http://researchonline.federation.edu.au/vital/access/manager/Index ${session.getAttribute("locale")} 5 http://researchonline.federation.edu.au/vital/access/manager/Repository/vital:1078 Wed 07 Apr 2021 13:32:06 AEST ]]> http://researchonline.federation.edu.au/vital/access/manager/Repository/vital:863 Wed 07 Apr 2021 13:31:51 AEST ]]> http://researchonline.federation.edu.au/vital/access/manager/Repository/vital:862 Wed 07 Apr 2021 13:31:51 AEST ]]> http://researchonline.federation.edu.au/vital/access/manager/Repository/vital:860 smectite > mixed-layer (ML) ≈ vermiculite. The soil clay mineralogy did not change systematically with depth (0- 10, 10- 20 and 20- 30 cm) and showed large variations spatially. The high proportion of kaolinite was probably due to the removal of 2:1 phyllosilicates by the formation of 1:1 kaolinite through weathering, which also reduced the cation exchange capacity (CEC) and electrical conductivity (EC, soil: water ratio of 1:5) of soils by aging. Soils were classified as silty loam to loam with a low clay size (≤ 2]]> Wed 07 Apr 2021 13:31:51 AEST ]]>