Saline water irrigation scheduling through a crop-water-salinity production function and a soil-water-salinity dynamic model

被引:26
|
作者
Wang Yang-Ren
Kang Shao-Zhong [1 ]
Li Fu-Sheng
Zhang Lu
Zhang Jian-Hua
机构
[1] China Agr Univ, Ctr Agr Water Res China, Beijing 100083, Peoples R China
[2] Tianjin Agr Univ, Dept Water Conservancy Engn, Tianjin 300384, Peoples R China
[3] Guangxi Univ, Agr Coll, Nanning 530005, Peoples R China
[4] CSIRO, Land & Water, Canberra, ACT 2601, Australia
[5] Hong Kong Baptist Univ, Dept Biol, Kowloon Tang, Hong Kong, Peoples R China
基金
中国国家自然科学基金;
关键词
crop-water-salinity production function; irrigation scheduling; saline water irrigation; water-salinity dynamic model; CARTHAMUS-TINCTORIUS L; NONSALINE WATERS; CONJUNCTIVE USE; CAPILLARY RISE; YIELD RESPONSE; SIMULATION; WHEAT; VALIDATION;
D O I
10.1016/S1002-0160(07)60037-X
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Using a crop-water-salinity production function and a soil-water-salinity dynamic model, optimal irrigation scheduling was developed to maximize net return per irrigated area. Plot and field experiments were used to obtain the crop water sensitivity index, the salinity sensitivity index, and other parameters. Using data collected during 35 years to calculate the 10-day mean precipitation and evaporation, the variation in soil salinity concentrations and in the yields of winter wheat and cotton were simulated for 49 irrigation scheduling that were combined from 7 irrigation schemes over 3 irrigation dates and 7 salinity concentrations of saline irrigation water (fresh water and 6 levels of saline water). Comparison of predicted results with irrigation data obtained from a large area of the field showed that the model was valid and reliable. Based on the analysis of the investment cost of the irrigation that employed deep tube wells or shallow tube wells, a saline water irrigation schedule and a corresponding strategy for groundwater development and utilization were proposed. For wheat or cotton, if the salinity concentration was higher than 7.0 g L-1 in groundwater, irrigation was needed with only fresh water; if about 5.0 g L-1, irrigation was required twice with fresh water and once with saline water; and if not higher than 3.0 g L-1, irrigation could be solely with saline water.
引用
收藏
页码:303 / 317
页数:15
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