N. J. Barrow

Sep 8, 2023 | bsssjournals.onlinelibrary.wiley.com | Nelly Raymond |Peter Kopittke |N. J. Barrow |Michael Bell

Supporting Information Filename Description ejss13418-sup-0001-Supinfo.pdfPDF document, 1.1 MB Data S1: Supplementary File ejss13418-sup-0002-TableS1.xlsxExcel 2007 spreadsheet , 24.6 KB Table S1: Detailed soil properties for a range of Vertisols from the Northern Grain Region of Australia and other contrasting soils

Feb 22, 2023 | bsssjournals.onlinelibrary.wiley.com | N. J. Barrow

Abstract The partition of materials that react with soil between the solid and the solution phase, and how this changes with time, can often be described by a simple equation: S = a cb1tb2 where S is the amount sorbed, c is the solution concentration, t the time of contact, and a, b1 and b2 are parameters. However, when the range of values for sorption is large, it is apparent that both b1 and b2 increase with decreasing sorption.