Cl/Br and δ 37 Cl evolution in seawater expelled during the compaction of MX-80 smectite
Cl/Br and δ 37 Cl evolution in seawater expelled during the compaction of MX-80 smectite
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Language
English
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Contents
During a high pressure (up to 150 MPa) high temperature (up to 150°C) compaction experiment of MX-80 smectite equilibrated with ocean water, it was found that the Cl and Br concentrations in the expelled solution are progressively being decreased while simultaneously being increased in the compacted clay. This significant retention of Cl and Br in...
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Full title
Cl/Br and δ 37 Cl evolution in seawater expelled during the compaction of MX-80 smectite
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TN_cdi_crossref_primary_10_1051_e3sconf_20199812022
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_crossref_primary_10_1051_e3sconf_20199812022
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ISSN
2267-1242
E-ISSN
2267-1242
DOI
10.1051/e3sconf/20199812022
