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中国沙漠 ›› 2011, Vol. 31 ›› Issue (2): 302-308.

• 2010年烟台沙漠学术研讨会论文选 • 上一篇    下一篇

地下水深埋区咸水灌溉对土壤盐渍化影响的初步研究——以民勤绿洲为例

尤全刚, 薛 娴, 黄翠华   

  1. 中国科学院 寒区旱区环境与工程研究所 沙漠与沙漠化重点实验室, 甘肃 兰州 730000
  • 收稿日期:2010-09-18 修回日期:2010-10-19 出版日期:2011-03-20 发布日期:2011-03-20

Preliminary Study on the Effects of Saline Water Irrigation on Soil Salinization in Deep Groundwater Area: A case study of Minqin oasis

YOU Quan-gang, XUE Xian, HUANG Cui-hua   

  1. Key Laboratory of Desert and Desertification,Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Science, Lanzhou 730000, China
  • Received:2010-09-18 Revised:2010-10-19 Online:2011-03-20 Published:2011-03-20

摘要: 针对民勤绿洲近几十年来大量开采地下水造成地下水位急剧下降,同时大规模开采地下劣质咸水用于农业灌溉的现状,采用咸水沟灌大田试验,就绿洲地下水深埋区(>5 m)咸水灌溉对土壤盐渍化的影响进行了研究。结果表明,在地下水深埋区,灌溉水带入的盐分是土壤表层盐分积累的主要来源;播种前大定额淡水灌溉,土壤明显脱盐,但随着生长季内咸水灌溉及灌溉定额的减少,土壤开始返盐,到生长季末,根区土壤显著积盐,2 g·L-1和5 g·L-1咸水灌溉下土壤的积盐率分别为22.67%和35.30%;高垄覆膜种植方式下,膜上沟灌对沟下土壤盐分淋洗明显,但是在行间非覆膜区盐分强烈聚集;咸水灌溉导致根区土壤pH值升高,碱化度增大,绿洲土壤存在着明显的碱化趋势。

关键词: 咸水灌溉, 土壤盐渍化, 地下水深埋区, 民勤绿洲

Abstract: Massive exploitation of underground water in Minqing oasis in recent decades caused a sharp decline in groundwater level, and underground salt water is still being mined for agricultural irrigation. The present study investigates the effects of salt water irrigation on soil salinity in the deep groundwater zone by using the field experiment. The salt from irrigation water is the main source of salt accumulated in soil surface of areas where groundwater table is very deep and saline water is used for agricultural irrigation. During the process of saline water irrigation, soil salinity of the root zone increased rapidly after previous fresh water leaching process. High salt concentration of the irrigation water leads to a significant increase of soil salinity in the soil. The rate of salt accumulation were 22.67% and 35.30% under 2 g·L-1 and 5 g·L-1 saline water irrigation respectively. Referring to sweet melon planted with high ridge and film mulching, the soil salt is leached significantly under film-furrow irrigation. However, due to the field partially covered by film mulching, uncovered soil encounters a strong evaporation which results in salt accumulation. Saline water irrigation increases pH value and enhances soil Exchangeable Sodium Percentage (ESP), especially when the salinity of irrigation water is 5 g·L-1. The ESP value is 5.7 in plough layer and soil shows slight alkalization when 5 g·L-1 salt water is used.

Key words: saline water irrigation, soil salinization, deep groundwater area, Minqin oasis

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