Open AccessThe U‐tube: A novel system for acquiring borehole fluid samples from a deep geologic CO 2 sequestration experiment
Author(s) -
Freifeld Barry M.,
Trautz Robert C.,
Kharaka Yousif K.,
Phelps Tommy J.,
Myer Larry R.,
Hovorka Susan D.,
Collins Daniel J.
Publication year - 2005
Publication title -
journal of geophysical research: solid earth
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2005jb003735
Subject(s) - supercritical fluid , brine , borehole , plume , geology , aquifer , core sample , petroleum engineering , mineralogy , groundwater , materials science , geotechnical engineering , chemistry , core (optical fiber) , physics , organic chemistry , composite material , thermodynamics
A novel system has been deployed to obtain geochemical samples of water and gas, at in situ pressure, during a geologic CO 2 sequestration experiment conducted in the Frio brine aquifer in Liberty County, Texas. Project goals required high‐frequency recovery of representative and uncontaminated aliquots of a rapidly changing two‐phase fluid (supercritical CO 2 and brine) fluid from 1.5 km depth. The data sets collected, using both the liquid and gas portions of the downhole samples, provide insights into the coupled hydrogeochemical issues affecting CO 2 sequestration in brine‐filled formations. While the basic premise underlying the U‐tube sampler is not new, the system is unique because careful consideration was given to the processing of the recovered two‐phase fluids. In particular, strain gauges mounted beneath the high‐pressure surface sample cylinders measured the ratio of recovered brine to supercritical CO 2 . A quadrupole mass spectrometer provided real‐time gas analysis for perfluorocarbon and noble gas tracers that were injected along with the CO 2 . The U‐tube successfully acquired frequent samples, facilitating accurate delineation of the arrival of the CO 2 plume, and on‐site analysis revealed rapid changes in geochemical conditions.