Pressure-induced ion pairing in MgSO4 solutions: Implications for the oceans of icy worlds
Pressure-induced ion pairing in MgSO4 solutions: Implications for the oceans of icy worlds
复制标题
MgSO4 溶液中压力诱导的离子配对:对冰冷世界海洋的影响
DOI:
10.7185/geochemlet.1707
复制
发表时间:
2017
期刊:
影响因子:
--
通讯作者:
C. Manning
中科院分区:
文献类型:
--
作者:
C. Schmidt;C. Manning
At ambient temperature, liquid water transforms from a low-density to a high-density dynamic structure at ~0.2 GPa. The transition persists in electrolyte solutions; however, its effects on solute properties are unknown. We obtained Raman spectra of 0.5–2.0 molal MgSO 4 solutions at 21 °C and 10 -4 to ~1.6 GPa. Above about 0.4 GPa, we observed an increase in the MgSO 4 contact ion pair abundance with pressure, regardless of concentration. This phenomenon contravenes the general rule that dissolved salts dissociate upon compression, and is likely caused by the structural collapse in the solvent with pressure due to increased hydrogen-bond breaking. Increasing ion association in high-pressure aqueous solutions implies that, at a given salinity, high-density water in deep, cold planetary oceans and pore waters will possess lower ionic strength and electric conductivity than previously thought. This behaviour will also lead to higher ocean salinity in the interiors of Pluto and the largest icy moons of Jupiter and Saturn, Ganymede, Callisto, and Titan, or in exoplanet water-worlds, through enhancement of submarine silicate weathering.
DOI:
10.1088/2041-8205/775/2/l47
发表时间:
2013
期刊:
The Astrophysical Journal Letters
影响因子:
--
作者:
Kaltenegger;Sasselov D;Rugheimer S.
通讯作者:
Rugheimer S.
影响因子:
5
作者:
Valenti P;Bodnar R.J;Schmidt C.
通讯作者:
Schmidt C.
DOI:
10.1002/2014ja020778
发表时间:
2015
期刊:
Journal of Geophysical Research: Space Physics
影响因子:
--
作者:
Duling;Strobel;Feldman;Hartkorn
通讯作者:
Hartkorn