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Samples were removed from the soil with a maximum of 8 mm soil attached to them.
The POM was separated by size fractionation (> 53 μm) from coarsely sieved (> 6 mm) soil.
Each pot contained 8 kg dried and sieved (2 mm) soil collected from the University research area.
In the grass patch, macropores were distributed mainly in the 0 200 mm soil layer, while in the shrub patch, they were found throughout the 0 400 mm soil layer.
N mineralization and N2O N emissions were positively correlated with the amount of large (> 2 mm) soil aggregates.
The extraction of pore network visualizations and quantifications from SR-μCT data is demonstrated on a 5 mm soil aggregate.
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Burning depth varied between 24 mm (soils from the top of the gradient) to 12 mm (slope and foot soils) indicating a difference in flammability.
As expected, the 0.5-mm soil particle diameter had the highest excess shear and potential erosion while the 32 mm had the lowest excess shear stress for the current scenario without any GI.
SOCc was highest in the most eroded shoulder-backslope zone (Z2) though soil organic carbon storage (SOCs) there was the lowest because of the zone's high >2-mm soil fraction.
Sub-samples of the initial soil samples were air dried, sieved and the <2-mm soil fraction analysed for total organic carbon using a LECO FPS-2000 CNS thermal combustion furnace (modified Dumas method) and pH using 1 2.5 soil to water ratio.
In a quest for submergence tolerance at the seedling stage, Yamauchi et al. (1993) screened 258 accessions from the International Rice Research Institute (IRRI) gene bank and 404 from the International Network for the Genetic Evaluation of Rice (INGER), using seeds pre-germinated for 2 days and then sown at 25-mm soil depth and submerged with 20 50 mm of water.
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