TY - CHAP
T1 - DigitalCrust - a 4D data system of material properties for transforming research on crustal fluid flow
AU - Fan, Ying
AU - Richard, Stephen
AU - Sky Bristol, R.
AU - Peters, Shanan E.
AU - Ingebritsen, Steven E.
AU - Moosdorf, Nils
AU - Packman, Aaron
AU - Gleeson, Tom
AU - Zaslavsky, Ilya
AU - Peckham, Scott
AU - Murdoch, Lawrence
AU - Fienen, Michael
AU - Cardiff, Michael
AU - Tarboton, David
AU - Jones, Norman
AU - Hooper, Richard
AU - Arrigo, Jennifer
AU - Gochis, David
AU - Olson, J.
AU - Wolock, David
N1 - Publisher Copyright:
© 2017 by John Wiley & Sons Ltd. All rights reserved.
PY - 2016/10/31
Y1 - 2016/10/31
N2 - Fluid circulation in the Earth's crust plays an essential role in surface, near-surface, and deep-crustal processes. The permeability of the Earth's crust is of particular interest because it determines the feasibility of important physicochemical processes, such as advective solute/heat transport and the generation of elevated fluid pressures by processes such as physical compaction, heating, mineral dehydration, and fluid injection. The foundation of DigitalCrust is a geologic scaffolding that describes the basic geologic fabric of the Earth's upper crust, from the critical zone to the brittle-ductile transition, and includes data spanning its full range of physical, chemical, and biological properties. Within the foundational geologic scaffolding, DigitalCrust will support multiscale integration of fluid-relevant properties. For geofluids applications, the DigitalCrust architecture needs to assimilate observational data and interpretations from all available sources, including geologic maps, cross sections and structural contours, hydrogeologic unit delineations, soil tests, slug tests, aquifer pump tests, and indirect property estimates obtained through model inversions.
AB - Fluid circulation in the Earth's crust plays an essential role in surface, near-surface, and deep-crustal processes. The permeability of the Earth's crust is of particular interest because it determines the feasibility of important physicochemical processes, such as advective solute/heat transport and the generation of elevated fluid pressures by processes such as physical compaction, heating, mineral dehydration, and fluid injection. The foundation of DigitalCrust is a geologic scaffolding that describes the basic geologic fabric of the Earth's upper crust, from the critical zone to the brittle-ductile transition, and includes data spanning its full range of physical, chemical, and biological properties. Within the foundational geologic scaffolding, DigitalCrust will support multiscale integration of fluid-relevant properties. For geofluids applications, the DigitalCrust architecture needs to assimilate observational data and interpretations from all available sources, including geologic maps, cross sections and structural contours, hydrogeologic unit delineations, soil tests, slug tests, aquifer pump tests, and indirect property estimates obtained through model inversions.
KW - 3D hydrological flow paths
KW - 4D space-time data infrastructure
KW - Crustal permeability
KW - DigitalCrust architecture
KW - Earth's crust
KW - Fluid injection
KW - Geofluids
KW - Mineral dehydration
KW - Slug tests
KW - Soil tests
UR - http://www.scopus.com/inward/record.url?scp=85019430562&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=85019430562&partnerID=8YFLogxK
U2 - 10.1002/9781119166573.ch2
DO - 10.1002/9781119166573.ch2
M3 - Chapter
AN - SCOPUS:85019430562
SN - 9781119166566
SP - 6
EP - 12
BT - Crustal Permeability
PB - wiley
ER -