| 炼山对板栗林地土壤物理性状的影响 |
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| 引用本文： | 沈夫钧,张吉平,唐桂凤.炼山对板栗林地土壤物理性状的影响[J].林业科技,2002,27(2):16-17. |
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| 作者姓名： | 沈夫钧 张吉平 唐桂凤 |
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| 作者单位： | 辽宁省丹东市林业局，丹东 118000 |
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| 摘 要： | 炼山后板栗林地土壤孔隙度大大增加 ,其增加程度取决于非毛管孔隙度的增加 ;土壤中大于 0 .2 5 mm的水稳性团聚体含量降低 ,虽改善了土壤的通透性和肥力 ,但遇强降雨时 ,坡度较大的林地易引发水土流失
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| 关 键 词： | 炼山 土壤孔隙度 土壤团聚体组成 |
| 文章编号： | 1001-9499(2002)02-0016-02 |
| 修稿时间： | 2001年12月6日 |
Effect of Mountain Smelting on the Soil Physical Features of Castanea mollissima Stands |
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| SHEN Fujun.Effect of Mountain Smelting on the Soil Physical Features of Castanea mollissima Stands[J].Forestry Science & Technology,2002,27(2):16-17. |
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| Authors: | SHEN Fujun |
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| Abstract: | The soil porosity increase greatly after mountain smelting and the increase degree depend on the increase of uncapillary porosity. Despite the decrease of water steady granule quantity bigger than 0.25 mm in the soil improving the aerate and fertility of soil,stands on steeper slope take place soil erosion easily when it meet strong rainfall. |
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| Keywords: | Mountain smelting Soil porosity Soil granule composition |
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