Soil salt distribution under mulched drip irrigation in an arid area of northwestern China

被引:56
|
作者
Zhang, Zhi [1 ]
Hu, Hongchang [1 ]
Tian, Fuqiang [1 ]
Hu, Heping [1 ]
Yao, Xinhua [2 ]
Zhong, Ruisen [3 ]
机构
[1] Tsinghua Univ, State Key Lab Hydiosci & Engn, Dept Hydraul Engn, Beijing 100084, Peoples R China
[2] Xinjiang Tarim River Basin Management Bur, Xinjiang 841000, Bayangol Prefec, Peoples R China
[3] Chinese Acad Sci, Xinjiang Inst Ecol & Geog, Urumqi 830011, Xinjiang, Peoples R China
基金
美国国家科学基金会;
关键词
Cotton; Salinization; Salt accumulation; Soil particle size distribution; WATER-USE; SALINITY DISTRIBUTION; LINT YIELD; COTTON; AGRICULTURE; PRINCIPLES; TOLERANCE; ZONES;
D O I
10.1016/j.jaridenv.2014.01.012
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Mulched drip irrigation (MDI) has now become popular in arid and semi-arid areas, under which, however, salts are likely to build up in the surface soil due to deficient leaching water. To explore this new kind of secondary salinization issue, a 3-year experiment was conducted in an arid area in Xinjiang, northwestern China from 2008 to 2011. Over 15,000 soil samples were collected during the experimental years. The patterns of soil salinity distribution under MDI along the horizontal direction as well as vertical direction have been explored. Our results indicate that soil particle size distribution has great impact on soil salt migration and distribution. The salt will build up above the relatively impermeable layer along the soil profile. The zone below drip pipe obtains the lowest salinity level and the salt accumulates in the inter-film zone at the end of growth period. The salinity in the inter-film zone is 1.24-2.34 times the value in the zone below drip pipe within 50 cm soil depth, according to the soil texture. Furthermore, our analysis suggests that surface salinity distribution is dominated by MDI while the influence of MDI on salinity distribution is decreasing with the downward distance from ground surface. (C) 2014 The Authors. Published by Elsevier Ltd. All rights reserved.
引用
收藏
页码:23 / 33
页数:11
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