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新疆典型小流域土壤水稳性团聚体分布特征研究
引用本文:柴仲平,王雪梅,陈波浪,孙霞,贾宏涛. 新疆典型小流域土壤水稳性团聚体分布特征研究[J]. 水土保持通报, 2009, 23(3): 94-96,102
作者姓名:柴仲平  王雪梅  陈波浪  孙霞  贾宏涛
作者单位:柴仲平,陈波浪,孙霞,贾宏涛(新疆农业大学草业与环境科学学院,新疆,乌鲁木齐,830052);王雪梅(新疆师范大学地理科学与旅游学院,新疆,乌鲁木齐,830054) 
基金项目:973课题"新疆绿洲棉田土壤质量演变规律与可持续利用研究",自治区科技攻关,重点项目计划课题"果树营养特性与水肥耦合技术研究",土壤学自治区重点学科资助 
摘    要:新疆是全国水土流失面积大区.以新疆典型小流域-阜康市三工河流域为例,对区域土壤水稳性团聚体分布特征及其影响因素做了初步研究,旨在为小流域土壤侵蚀治理提供重要参考依据.通过对流域内典型梁峁坡地、不同坡度坡地及不同植被覆盖地0-20 cm和20-50 cm剖面层土壤进行采样分析.结果表明,该流域土壤水稳性团聚体含量分布存在以下特征:土壤同-剖面自上而下呈递减趋势;同一坡面随坡位自上而下呈增加趋势;不同坡度则随坡度的增加而减少;不同植被覆盖度土壤水稳性团聚体含量呈现:农用坡耕地<林地<草地<草灌地.

关 键 词:新疆  水土流失  小流域  水稳性团聚体  分布特征
收稿时间:2008-09-03
修稿时间:2008-11-18

Distribution Characteristics of Soil Water Stable Aggregates in a Small Typical Watershed of Xinjiang Wei Autonomous Region
CHAI Zhong-ping,WANG Xue-mei,CHEN Bo-lang,SUN Xia and JIA Hong-tao. Distribution Characteristics of Soil Water Stable Aggregates in a Small Typical Watershed of Xinjiang Wei Autonomous Region[J]. Bulletin of Soil and Water Conservation, 2009, 23(3): 94-96,102
Authors:CHAI Zhong-ping  WANG Xue-mei  CHEN Bo-lang  SUN Xia  JIA Hong-tao
Affiliation:College of Pratacultural and Environmental Science, Xinjiang Agricultural University, Urumqi, Xinjiang 830052, China;;College of Geographical Science and Tourism, Xinjiang Normal University, Urumqi, Xinjiang 830054, China;College of Pratacultural and Environmental Science, Xinjiang Agricultural University, Urumqi, Xinjiang 830052, China;;College of Pratacultural and Environmental Science, Xinjiang Agricultural University, Urumqi, Xinjiang 830052, China;;College of Pratacultural and Environmental Science, Xinjiang Agricultural University, Urumqi, Xinjiang 830052, China;
Abstract:Xinjiang is a large district suffering from soil and water loss in China,but soil erosion processes in the region have not yet been under stood deeply.Taking San'gong River water shed in Fukang City,Xinjiang Wei Autonomous Region,as an example,a preliminary study for the distribution characteristics of waterstable aggregate content and its influence factors was performed to provide an important basis for soil erosion control.Soils of 0-20 cm and 20-50 cm on a typical hilly slope,slopes of different gradients,and vegetation converage of different degrees were analyzed.Results showed that the dist ribution of soil water stable aggregates in the small watershed had the following characteristics:it had a decreasing tendency from surface down to bottom in the same soil profile;on the same slope,it had a increasing tendency from top to bottom;and on slopes of different gradients,it had a decreasing tendency with slope increasing.In terms of the water stable aggregate content under vegetation coverage of different degrees,landuse was in the descendant order of sloping cropland
Keywords:Xinjiang  soil and water loss  small watershed  water stable aggregate  distribution characteristics
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