[1]阿斯耶姆·图尔迪,李新国,靳万贵,等.开都河流域下游绿洲土壤盐渍化影响因子分析[J].水土保持研究,2014,21(02):82-86.
　Asiyemu·Tuerdi,LI Xin-guo,JIN Wan-gui,et al.Analysis of Affecting Factors of Oasis Soil Salinization in the Lower Reaches of Kaidu River Basin[J].Research of Soil and Water Conservation,2014,21(02):82-86.
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开都河流域下游绿洲土壤盐渍化影响因子分析

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 21 期数: 2014年02期 页码: 82-86 栏目: 出版日期: 2014-04-28
Title:
Analysis of Affecting Factors of Oasis Soil Salinization in the Lower Reaches of Kaidu River Basin
作者:
阿斯耶姆·图尔迪1,2, 李新国1,2, 靳万贵1,2, 梁东1,2
1. 新疆师范大学 地理科学与旅游学院, 乌鲁木齐 830054;
2. 新疆干旱区湖泊环境与资源实验室, 乌鲁木齐 830054
Author(s):
Asiyemu·Tuerdi1,2, LI Xin-guo1,2, JIN Wan-gui1,2, LIANG Dong1,2
1. School of Geographic Sciences and Tourism, Xinjiang Normal University, Urμmqi 830054, China;
2. Xinjiang Laboratory of Lake Environment and Resources in Arid Zone, Urμmqi 830054, China
关键词:
土壤盐渍化; 影响因子; 土壤含盐量; 灰色关联度; 开都河流域下游绿洲
Keywords:
soil salinization; affecting factor; soil salt content; grey correlation degree; oasis in the lower reaches of Kaidu River
分类号:
S156.4
摘要:
以开都河流域下游绿洲为例，应用灰色关联度方法分析了6种影响因子在土地盐渍化过程的相对影响力大小。结果表明：自然和人为因素共同作用于研究区土壤盐渍化过程。土壤含盐量与土壤盐渍化影响因子之间的关联度排序0—10 cm层为：地下水埋深 > 最近排水渠距离 > 高程 > 最近灌溉水渠距离 > 最近湖岸距离 > 地下水矿化度；10—30 cm层为：地下水埋深 > 最近湖岸距离 > 最近排水渠距离 > 高程 > 最近灌溉水渠距离 > 地下水矿化度；30—50 cm层：最近灌水渠距离 > 地下水埋深 > 最近排水渠距离 > 地下水矿化度 > 最近湖岸距离 > 高程。在3个不同土层深度上土壤盐渍化影响因子的影响力不同，土壤盐渍化防治需要综合考虑多种影响因子的作用。
Abstract:
Through the spatial factor and experimental data analysis of oasis soil salinization of Kaidu River Basin, taking the downstream oasis as an example, using application of grey correlation degree analysis of each factor in size relative influence of land salinization process, six impact factors were selected. The results showed that the natural and anthropic factors commonly influenced soil salinization. Soil moisture correlation in 0—10 cm layer between the amount of salt and influencing factors ranked in the order of groundwater depth > recent drainage distance > elevation > recent irrigation canals distance > recent lake distance > mineralization of groundwater; for 10—30 cm layer, groundwater depth > recent lake distance > recent drainage distance > elevation > recent irrigation canals distance > mineralization of groundwater; for 30—50 cm, recent irrigation distance > groundwater depth > recent drainage distance > mineralization of groundwater > recent lake distance > elevation. Each one in each soil depth on influence factors is different, soil salinization of land in the area is complex, its governance work required a comprehensive consideration of all factors.

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备注/Memo

收稿日期:2013-08-01;改回日期:2013-08-27。
基金项目:新疆维吾尔自治区自然科学基金项目（2012211A053）
作者简介:阿斯耶姆·图尔迪(1988-),女(维吾尔族),新疆且末县人,硕士研究生,主要从事干旱区土壤资源变化及其遥感应用研究。E-mail:asiya.tr@gmail.com
通讯作者:李新国(1971-),男,甘肃玉门人,博士,教授,硕士生导师,主要从事干旱区水土资源变化研究。E-mail:onlinelxg@sina.com

更新日期/Last Update: 1900-01-01