《Table 2 Soil properties of the selected sites》

《Table 2 Soil properties of the selected sites》   提示：宽带有限、当前游客访问压缩模式
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《"Changes in soil properties and erodibility of gully heads induced by vegetation restoration on the Loess Plateau, China"》


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Note:CLA，clay content；SIL，silt content；SAN，sand content；SBD，soil bulk density；STP，soil total porosity；SDR，soil disintegration rate；SHC，soil saturated hydraulic conductivity；SOM，soil organic matter.Different lowercase letters and capital letters in

As shown in Table 2，the soil bulk density of cropland was 1.16 g/cm3，and the average soil bulk density of grassland，woodland and shrubland was 4.31%，7.76%and 2.59%greater than that of cropland，respectively.No significant difference was found among the soil bulk density values of the 3 land-use types，indicating that the soil bulk density was not affected by land uses.For the 5sites in the grassland，the soil bulk density values of GA（1.31 g/cm3）and GC（1.26 g/cm3）were significantly higher than those of the other 3 sites（P<0.05），with the lowest soil bulk density（1.12 g/cm3）in GCC.For woodland and shrubland，WP had the highest bulk density（1.35g/cm3），with no significant difference with the other sites.Similarly，land uses had no significant effect on soil total porosity（Table 2）.Among the 10 sites，the highest soil total porosity（57.66%）was in GCC and the lowest（49.08%）in WP.The soil total porosity values of GA，GC and WPwere 9.55%，6.35%and 12.42%higher than that of CZ，respectively.

图表编号XD0020361800    严禁用于非法目的
绘制时间2018.10.01
作者GUO Mingming、WANG Wenlong、KANG Hongliang、YANG Bo
绘制单位State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation,Northwest A&F University、State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Con
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