Background colours are based on δ13C values of soil organic matter from soils supporting C3 and C4 plants as reported by Dümig et al.25.
Mean values of soil thickness are 1.08, 0.62 and 0.45 m in lynchets, undulations and undifferentiated areas, respectively.
The results showed the importance of heat transfer losses by radiation, particularly for low values of soil heat flux (SHF).
The characteristic values of shear strength parameters were evaluated basing on the effective values of soil parameters.
Surrogate values of soil water were obtained with a locally calibrated neutron probe adjacent to EM38 measurements.
The average values of soil moisture were on the order of farmland > orchard > grassland > abandoned land > shrubland > forestland.
Descriptive statistics and ANOVAs of sub-datasets by region and soil textural class for all CASH indicators were performed, allowing comparisons among these three regions in measured values of soil health indicators.
Theoretical estimates of soil carbon sequestration in Australian farming systems often do not coincide with measured values of soil carbon, possibly due to post sequestration carbon losses.
After 18 months, the average values of soil ECe for five treatments were 2.32 and 2.78 dS/m in 0 35 and 0 95 cm soil profile, respectively.
The model uses no adjustable parameters, but proceeds from first principles based upon known or estimated values of soil properties as a function of depth.
In general, shrub and herbaceous cover was higher on southern slopes with a more diverse overstorey, high values of soil temperature and low values of litter cover.
