农田荒漠过渡带包气带土壤水盐运移规律研究
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S275

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河北省青年科学基金(D2021504040);河西走廊石羊河流域水文地质调查(DD20190349)


Water and salt transport in vadose zone of transition zone between farmland and desert
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    摘要:

    为实现农田区和荒漠保护区植被协同发展,通过石羊河流域下游某试验场原位试验研究农田荒漠过渡带包气带土壤水盐运移规律。结果表明:农田荒漠过渡带上,荒漠区土壤包气带水盐运移与农田区灌溉息息相关。灌溉后,农田区土壤盐分随灌溉水进入地下水中,继而流向荒漠区,引起荒漠区表层土壤盐分大幅升高。水位调控后,灌溉对农田区表层土壤脱盐效果更好,盐分随灌溉水向下运移更深。同时,不仅农田区侧向流入荒漠区盐分减少,而且减少了浅层咸水进入荒漠区包气带土壤中的盐分,有效缓解了荒漠区表层土壤聚盐效应。

    Abstract:

    In order to realize the coordinated development of vegetation in farmland and desert areas, the law of soil water and salt transport in the aeration zone of farmland desert transition zone was studied by in-situ experiment at a test site in the lower reaches of Shiyang River Basin.The results showed that water and salt transport in soil aeration zone in desert area was affected by farmland irrigation. After irrigation, soil salt in farmland area entered groundwater with irrigation water, and then flowed to desert area. It caused the salt content of surface soil in desert area to increase greatly. After water level regulation, irrigation in farmland had a better effect on surface soil desalination, and salt moved deeper downward with irrigation water. After the regulation of the desert area, not only the salt flowing into the desert area from the farmland area was reduced,. but also the salt in the groundwater entering the aeration zone soil was reduced, which effectively alleviated the salt accumulation effect of the surface soil in the desert area.

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崔尚进,刘鹏飞,聂振龙,等. 农田荒漠过渡带包气带土壤水盐运移规律研究[J]. 科学技术与工程, 2022, 22(20): 8640-8645.
Cui Shangjin, Liu Pengfei, Nie Zhenlong, et al. Water and salt transport in vadose zone of transition zone between farmland and desert[J]. Science Technology and Engineering,2022,22(20):8640-8645.

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  • 收稿日期:2022-01-09
  • 最后修改日期:2022-04-15
  • 录用日期:2022-03-04
  • 在线发布日期: 2022-08-04
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