Mass transfer and porosity evolution during low temperature water–rock interaction in gneisses of the simano nappe: Arvigo, Val Calanca, Swiss Alps

2010 ◽  
Vol 162 (1) ◽  
pp. 61-81 ◽  
Author(s):  
Tobias Weisenberger ◽  
Kurt Bucher
Keyword(s):  
Mass Transfer ◽  
Low Temperature ◽  
Swiss Alps ◽  
Rock Interaction ◽  
Porosity Evolution ◽  
Temperature Water ◽  
Water Rock Interaction

Europium anomaly variation under low-temperature water-rock interaction: A new thermometer

2017 ◽  
Vol 55 (9) ◽  
pp. 822-832 ◽  
Author(s):  
R. Nakada ◽  
T. Shibuya ◽  
K. Suzuki ◽  
Y. Takahashi
Keyword(s):  
Low Temperature ◽  
Rock Interaction ◽  
Temperature Water ◽  
Water Rock Interaction

scholarly journals Mobility of dissolved palladium and platinum species under water-rock interaction in chloride media: modeling of PGE behavior under interaction of oceanic serpentinites with sea water derivates

2019 ◽  
Vol 64 (3) ◽  
pp. 263-272
Author(s):  
I. V. Kubrakova ◽  
O. A. Tyutyunnik ◽  
S. A. Silant’ev
Keyword(s):  
Low Temperature ◽  
Complex Compound ◽  
Sea Water ◽  
Experimental Conditions ◽  
Rock Interaction ◽  
Hydrothermal Transformation ◽  
Temperature Transformation ◽  
Intermediate Oxidation ◽  
Platinum Species ◽  
Water Rock Interaction

To elucidate the possibility of PGE transfer by highly-salt chloride solutions, the palladium and platinum behavior was simulated in the conditions of low-temperature hydrothermal transformation of serpentinites of the oceanic crust. In dynamic water-rock experiments using columns filled with crushed ultrabasic rocks of the ocean floor (harzburgite serpentinites of mid-oceanic ridges with different degrees of carbonatization), it is established that the efficiency of palladium transfer depends on the alteration (carbonatization) degree of peridotites and under the experimental conditions is 80–100%. It is assumed that the transport of palladium occurs as a result of the formation of a strong complex compound with thiosulfate ion, which is an intermediate oxidation product in the “sulphide-sulfate” system. Platinum, hydrolyzed at approximately neutral pH and not forming compounds with thiosulfate ion, is completely retained by serpentinites, possibly due to sorption interactions with silicates. Thus, the higher mobility of palladium during the low- temperature transformation of abyssal peridotites and the dependence of the character of its distribution in the studied rocks on the processes of serpentinization and carbonatization have been confirmed.

Mass Transfer from CO2Drops Traveling in High-Pressure and Low-Temperature Water

2001 ◽  
Vol 15 (1) ◽  
pp. 147-150 ◽  
Author(s):  
Keiichi Ogasawara ◽  
Akihiro Yamasaki ◽  
Ho Teng
Keyword(s):  
Mass Transfer ◽  
High Pressure ◽  
Low Temperature ◽  
Temperature Water

Isotope (δD, δ18O, 3H, δ13C, 14C) and chemical (B, Cl) Constrains on water origin, mixing, water-rock interaction and age of low-temperature geothermal water

2019 ◽  
Vol 108 ◽  
pp. 104380 ◽  
Author(s):  
Andri Stefánsson ◽  
Stefán Arnórsson ◽  
Árný E. Sveinbjörnsdóttir ◽  
Jan Heinemaier ◽  
Hrefna Kristmannsdóttir
Keyword(s):  
Low Temperature ◽  
Geothermal Water ◽  
Rock Interaction ◽  
Water Origin ◽  
Mixing Water ◽  
Water Rock Interaction
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