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Properties of CO2 clathrate hydrates formed in the presence of MgSO4 solutions with implications for icy moons

DOI: 10.1051/0004-6361/201629791 DOI Help

Authors: Emmal Safi (Keele University; Diamond Light Source) , Stephen P. Thompson (Diamond Light Source) , A. Evans (Keele University) , S. J. Day (University of Keele) , C. A. Murray (Diamond Light Source) , J. E. Parker (Diamond Light Source) , A. R. Baker (Diamond Light Source) , J. M. Oliveira (Keele University) , J. Th. Van Loon (Keele University)
Co-authored by industrial partner: No

Type: Journal Paper
Journal: Astronomy & Astrophysics

State: Published (Approved)
Published: January 2017
Diamond Proposal Number(s): 9703 , 11174

Abstract: Context. There is evidence to suggest that clathrate hydrates have a significant effect on the surface geology of icy bodies in the Solar System. However the aqueous environments believed to be present on these bodies are likely to be saline rather than pure water. Laboratory work to underpin the properties of clathrate hydrates in such environments is generally lacking. Aims. We aim to fill this gap by carrying out a laboratory investigation of the physical properties of CO2 clathrate hydrates produced in weak aqueous solutions of MgSO4. Methods. We use in situ synchrotron X-ray powder diffraction to investigate clathrate hydrates formed at high CO2 pressure in ice that has formed from aqueous solutions of MgSO4 with varying concentrations. We measure the thermal expansion, density and dissociation properties of the clathrates under temperature conditions similar to those on icy Solar System bodies. Results. We find that the sulphate solution inhibits the formation of clathrates by lowering their dissociation temperatures. Hysteresis is found in the thermal expansion coefficients as the clathrates are cooled and heated; we attribute this to the presence of the salt in solution. We find the density derived from X-ray powder diffraction measurements is temperature and pressure dependent. When comparing the density of the CO2 clathrates to that of the solution in which they were formed, we conclude that they should sink in the oceans in which they form. We also find that the polymorph of ice present at low temperatures is Ih rather than the expected Ic, which we tentatively attribute to the presence of the MgSO4. Conclusions. We (1) conclude that the density of the clathrates has implications for their behaviour in satellite oceans as their sinking and floating capabilities are temperature and pressure dependent, (2) conclude that the presence of MgSO4 inhibits the formation of clathrates and in some cases may even affect their structure and (3) report the dominance of Ih throughout the experimental procedure despite Ic being the stable phase at low temperature.

Journal Keywords: Molecular data; surfaces; Europa; Enceladus

Subject Areas: Earth Science, Chemistry


Instruments: I11-High Resolution Powder Diffraction