Predictive Inverse Model for Advective Heat Transfer in a Planar Fracture with Heterogeneous Permeability

2020 ◽  
Author(s):  
Adam Jacob Hawkins ◽  
Don Bruce Fox ◽  
Donald Koch ◽  
Matthew W Becker ◽  
Jefferson William Tester
Keyword(s):  
Heat Transfer ◽  
Inverse Model ◽  
Advective Heat Transfer

scholarly journals Predictive Inverse Model for Advective Heat Transfer in a Short‐Circuited Fracture: Dimensional Analysis, Machine Learning, and Field Demonstration

2020 ◽  
Vol 56 (11) ◽  
Author(s):  
Adam J. Hawkins ◽  
Don B. Fox ◽  
Donald L. Koch ◽  
Matthew W. Becker ◽  
Jefferson W. Tester
Keyword(s):  
Heat Transfer ◽  
Machine Learning ◽  
Dimensional Analysis ◽  
Inverse Model ◽  
Advective Heat Transfer

Predictive Inverse Model for Advective Heat Transfer in a Planar Fracture with Heterogeneous Permeability

2020 ◽  
Author(s):  
Adam Jacob Hawkins ◽  
Don Bruce Fox ◽  
Donald Koch ◽  
Matthew W Becker ◽  
Jefferson William Tester
Keyword(s):  
Heat Transfer ◽  
Inverse Model ◽  
Advective Heat Transfer

Advances in convective and advective heat transfer in geological systems

2009 ◽  
Vol 101 (1) ◽  
pp. 128 ◽  
Author(s):  
Chongbin Zhao ◽  
Bruce E. Hobbs ◽  
Alison Ord
Keyword(s):  
Heat Transfer ◽  
Advective Heat Transfer

scholarly journals Thermal Structure of the Nankai Accretionary Prism and Effects of Advective Heat Transfer by Pore Fluid Flows.

2000 ◽  
Vol 109 (4) ◽  
pp. 540-553 ◽  
Author(s):  
Makoto YAMANO ◽  
Masataka KINOSHITA ◽  
Osamu MATSUBAYASHI ◽  
Yukihiko NAKANO
Keyword(s):  
Heat Transfer ◽  
Thermal Structure ◽  
Fluid Flows ◽  
Accretionary Prism ◽  
Pore Fluid ◽  
Advective Heat Transfer

Fe-Cu-Au-bearing scapolite skarn in moat sediments of the Taum Sauk Caldera, southeastern Missouri, USA

2001 ◽  
Vol 65 (3) ◽  
pp. 373-396 ◽  
Author(s):  
G. R. Lowell ◽  
P. D. Noll
Keyword(s):  
Heat Transfer ◽  
Host Rock ◽  
Flow Path ◽  
Contact Aureole ◽  
Combined Effects ◽  
Advective Heat Transfer

AbstractStromatolitic carbonate in moat-fill of a 1.48 Ga caldera was converted to mineralized calc-silicate skarn by interaction with magma-derived brine at Ketcherside Gap in southeastern Missouri. The skarnrecords early low fO2 conditions similar to those of reduced W and Au skarns. Initial skarn-forming conditions were: PL ≤ 221 bar (22.1 MPa), XCO2 ≤ 0.10, T = 450–;400°C, log fO2 ≈ –30, and log fS2 ≤ –13. Late skarn records combined effects of T↓, fO2↑,fS2↑, XCO2↓, and appearance of an immiscible CO2-rich vapour. The absence of a contact aureole indicates that skarn reactions were driven by advective heat transfer from an infiltrating fluid. Elsewhere in the region, hypersaline, synvolcanic fluids produced oxidized endoskarn in rhyolite. Development of carbonate-hosted, reduced skarn in caldera moat sediments is attributed to: (1) the nature of the host rock and reaction along a lengthy flow path; (2) early, but temporary, dilution of brine influx by CO2-producing reactions; and (3) cooling, possibly accompanied by increased brine influx with time.

THERMIC: a 2-D finite-element tool to solve conductive and advective heat transfer problems in Earth Sciences

1999 ◽  
Vol 25 (10) ◽  
pp. 1137-1148 ◽  
Author(s):  
Alain Bonneville ◽  
Patrick Capolsini
Keyword(s):  
Earth Sciences ◽  
Heat Transfer ◽  
Finite Element ◽  
Advective Heat Transfer ◽  
Transfer Problems
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