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垂直線源入滲土壤水分分布特性模擬
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國家科技支撐計劃資助項目(2007BAD38B03)和新疆自治區(qū)重大專項(200731136-5)


Simulation of Soil Water Distribution under Vertical Line Source Infiltration
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    摘要:

    基于非飽和土壤水動力學理論,利用Hydrus-2D軟件分析了垂直線源入滲條件下的土壤水分分布特征。通過試驗對比驗證,反推出試驗土壤的水力參數(shù)。結(jié)果表明,Hydrus-2D軟件可用于垂直線源入滲土壤水分分布特征的模擬,且精度較好。對不同灌水技術(shù)要素條件下的垂直線源入滲土壤水分分布特征進行模擬研究,結(jié)果表明,垂直線源入滲條件下,不同質(zhì)地土壤的濕潤體形狀差別不大,大小有明顯的差別:砂壤土和粘壤土的水平濕潤半徑分別是砂土的0.59和0.24,垂直濕潤深度分別是砂土的0.42和0.31;在不同線源埋深情況下,土壤濕潤體的形狀和大小差別不大,濕潤體的位置有顯著的差別,當埋深增加5cm,砂土、砂壤土、粘壤土的垂直濕潤深度分別增加6%、11.5%、16%;線源長度和直徑對土壤水分分布影響較大,其中線源長度主要影響垂直濕潤深度,線源直徑主要影響水平濕潤半徑;初始含水率高時,相同斷面處的含水率增大;在相同入滲時段內(nèi),濕潤鋒水平運移距離和垂直運移距離隨土壤初始含水率的增大而增大。

    Abstract:

    Based on the theory of unsaturated soil water dynamics, the soil water distribution under vertical line source infiltration was analyzed by the software Hydrus-2D. The model was testified by the experiments and soil hydraulic parameters were estimated. The result showed that this model could be used to simulate soil water infiltration characteristics with certain accuracy. The characteristics of water distribution under line source irrigation were simulated concerning different irrigation technique factors. The results showed that, under the condition of line source irrigation, the shape of wetting patterns under different soil textures was similar, and the scale was different: the ratio between the maximum sand loam and clay loam’s level wetting radius and sand’s were 0.59 and 0.24, the ratios of vertical humid depth were 0.42 and 0.31; on the condition of different line source depth, the shape and scale of wetting patterns were similar, and the positions had great difference, when the depth increased 5cm, the vertical humid depths of sand, sandy loam and clay loam were increasing by 6%, 11.5%, 16% separately; the length and the diameter of the line source had conspicuous influence on soil water distribution, the length had a major impact on the vertical humid depth, the diameter had a primary influence on horizontal wetting radius; when the initial water Symbol`content was high, the water content in the same cross-section increased; in the same period of irrigation time, the wetting front distance of level and vertical increased with the increasing of initial water content. 

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李淑芹,王全九.垂直線源入滲土壤水分分布特性模擬[J].農(nóng)業(yè)機械學報,2011,42(3):51-57. Li Shuqin, Li Shuqin. Simulation of Soil Water Distribution under Vertical Line Source Infiltration[J]. Transactions of the Chinese Society for Agricultural Machinery,2011,42(3):51-57.

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