SCHRIFTENREIHE Institut für Pflanzenernährung und Bodenkunde ...
SCHRIFTENREIHE Institut für Pflanzenernährung und Bodenkunde ...
SCHRIFTENREIHE Institut für Pflanzenernährung und Bodenkunde ...
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Chapter 2 Spatial variability of soil properties affected by grazing intensity in Inner Mongolia grassland<br />
Table 2.1. Descriptive statistics of soil water content measured on three sampling soil water<br />
statuses in 2004.<br />
Treatment<br />
Sampling soil<br />
Water<br />
statuses<br />
Min. Max. Mean SD CV Skewness Kurtosis<br />
UG 79 Dry 0.03 0.09 0.06 0.01 20.00 0 -0.11<br />
Wet 0.24 0.37 0.30 0.03 9.00 0.16 -0.45<br />
Medium 0.10 0.24 0.17 0.03 17.75 0.23 -0.28<br />
UG 99 Dry 0.04 0.10 0.07 0.02 21.43 -0.04 -0.07<br />
Wet 0.31 0.40 0.36 0.02 6.39 -0.13 -0.79<br />
Medium 0.12 0.31 0.22 0.03 12.73 -0.04 0.43<br />
WG Dry 0.02 0.07 0.04 0.01 23.75 0.16 0.52<br />
Wet 0.29 0.38 0.34 0.02 5.29 -0.09 -0.50<br />
Medium 0.15 0.23 0.19 0.02 9.47 -0.02 -0.28<br />
CG Dry 0.02 0.08 0.05 0.01 22.22 0.55 1.27<br />
Wet 0.29 0.38 0.34 0.02 5.33 -0.10 -0.46<br />
Medium 0.12 0.24 0.19 0.03 13.30 -0.05 -0.32<br />
HG Dry - - - - - - -<br />
Wet 0.21 0.34 0.28 0.03 10.79 -0.02 -0.45<br />
Medium 0.07 0.21 0.13 0.03 20.54 0.59 0.74<br />
Min.: Minimum (cm 3 cm -3 ); Max.: Maximum (cm 3 cm -3 ); SD: Standard deviation (cm 3 cm -3 ); CV:<br />
Coefficient of variation (%); -: No data available.<br />
changes of WDPT for the three water statuses. Generally, with increasing water<br />
status the mean WDPT decreased. But WDPT was the highest during the<br />
medium moisture (Sept, 12), which might be due to more litter accumulation or<br />
decomposition corresponding with the late season of growth. WDPT was higher<br />
in the ungrazed plots showing a slight to strong water repellency than in the<br />
grazed plots where the soil was wettable to slight water repellency. The<br />
micro-relief of plant surface covered soil surface as a cuticle, which was<br />
composed of soluble, hydrophobic lipids embedded in a polyester matrix, often<br />
induces effective water repellency (Holloway, 1994; Dekker and Ritsema, 2000).<br />
Because of protection from grazing for 25 years in UG 79 and for 5 years in UG<br />
99, much accumulation of organic matter with hydrophobic components on the<br />
soil surface could have led to the observed relative strong water repellency.<br />
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