干旱区生态环境知识资源中心(Arid): 山地森林-干旱河谷交错带表层土壤侵蚀率与土壤物理性质的关系

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	山地森林-干旱河谷交错带表层土壤侵蚀率与土壤物理性质的关系
其他题名	Relationship Between Surface Soil Erosion Rate and Soil Physical Properties in a Mountain Forests-Arid Valley Ecotone
	何淑勤 1; 宫渊波 1; 郑子成 2; 王玲 1
来源期刊	资源科学
ISSN	1007-7588
出版年	2013
卷号	35 期号:4 页码:824-830
中文摘要	采用野外调查与室内分析相结合的方法,研究了山地森林-干旱河谷交错带表层土壤侵蚀率及其与土壤物理性质的关系。结果表明:岷江上游干旱河谷区不同植被条件下表层土壤侵蚀较为严重,平均土壤侵蚀率为27.58%。土壤侵蚀率与土壤结构破坏率(SPBR)极显著正相关;与土壤有机质含量、>0.25mm水稳性团聚体含量(WSA)、湿筛后团聚体平均重量直径(MWD)和几何平均直径(GMD)显著负相关。土壤侵蚀率分别与土壤有机质含量、结构破坏率、湿筛后团聚体MWD和GMW、>0.25mm水稳性团聚体含量建立的回归方程预测效果相对较好。
英文摘要	Soil erosion is the main cause of land degeneration, and can be considered a natural disaster restricting human survival and development of the global environment. Using field investigations and laboratory analyses, surface soil erosion rate and the relationship between soil erosion rate and soil physical properties in dry valleys of the upper Minjiang River were studied. We found severe soil erosion and an average erosion rate of 27.58% across vegetation types. Soil erosion was the most serious for Robinia pseudoacacia, and minor for the conversion of farmland to Minjiang cypress. The soil erosion rate of Robinia pseudoacacia was 3.28 times that of conversion of farmland to Minjiang cypress. Soil erosion rate was correlated with the structure ped breaking ratio(SPBR). The clay ratios were less than 0.30 for the different vegetation types, and soil coarsening was widespread. Sand and coarse silt content were significantly higher than those of fine silt and clay content, and clay content was lowest. Average organic matter content was 45.73 g / kg for topsoil. Soil erosion rates were correlated with soil organic matter content, >0.25 mm water-stable aggregate content, aggregate mean weight diameter(MWD)and geometric mean diameter (GMD) after wet sieving. The change characteristic of stable aggregate content and organic matter content showed synchronization. Strengthening existing shrub and natural secondary forest protection, reducing human disturbance, and implementing natural recovery would contribute to the accumulation of soil organic matter in the mountain forests-arid valley ecotone. These measures would inhibit the expansion of the dry valley and extend the ecological functions of subalpine forest. This study reveals the essence of soil erosion and provides a theoretical basis for ecological construction and the conversion of farmland to forest.
中文关键词	山地森林/干旱河谷交错带 ; 土壤侵蚀率 ; 土壤物理性质 ; 不同植被
英文关键词	Mountain forests-arid valley ecotone Soil erosion rate Soil physical properties Different vegetation
语种	中文
国家	中国
收录类别	CSCD
WOS类目	FORESTRY
WOS研究方向	Forestry
CSCD记录号	CSCD:4818040
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/230748
作者单位	1.四川农业大学林学院, 林业生态工程四川省省级重点实验室, 雅安, 四川 625014, 中国; 2.四川农业大学资源环境学院, 成都, 四川 611130, 中国
推荐引用方式 GB/T 7714	何淑勤,宫渊波,郑子成,等. 山地森林-干旱河谷交错带表层土壤侵蚀率与土壤物理性质的关系[J],2013,35(4):824-830.
APA	何淑勤,宫渊波,郑子成,&王玲.(2013).山地森林-干旱河谷交错带表层土壤侵蚀率与土壤物理性质的关系.资源科学,35(4),824-830.
MLA	何淑勤,et al."山地森林-干旱河谷交错带表层土壤侵蚀率与土壤物理性质的关系".资源科学 35.4(2013):824-830.