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The KE and TS decreased with increasing soil water potentials.
Soil salt content increased with increasing soil depth.
SOC storage decreased with increasing soil sampling depth.
The soil CO2 concentrations increased with increasing soil depth, whereas CO2 production decreased with increasing soil depth.
Mycorrhizal dependency significantly (P < 0.05) decreased with increasing soil Olsen-P.
Intact soils showed a significant decrease in big/long diaspores with increasing soil depth.
Soil strength increased with increasing soil depth removal and was significantly reduced by poultry manure.
Larval survival decreased from 80% to 60% with increasing soil pH from 4.8 to 5.7.
Degradation reaction rates of PBDEs increased with increasing ozone concentration but decreased with increasing soil depth.
Soil DP increased with increasing soil moisture content and water-extractable soil organic carbon (WESOC).
The inorganic carbon (IC) behaved oppositely; its rate of production decreased with increasing soil carbon.
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