wetting front

  • wetting front
  • 释义

    湿润锋;湿润界面

纠错 数据更新时间:2026-04-19 13:00:33
1、

The movement of soil water achieved the temporary balance in 24 h after stopping irrigation. Subsequently the change of the soil water content became very small, and the wetting front was kept nearly un-expanded.

灌溉结束24h后土壤水分运动达到暂时的平衡,此后土壤含水量变化很小,土壤湿润锋几乎不再扩展。

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2、

Influence Factors on Soil Wetting Front under Point Drip Irrigation

滴灌点源入渗湿润锋影响因子的研究

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3、

Wetting front moved with time and the curve of water ration gradually changed to be gentle;

湿润锋随灌施时间延长不断迁移,含水率分布曲线由比较陡直逐渐变为相对平缓;

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4、

The emitter discharge rate has remarkable effects on the ratio between horizontal and vertical wetting front.

滴头流量对湿润体水平和垂向湿润距离的比值有显著的影响,滴头流量越大该值也越大,并且该值随着入渗时间的增加而逐渐变小。

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5、

Results showed that with temperature raising, wetting front distance and cumulative infiltration volume increased.

并建立考虑温度影响的湿润锋运移模型和累积入渗量模型,经实测资料进行验证,结果良好。

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6、

Wetting front characteristics under film single hole point source infiltration of fertilizer solution

膜孔单点源肥液入渗湿润体特性试验研究

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