Soil Physical Characteristics on Different Degraded Alpine Grasslands in Maqu County in Upper Yellow River
|更新时间:2025-03-12
|
Soil Physical Characteristics on Different Degraded Alpine Grasslands in Maqu County in Upper Yellow River
Bulletin of Soiland Water ConservationVol. 29, Issue 5, Pages: 16-21(2010)
作者机构:
甘肃省林业科学研究院,甘肃,兰州,730020
作者简介:
基金信息:
DOI:
CLC:
Published:2010
稿件说明:
移动端阅览
WEI Qiang, WANG Fang, CHEN Wenye, et al. Soil Physical Characteristics on Different Degraded Alpine Grasslands in Maqu County in Upper Yellow River[J]. Bulletin of Soiland Water Conservation, 2010, 29(5): 16-21.
DOI:
WEI Qiang, WANG Fang, CHEN Wenye, et al. Soil Physical Characteristics on Different Degraded Alpine Grasslands in Maqu County in Upper Yellow River[J]. Bulletin of Soiland Water Conservation, 2010, 29(5): 16-21.DOI:
Soil Physical Characteristics on Different Degraded Alpine Grasslands in Maqu County in Upper Yellow River
The soil physical characteristics on five types of degraded alpine grasslands in Maqu County in the Upper Yellow River were studied.Results showed that soil bulk density
porosity
moisture capacity
and water storage capacity in 0—30 cm soil layer of the five degraded grasslands were significantly different.Soil bulk density increased with the aggravation of degraded alpine grasslands and also increased with the increment of soil depth.The corresponding values ranged from 1.085 to 1.447 g/cm3 and 1.111 to 1.248 g/cm3
respectively.Soil total porosity
maximum moisture capacity
and total water storage capacity decreased with the aggravation of degraded grasslands
their range values were 46.214%~58.162%
26.765%~52.369%
and 1 386.420~1 744.872 t/hm2
respectively.The soil physical characteristics decreased with the increment of soil depth and the range values were 52.783%~57.285%
40.504%~50.057%
and 527.833 t/hm2~572.852 t/hm2
respectively.Soil permeability firstly decreased with the aggravation of degraded grasslands and then increased.By soil permeability
the order of grasslands was moderately degraded grasslandslightly degraded grasslandheavily degraded grasslandnon-degraded grasslandextremely degraded grassland.Study of infiltration process indicated that soil permeability of non-degraded grassland was good and its water conservation function was better than heavily degraded grassland.