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塔里木盆地西南缘灌区低洼农田水盐运移特征/Soil Water and Salt Migration of Low-lying Parts of Irrigation Area in the Southwestern Tarim Basin[J]
Authors
中国科学院大学,北京100049
中国科学院新疆生态与地理研究所,新疆乌鲁木齐,830011
+6 more
中国科学院新疆生态与地理研究所,新疆乌鲁木齐830011
乔木
宋鹏
尹传华
徐薇薇
田长彦
Publication date
1 January 2014
Publisher
Abstract
为科学治理塔里木盆地西南缘灌区重度盐渍化,对其一处低洼农田水盐进行监测.结果显示:排除漫灌影响,7月初至11月初,农田地下水埋深呈单峰型,表现为监测前期缓慢上升,8月初达到最大值,后波动性降低;而地下水矿化度一直缓慢降低.0~60 cm土壤总盐量表现为单峰型,监测前期缓慢升高,8月达到最大值,后缓慢降低.相关分析表明,整个监测时期,农田地下水埋深、矿化度、0~60 cm总盐量均表现为正相关,且随着土壤深度的增加,总盐量与地下水埋深、矿化度的相关程度增大
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Last time updated on 29/11/2016