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礦化度對微潤灌土壤入滲特性的影響
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國家高技術(shù)研究發(fā)展計劃(863計劃)資助項目(2011AA100507)和高等學(xué)校學(xué)科創(chuàng)新引智計劃(111計劃)資助項目(B12007)


Effects of Mineralization Degrees on Soil Infiltration under Moistube-irrigation
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    采用室內(nèi)土箱模擬試驗的方式,研究了5種礦化度條件下微潤灌土壤水分的入滲特性。試驗結(jié)果表明:礦化度對濕潤體形狀影響小,微潤灌濕潤體橫剖面呈近似圓形;礦化度對濕潤體體積影響較大,礦化水濕潤體體積大于清水的濕潤體體積。當(dāng)?shù)V化度為3g/L時,微潤灌濕潤體濕潤鋒運移速率最大,濕潤鋒運移速率與時間呈冪函數(shù)關(guān)系。礦化水可增加微潤灌的累計入滲量,但累計入滲量與礦化度之間不是單調(diào)關(guān)系,當(dāng)?shù)V化度為3g/L時,累計入滲量達(dá)到最大,土壤平均含水率也最大。

    Abstract:

    n order to explore the impact of mineralization degrees on infiltration character of soil under moistubeirrigation, an indoor soil box simulation experiment method was used to investigate the infiltration character of soil water under five different mineralization degrees selectively. Results indicated that the degree of mineralization had small impact on the shapes of soil wetted zone, and the wetting front shape were similar to circle. Degree of mineralization had a relatively bigger influence on the volume of wetted soil.The volume of wetted soil in mineralized water was bigger than that in pure water. When the degree of mineralization was 3g/L, the wetting front (horizontal, vertical up and down) migration distance was the farthest, which had a power function relationship with time. The mineralized water could increase cumulative infiltration.However the relationship between cumulative infiltration and degree of mineralization was not linear relationship.The cumulative infiltration and average soil moisture content was the biggest when the degree of mineralization was 3g/L.The results of this study provided reference for the utilization of moistubeirrigation with mineralized water.

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牛文全,薛萬來.礦化度對微潤灌土壤入滲特性的影響[J].農(nóng)業(yè)機械學(xué)報,2014,45(4):163-172. Niu Wenquan, Xue Wanlai. Effects of Mineralization Degrees on Soil Infiltration under Moistube-irrigation[J]. Transactions of the Chinese Society for Agricultural Machinery,2014,45(4):163-172.

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  • 收稿日期:2013-05-18
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  • 在線發(fā)布日期: 2014-04-10
  • 出版日期: 2014-04-10