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Distribution and Variation of Soil Water and Salt before and after Autumn Irrigation

Author

Listed:
  • Yin Zhang

    (College of Water Conservancy and Civil Engineering, Inner Mongolia Agricultural University, Hohhot 010018, China
    Department of Water Conservancy and Civil Engineering, Hetao College, Bayannur 015000, China)

  • Qingfeng Miao

    (College of Water Conservancy and Civil Engineering, Inner Mongolia Agricultural University, Hohhot 010018, China)

  • Ruiping Li

    (College of Water Conservancy and Civil Engineering, Inner Mongolia Agricultural University, Hohhot 010018, China)

  • Minghai Sun

    (Department of Water Conservancy and Civil Engineering, Hetao College, Bayannur 015000, China)

  • Xinmin Yang

    (Urat Sub-Center, Inner Mongolia Hetao Irrigation District Water Conservancy Development Centre, Bayannur 014400, China)

  • Wei Wang

    (Urat Sub-Center, Inner Mongolia Hetao Irrigation District Water Conservancy Development Centre, Bayannur 014400, China)

  • Yongping Huang

    (Water Conservancy Research Institute of Bayannur City, Bayannur 015000, China)

  • Weiying Feng

    (School of Materials Science and Engineering, Beihang University, Beijing 100191, China)

Abstract

Autumn irrigation is a key measure for alleviating soil salinity and promoting sustainable agricultural development in the Hetao Irrigation district; however, only a part of farmland is irrigated in autumn during the non-growth period of crops, which leads to the redistribution of soil water and salt between autumn-irrigated land (AIL) and adjacent non-autumn-irrigated land (NAIL) after autumn irrigation. To explore the distribution and variation of soil water and salt in different positions of AIL and NAIL after local autumn irrigation and reveal the interaction range between AIL and NAIL, field experiments were carried out for two years in typical test areas. The results showed that compared with non-autumn irrigation, autumn irrigation improved the distribution uniformity of soil water and salt profiles in both horizontal and vertical directions; after autumn irrigation, the water content of the soil at the nearest sampling point to the boundary in the AIL increased the least, but the desalination rate was the greatest, while the water and salt contents of the soil within 45 m from the sampling points to the boundary in the NAIL both increased significantly. NAIL received the drainage of AIL and made the groundwater level after the rise in AIL fell quickly back, but unreasonable autumn irrigation caused the groundwater level of AIL to remain at a high level before freezing, exacerbating the risk of groundwater carrying salts to the surface soil during the freezing and thawing period, detrimental to the growth of crops in the next spring. The research results are of great significance to the rational use of farmland water resources and the improvement of soil salinization in cold and dry areas.

Suggested Citation

  • Yin Zhang & Qingfeng Miao & Ruiping Li & Minghai Sun & Xinmin Yang & Wei Wang & Yongping Huang & Weiying Feng, 2024. "Distribution and Variation of Soil Water and Salt before and after Autumn Irrigation," Land, MDPI, vol. 13(6), pages 1-18, May.
    • Handle: RePEc:gam:jlands:v:13:y:2024:i:6:p:773-:d:1405425
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    References listed on IDEAS

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