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基于HYDRUS-3D模型的微潤灌溉土壤水分入滲模擬
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國家重點(diǎn)研發(fā)計(jì)劃項(xiàng)目(2017YFD0201500-2017YFD0201501)和國家自然科學(xué)基金項(xiàng)目(31471409)


Numerical Simulation of Soil Water Infiltration Based on HYDRUS-3D Finite Element Model under Moistube-irrigation
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    摘要:

    掌握土壤水分入滲規(guī)律對于合理制定灌溉方案、設(shè)置灌溉參數(shù)和改進(jìn)灌溉技術(shù)有重要意義。為探究微潤灌溉條件下土壤水分入滲規(guī)律,利用HYDRUS-3D有限元模型對微潤灌溉下土壤水分入滲進(jìn)行了數(shù)值模擬,討論了初始壓力水頭和土壤質(zhì)地對土壤水分入滲的影響。數(shù)值模擬結(jié)果顯示:在土壤水分入滲的垂直剖面上濕潤體以微潤管為中心呈同心圓狀向外擴(kuò)散,擴(kuò)散速率與初始壓力水頭呈正相關(guān)。模擬試驗(yàn)周期為36h,分3個(gè)時(shí)間段進(jìn)行土壤水分?jǐn)U散速率的計(jì)算,0~5h內(nèi)土壤水分平均入滲速率為1.85cm/h,6~15h內(nèi)的平均入滲速率為0.79cm/h,16~36h內(nèi)的平均水分入滲速率為0.59cm/h。土壤含水率最大值出現(xiàn)在微潤管周圍,向外圍呈減小趨勢。相同時(shí)間內(nèi)土壤濕潤峰運(yùn)移距離隨初始壓力水頭的增大而增大,微潤灌溉下水分入滲速率在3種質(zhì)地的土壤(砂壤土、壤土、粘壤土)中依次增大,并測得在壓力水頭為-180cm時(shí)整個(gè)模擬周期中3種質(zhì)地土壤的平均水分?jǐn)U散速率分別為:0.69、0.53、0.46cm/h。研究表明,土壤含水率和水分?jǐn)U散速率隨壓力水頭的增大而增大,隨土壤黏粒含量的增大而減小。

    Abstract:

    It is important to master the law of soil water infiltration for the rational development of irrigation scheme, setting irrigation parameters and improving irrigation technology. In order to explore the law of soil water infiltration under the condition of moistube-irrigation, HYDRUS-3D finite element model was used to simulate the soil water infiltration under micro-irrigation. The effects of initial pressure head and soil texture on soil water infiltration were discussed. The numerical simulation results showed that the wetting body was diffused around the micro-tube in the vertical section of soil water infiltration, and the diffusion rate was positively correlated with the initial pressure head. The average infiltration rate of soil water was 1.85cm/h in the first 5 hours, the average infiltration rate was 0.79cm/h between the 6th hour to 15th hour, and the average water infiltration rate in the period from 16th hour to 36th hour was 0.59cm/h. The maximum soil moisture content appeared around the micro fabricated tube and tended to decrease to the periphery. The migration distance of soil wetting peak increased with the increase of initial pressure head. The infiltration rate of micro-irrigation increased in three soil layers (sandy loam, loam, loam loam). When the pressure head was -180cm, the average water diffusion rates of the three soils were 0.69cm/h, 0.53cm/h and 0.46cm/h, respectively.

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冀榮華,劉秋霞,陳振海,鄭立華.基于HYDRUS-3D模型的微潤灌溉土壤水分入滲模擬[J].農(nóng)業(yè)機(jī)械學(xué)報(bào),2017,48(s1):290-295. JI Ronghua, LIU Qiuxia, CHEN Zhenhai, ZHENG Lihua. Numerical Simulation of Soil Water Infiltration Based on HYDRUS-3D Finite Element Model under Moistube-irrigation[J]. Transactions of the Chinese Society for Agricultural Machinery,2017,48(s1):290-295.

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  • 收稿日期:2017-07-10
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  • 在線發(fā)布日期: 2017-12-10
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