matrix (i.e., flow‐wetted surface area, A). Tracer tests and heat injections occurred at a mesoscale well field in Altona, NY. A subhorizontal bedding plane fracture ∼7.6 m below ground surface connects two wells separated by 14.1 m. Recovery of the adsorbing tracer cesium was roughly 72% less than the inert tracer iodide. Using an advection‐dispersion‐reaction model in one‐dimension, the adsorbing/inert tracer method identified substantial flow channelization. These results are consistent with Ground Penetrating Radar (GPR) and thermal sensors. All characterization methods suggest circulating fluids were concentrated in a narrow, 1–2 m wide channel directly connecting the injection and production well. The inert/adsorbing tracer method identified two flow channels with areas of 28 and 80 m 2 . A one‐dimensional heat transport model predicted production well temperature rises 20.5°C in 6 days, whereas measured temperature rise was 17.6°C. For comparison, two‐dimensional heat transport through a fracture of uniform aperture (i.e., homogeneous permeability) predicted roughly 670 days until production well temperature would rise 17.6°C. This suggests that the use of a fracture of uniform aperture to predict heat transport may drastically overpredict the thermal performance of a geothermal system. In the context of commercial geothermal reservoirs, the results of this study suggest that combined inert/adsorbing tracer tests could predict production well thermal drawdown, leading to improved reservoir monitoring and management.},
doi = {10.1029/2017wr021910},
journal = {Water Resources Research},
number = 8,
volume = 54,
place = {United States},
year = {Wed May 09 00:00:00 EDT 2018},
month = {Wed May 09 00:00:00 EDT 2018}
}

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Works referencing / citing this record:

Solute tracer test quantification of the effects of hot water injection into hydraulically stimulated crystalline rock
journal, June 2020


Solute tracer test quantification of the effects of hot water injection into hydraulically stimulated crystalline rock
text, January 2020