Soil macropore characteristics under typical vegetations in Liupan Mountains

The radius and density of soil macropores under eight typical vegetations in Liupan Mountains of Northwest China were studied by using water breakthrough curves and Poiseuille equation. The results indicated that the radii of soil macropores ranged from 0.4 mm to 2.3 mm, and the weighted mean radii...

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Published inYing yong sheng tai xue bao Vol. 18; no. 12; p. 2675
Main Authors Shi, Zhong-Jie, Wang, Yan-Hui, Xu, Li-Hong, Yu, Peng-Tao, Xiong, Wei, Xu, Da-Ping
Format Journal Article
LanguageChinese
Published China 01.12.2007
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Abstract The radius and density of soil macropores under eight typical vegetations in Liupan Mountains of Northwest China were studied by using water breakthrough curves and Poiseuille equation. The results indicated that the radii of soil macropores ranged from 0.4 mm to 2.3 mm, and the weighted mean radii ranged from 0.57 mm to 1.21 mm, with a mean of 0.89 mm. The density of soil macropores ranged from 57 individuals per dm2 to 1 117 individuals per dm2, with a mean of 408 individuals per dm2. The macropores with radii bigger than 1.4 mm had a lower density, accounting for only 6.86% of the total. The area proportion of soil macropores ranged from 0.76% to 31.26%, with a mean of 10.82%. In study area, the density of soil macropores was higher in broadleaf forest than in coniferous forest, but basically the same in sub-alpine meadow and in broadleaf forest, as well as in shrubs and in coniferous forest. As for the area proportion of soil macropores, it was also higher in broadleaf forest than in coniferous forest, bu
AbstractList The radius and density of soil macropores under eight typical vegetations in Liupan Mountains of Northwest China were studied by using water breakthrough curves and Poiseuille equation. The results indicated that the radii of soil macropores ranged from 0.4 mm to 2.3 mm, and the weighted mean radii ranged from 0.57 mm to 1.21 mm, with a mean of 0.89 mm. The density of soil macropores ranged from 57 individuals per dm2 to 1 117 individuals per dm2, with a mean of 408 individuals per dm2. The macropores with radii bigger than 1.4 mm had a lower density, accounting for only 6.86% of the total. The area proportion of soil macropores ranged from 0.76% to 31.26%, with a mean of 10.82%. In study area, the density of soil macropores was higher in broadleaf forest than in coniferous forest, but basically the same in sub-alpine meadow and in broadleaf forest, as well as in shrubs and in coniferous forest. As for the area proportion of soil macropores, it was also higher in broadleaf forest than in coniferous forest, bu
Author Wang, Yan-Hui
Shi, Zhong-Jie
Yu, Peng-Tao
Xu, Da-Ping
Xu, Li-Hong
Xiong, Wei
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Snippet The radius and density of soil macropores under eight typical vegetations in Liupan Mountains of Northwest China were studied by using water breakthrough...
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StartPage 2675
SubjectTerms Altitude
China
Coniferophyta - growth & development
Plant Roots - growth & development
Plant Roots - metabolism
Poaceae - growth & development
Porosity
Soil - analysis
Trees - growth & development
Title Soil macropore characteristics under typical vegetations in Liupan Mountains
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Volume 18
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