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Carbon isotopic constraints on CO2 degassing in cold-water geysers, Green River, Utah

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Carbon isotopic constraints on CO2 degassing in cold-water geysers, Green River, Utah. / Assayag, Nelly; Bickle, Mike; Kampman, Niko et al.
In: Energy Procedia, Vol. 1, No. 1, 02.2009, p. 2361-2366.

Research output: Contribution to Journal/Magazine › Journal article › peer-review

Harvard

Assayag, N, Bickle, M, Kampman, N & Becker, J 2009, 'Carbon isotopic constraints on CO2 degassing in cold-water geysers, Green River, Utah', Energy Procedia, vol. 1, no. 1, pp. 2361-2366. https://doi.org/10.1016/j.egypro.2009.01.307

APA

Assayag, N., Bickle, M., Kampman, N., & Becker, J. (2009). Carbon isotopic constraints on CO2 degassing in cold-water geysers, Green River, Utah. Energy Procedia, 1(1), 2361-2366. https://doi.org/10.1016/j.egypro.2009.01.307

Vancouver

Assayag N, Bickle M, Kampman N, Becker J. Carbon isotopic constraints on CO2 degassing in cold-water geysers, Green River, Utah. Energy Procedia. 2009 Feb;1(1):2361-2366. doi: 10.1016/j.egypro.2009.01.307

Author

Assayag, Nelly ; Bickle, Mike ; Kampman, Niko et al. / Carbon isotopic constraints on CO2 degassing in cold-water geysers, Green River, Utah. In: Energy Procedia. 2009 ; Vol. 1, No. 1. pp. 2361-2366.

Bibtex

@article{32bcb0e7b1454c1ca06c159b20125438,
title = "Carbon isotopic constraints on CO2 degassing in cold-water geysers, Green River, Utah",
abstract = "Cold-water geysers at Green River, in east central Utah are sourced by natural springs situated along the Little Grand Wash and Salt Wash faults zones, as well as abandoned oil and water wells. The intermittent geysers are driven by degassing of CO2 from CO2-rich waters sourced from the Jurassic Navajo sandstone. Here we discuss use of del13C analyses of water and gases to estimate the depth at which the ascending waters become CO2 saturated. This is a potentially important control in the unlikely event of rapid CO2 escape from CO2 reservoirs. In Green River, it is also important for calculation of the kinetics of fluid-mineral reactions in the Navajo sandstone as an analogue for predicting the fate of CO2 in carbon storage reservoirs",
keywords = "CO2 degassing, CO2 natural analogue , Dissolved inorganic carbon , Stable isotope",
author = "Nelly Assayag and Mike Bickle and Niko Kampman and John Becker",
year = "2009",
month = feb,
doi = "10.1016/j.egypro.2009.01.307",
language = "English",
volume = "1",
pages = "2361--2366",
journal = "Energy Procedia",
issn = "1876-6102",
publisher = "Elsevier BV",
number = "1",

}

RIS

TY - JOUR

T1 - Carbon isotopic constraints on CO2 degassing in cold-water geysers, Green River, Utah

AU - Assayag, Nelly

AU - Bickle, Mike

AU - Kampman, Niko

AU - Becker, John

PY - 2009/2

Y1 - 2009/2

N2 - Cold-water geysers at Green River, in east central Utah are sourced by natural springs situated along the Little Grand Wash and Salt Wash faults zones, as well as abandoned oil and water wells. The intermittent geysers are driven by degassing of CO2 from CO2-rich waters sourced from the Jurassic Navajo sandstone. Here we discuss use of del13C analyses of water and gases to estimate the depth at which the ascending waters become CO2 saturated. This is a potentially important control in the unlikely event of rapid CO2 escape from CO2 reservoirs. In Green River, it is also important for calculation of the kinetics of fluid-mineral reactions in the Navajo sandstone as an analogue for predicting the fate of CO2 in carbon storage reservoirs

AB - Cold-water geysers at Green River, in east central Utah are sourced by natural springs situated along the Little Grand Wash and Salt Wash faults zones, as well as abandoned oil and water wells. The intermittent geysers are driven by degassing of CO2 from CO2-rich waters sourced from the Jurassic Navajo sandstone. Here we discuss use of del13C analyses of water and gases to estimate the depth at which the ascending waters become CO2 saturated. This is a potentially important control in the unlikely event of rapid CO2 escape from CO2 reservoirs. In Green River, it is also important for calculation of the kinetics of fluid-mineral reactions in the Navajo sandstone as an analogue for predicting the fate of CO2 in carbon storage reservoirs

KW - CO2 degassing

KW - CO2 natural analogue

KW - Dissolved inorganic carbon

KW - Stable isotope

U2 - 10.1016/j.egypro.2009.01.307

DO - 10.1016/j.egypro.2009.01.307

M3 - Journal article

VL - 1

SP - 2361

EP - 2366

JO - Energy Procedia

JF - Energy Procedia

SN - 1876-6102

IS - 1

ER -