首页|甘肃疏勒河灌区垂直洗盐制度的模拟研究

甘肃疏勒河灌区垂直洗盐制度的模拟研究

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疏勒河灌区盐渍土面积大,分布范围广,已成为导致流域土地荒漠化的重要原因之一,通过建立垂直洗盐条件下的土壤水盐运移模型,运用数值模拟方法对疏勒河灌区垂直洗盐制度进行了研究,结果表明:第一次冲洗结束后72 h、随后几次冲洗间隔60 h能最大程度的溶解土壤盐分并有效防止表层返盐,取得最佳的脱盐效果;第一次冲洗水量控制在土壤饱和含水率以内,随后几次冲洗水量适当增加的处理TYS3可使脱盐率达91.3%;不同的冲洗定额,处理TYD3比TYD4每方水多脱盐0.0025%,说明冲洗水量太多对脱盐贡献率反而较小。通过以上模拟结果建立了灌区不同初始含盐量情况下的垂直洗盐制度。
Simulation Study on Vertical Salt Leaching System in Shule Irrigation District
With large area and wide distribution,saline soil has become one of the important causes for land desertification in Shule River Basin.Using numerical simulation method by building soil water-salt transport model,vertical salt leaching system was studied.The results showed that,72 h after the first leaching and 60 h intervals for other leaching times could dissolve salt in a maximal degree and prevent salinization effectively.The desalinization ratio reached to 91.3% while the leaching water for the first time was controlled within saturated water content and increased for other times subsequently.The desalinization amount of per cubic meter of TYD3 was 0.0025% higher than TYD4.It showed that contribution rate for too much leaching water was small.The salt leaching system of different salt content was established in Shule River Irrigation District.

Shule River Irrigation DistrictSaline soilSalt leaching system

陈丽娟、冯起、张新民、刘蔚、司建华、席海洋、郭瑞

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中国科学院寒区旱区环境与工程研究所,甘肃兰州730000

甘肃省水利科学研究院,甘肃兰州730000

清华大学水沙科学与水利水电工程国家重点实验室,北京100084

疏勒河灌区 盐渍土 洗盐制度

博士后面上基金国家基金委基金专项

200804403934094007

2010

土壤通报
中国土壤学会

土壤通报

CSTPCDCSCD北大核心
影响因子:0.818
ISSN:0564-3945
年,卷(期):2010.(6)
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