Modeling of Advective Heat Transfer in a Practical Building Atrium via Koopman Mode Decomposition

Author(s):  
Yohei Kono ◽  
Yoshihiko Susuki ◽  
Takashi Hikihara

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


2020 ◽  
Vol 56 (11) ◽  
Author(s):  
Adam J. Hawkins ◽  
Don B. Fox ◽  
Donald L. Koch ◽  
Matthew W. Becker ◽  
Jefferson W. Tester


2000 ◽  
Vol 109 (4) ◽  
pp. 540-553 ◽  
Author(s):  
Makoto YAMANO ◽  
Masataka KINOSHITA ◽  
Osamu MATSUBAYASHI ◽  
Yukihiko NAKANO


2001 ◽  
Vol 65 (3) ◽  
pp. 373-396 ◽  
Author(s):  
G. R. Lowell ◽  
P. D. Noll

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.



2017 ◽  
Vol 53 (2) ◽  
pp. 123-133 ◽  
Author(s):  
Yohei KONO ◽  
Yoshihiko SUSUKI ◽  
Mitsunori HAYASHIDA ◽  
Takashi HIKIHARA


2020 ◽  
Author(s):  
Adam Jacob Hawkins ◽  
Don Bruce Fox ◽  
Donald Koch ◽  
Matthew W Becker ◽  
Jefferson William Tester




2017 ◽  
Vol 53 (2) ◽  
pp. 188-197
Author(s):  
Yohei KONO ◽  
Yoshihiko SUSUKI ◽  
Takashi HIKIHARA




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