Pressure solution
compaction of sodium chlorate and implications for pressure solution in NaCl Bas den Brok
Institut für Geowissenschaften, Johannes Gutenberg-Universität, 55099 Mainz, Germany
Published in 1999 in Tectonophysics 307, pp. 297-312 doi:10.1016/S0040-1951(99)00103-1
Abstract
Sodium chloride (NaCl) has been extensively used as a material to develop, test and improve pressure solution (PS) rock deformation models. However, unlike silicate and carbonate rocks, NaCl can deform plastically at very low stresses (~0.5 MPa). This could mean that NaCl is less suitable for use as an analogue for rocks that do not deform plastically at conditions where PS is important. In order to test the reliability of NaCl as a rock analogue, we carried out a series of uniaxial compaction experiments on sodium chlorate (NaClO
3) at room pressure and temperature (P-T) conditions and applied effective stresses of 2.4 and 5.0 Mpa. NaClO3 is a very soluble, elastic-brittle salt, that cannot be deformed plastically at room P-T conditions. The results were compared with experiments on NaCl at similar conditions and show that NaClO3 behaves in a strikingly similar way to NaCl, despite its brittleness. Like NaCl, it most likely compacts by a grain boundary diffusion controlled PS mechanism. Mechanical data were fitted to a power law in the form:(with volumetric strain rate
Keywords: pressure solution, deformation, mechanical properties, diagenesis, sodium chloride, salt tectonics.
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