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Some water chemistry parameters, pH, conductivity, oxygen content and soil moisture tension were also monitored.
Both organic matter content and soil pH have increased considerably since 1971.
It is known to be influenced both by the organic matter content and soil biota.
However, those models rarely consider the combined effects of initial volumetric water content and soil density.
The differences in the P losses could be associated with the difference in the initial P content and soil texture.
The main soil characteristics, soil nitrogen (N) content, and soil carbon to nitrogen (C/N) ratio were also determined.
Mean soil water downward movement varied between 0.029 1379 mm h−1, depending on water content and soil depth.
The soil water retention curve (SWRC) is a unique relationship between water content and soil water potential.
There are two basic methods to measure the amount of water in the soil: soil water content and soil water potential measurements [10].
In fact, plant productivity appears to increase by a reduced turnover of the microbial biomass due to stabilized carbon content and soil pH.
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The ranches vary somewhat in slope, sand content, and soil-carbon content, and even before the fragments were created there were certain differences in tree abundance and species composition, but not tree-species richness, among the ranches (see Protocol S1).
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