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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.
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Samples were removed from the soil with a maximum of 8 mm soil attached to them.
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.
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.
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.
Carbonate dissolution rates amounted to approximately 1.7 3.0 mol m−2 year−1 if they are referred (normalised) to 1000 mm soil water fluxes.
The soil aggregate percents (SAP) > 0.84 mm and soil fragment percents (SFP) < 0.42 mm, water stable aggregate (WSA) > 0.5, WSA > 0.25 mm, soil bulk density (BD), and soil water infiltration were also measured in this study.
The simulated total ET during the entire growth period in 2013 was 332.41 mm, including 215.13 mm grassland transpiration (64.7%) and 117.28 mm soil evaporation.
Soil organic carbon content (SOC), texture, pH, carbonate content, electrical conductivity and cation exchange capacity were also determined on the air-dried and sieved (2 mm) soil.
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