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In all the soils investigated, ≤ 2 chroma redox depletions related to an average cumulative annual saturation percentage (CSP) of 15%.
The porosimetry provides evidence that the microstructural array in particles of three of the soils investigated is determined primarily by the platelet character of quasicrystalline clay minerals while that of another one of the soils, an Oxisol, appears to be dominated by its high iron oxide content.
No significant effect was observed of ash type or BE addition or an interaction between the two factors for any of the two soils investigated (P > 0.05, two-way ANOVA).
In general, the primer set Amx368 820 seemed more effective in capturing anammox bacteria compared to Brod541F Amx820R for the rice paddy soils investigated in this study.
At +10°C (initial level) in soils investigated, carbon dioxide emission varied between 7.4 to 43.8 mg C m-2h-1 depending on land use and moisture.
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For the soil investigated, the cohesion decreased with the increasing number of freeze thaw cycles, and the friction angle exhibit an increasing trend.
The results of the study show that for the soil investigated, the increase in the number of freeze thaw cycles results in the decrease of unconfined compressive strength of clay samples by 20 25%.
The clayey type of the soil investigated in this study may influence the infiltration rate which makes it slower.
Soil laboratory analyses results of Atterberg Limits with sieve analysis places the soil investigated in quite a wide range of soil types.
This possibility was confirmed by our microrespirometric data showing a higher active microbial biomass content in the upper layers of the soil investigated.
The decrease of values obtained using SIR measurements with the depth of soil indicates a higher active microbial biomass content in the upper layers of soil investigated (Table 2).
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