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机构地区:[1]兰州理工大学能源与动力工程学院,甘肃兰州730050
出 处:《兰州理工大学学报》2012年第3期61-66,共6页Journal of Lanzhou University of Technology
基 金:日本日立建机株式会社资助项目;兰州理工大学博士科研启动资金项目(BS06200902)资助
摘 要:以非饱和土壤水分运动理论为基础,研究膜孔灌单孔入渗土壤水分运动的数学模型,用SWMS-3D软件对多种典型土壤的单点膜孔入渗特性进行模拟.结果表明:单点膜孔的累积入渗量变化过程符合Kostiakov模型.提出包含膜孔直径、灌溉水深的单点膜孔Kostiakov入渗模型参数计算方法,采用多种土壤单点膜孔入渗室内试验结果与已有文献资料对所建模型进行验证,结果表明,所建模型能较准确地反映单点膜孔入渗特性,可为确定合理的膜孔灌灌水技术要素组合提供理论依据.Based on the theory of water movement in non-saturated soil, the mathematical model of film- hole irrigation with single-hole infiltration was investigated and the simulation of infiltration characteristics of various typical soils was performed by using SWMS-3D software. The result showed that the variation of cumulative infiltration through single hole conformed to Kostiakov model. A computation method of pa- rameters such as the film-hole diameter and irrigation depth was presented with single-point film-hole Kos- tiakov infiltration model. The model was verified by comparing indoor test result of single-point film-hole infiltration for various typical soils to that of other researcher's experiment. It was shown that the estab- lished model was able to reflect more accurately the characteristics of single-point film-hole infiltration and water to provide a theoretical basis for determing a resonable combination of irrigational technological ele- ments with film-hole infiltration.
关 键 词:膜孔灌 单点膜孔入渗 Kostiakov模型 膜孔直径 灌溉水深 数值模拟
分 类 号:S275.9[农业科学—农业水土工程]
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