地表滴灌土壤湿润体特征值的经验解
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* 国家高技术研究发展计划项目(2002AA2Z4031);烟台师范学院中青年自然科学基金项目(000444)资助


AN EMPIRICAL SOLUTION OF CHARACTERISTIC VALUES OF WETTED SOLUM UNDER SURFACE DRIP IRRIGATION
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    摘要:

    粘壤土地表点源入渗试验研究表明,其土壤湿润体形状近似为半椭球体,水平和竖直方向的最大入渗距离与入渗时间存在极显著的幂函数关系.湿润体体积和灌水量之间存在显著的线性关系,在2~4Lh-1的滴头流量范围内,灌水量相同时不同流量滴头对应的湿润体体积的最大差异保持在5%以内.地表点源入渗过程中,土壤湿润体内平均体积含水率的增量和入渗时间、滴头流量无关保持为一定值,在本研究条件下为0326.综合以上结果,提出了预测地表滴灌入渗土壤湿润体特征值的经验解模型.

    Abstract:

    Experiments on infiltration from a surface point source were conducted in the laboratory.The results showed that the wetted solum appeared in the shape of a semielliptic cone and that remarkable power function relat ions were observed between horizontal and vertical wetting fronts and the infiltration time and a significant linear relationship the volume of wetted solum and the volume of water applied;When the volume of water applied was kept the same, the volume of wetted solum did not vary much with the dripping rate, which was kept in range of 2~4 L h-1;in the process of point source infiltrat ion, the increment in soil water content had nothing to do with duration of the infiltration and the dripping rate, but appeared to a constant value being 0.326 for clay loam soil in this experiment.Based on the above-said findings, a model for empirical solution of characteristic values of wetted solum under surface drip irrigation was presented to predict horizontal and vertical wetting front and volume of wetted soil.

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张振华,蔡焕杰,杨润亚.地表滴灌土壤湿润体特征值的经验解[J].土壤学报,2004,41(6):870-875. DOI:10.11766/trxb200309010605 Zhang Zhenhua, Cai Huanjie, Yang Runya. AN EMPIRICAL SOLUTION OF CHARACTERISTIC VALUES OF WETTED SOLUM UNDER SURFACE DRIP IRRIGATION[J]. Acta Pedologica Sinica,2004,41(6):870-875.

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  • 收稿日期:2003-09-01
  • 最后修改日期:2004-06-07
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  • 在线发布日期: 2013-02-25
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