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Manure and deep tillage management resulted in two distinct groups of soil properties: (1) soils with manure application combined with deep tillage and (2) soils with conventional tillage.
The effects on test organisms exposed to biopile 2 soils were several times higher compared to those in biopile 1 soils, which correlated with the soil contaminants concentration.
Crop placement is determined by evaluating spatial variability of: 1) soils, 2) surface flow pathways, 3) shallow groundwater flow gradients, 4) subsurface nitrate concentrations, and 5) primary crop yield.
Table 1 Soils types within the mine lease boundaries in the Bowen Basin (derived from Queensland Government 2013a ) Soil Coal mine leases in the Bowen Basin Areaea (ha) Total mine leases area Chromosols 16,502 4 Kandosols 47,580 10 Rudosols 4,302 1 Sodosols 141,750 32 Vertosols 236,592 53.
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1) soil properties .
Image credits: 1) Soil sampling a wetland in First State National Park.
The uncontaminated Type 2 soil had pedological features similar to those of contaminated Type 1 soil.
V. corneae was detected in 1 soil water sample.
While the inoculants effectiveness was decreased in 400 mg Zn kg−1 soils, RAM induced significantly higher biomass production under all soil Zn treatments.
Duraisamy et al. (1988) also reported that the application of zinc (10 20 mg kg−1 soils) to rice crop improved the availability of zinc in soil.
Soil organic carbon stocks in the soil profiles were calculated as follows (Batjes 1996): Td = sumlimits_{i = 1}^{k} {rho iPiDi,,left( {1 - Si} right)}, (1 where Td = SOC stocks over depth (d) of layer (Mg m−2), ρi = BD of layer i (Mg m−3), Pi = C content of layer i (mg C g−1 soils), Di = thickness of layer i (m), and Si = percentage of rock fragment particles >2 mm in layer i.
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