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For instance, the increase of soil temperature may cause the decrease of soil moisture (Kirschbaum 1995; Davidson et al. 1998).
The mean comparison results of different CR application rate indicated that the application of CR cause significant decrease of soil bulk density (BD) in both soils.
A substantial decrease of soil erosion rates on arable slopes has been equally reflected in a corresponding decrease of aggradation rates in the main valley bottom and tributaries.
According to the classification of PI, 60% of the groundwater samples come under suitable category (class I) and the rest 40% come under marginally suitable category (class II) for irrigation due to decrease of soil permeability.
The trend of gradual decrease of soil porosity of the unaltered farmland with increasing soil depth observed in this study was consistent with the above references (Foth 1990; Hausenbuiller 1985).
In burned areas, a decrease of total N and microbial biomass N, and a slow-down of N- and P-cycle enzymatic activities were observed in the mid-term coinciding with a decrease of soil moisture.
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There was a decrease of soil-water with time for fertilizer treatments.
The results demonstrate a significant improvement of voluntary bowel movements or the ability to decide when to pass stools, as well as a significant decrease of soiling and constipation.
Burning at 150 200 °C resulted in decreasing of soil pH, whilst heating at 300 500 °C caused increase of pH compare to unheated soils.
However, less is known about the consequences of global warming-induced decreases of soil water on alpine wetland ecosystems on the Qinghai-Tibetan Plateau.
Clay may lead to decrease aeration of soil, but sand may lead to penetrate more water and air as well as decreasing water holding capacity and increasing rate of drainage in the soil.
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