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黃土高原重力式地下滴灌水分運動模型與分區(qū)參數(shù)研究
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    摘要:

    建立了重力式地下滴灌條件下的土壤水分運動模型,分析地下滴灌土壤水分入滲規(guī)律。對黃土高原不同分區(qū)的4種典型土壤、不同灌水技術(shù)要素條件下的地下滴灌土壤濕潤體形態(tài)、滴孔處出流量及土壤土水勢進行數(shù)值模擬得出: 榆林緊砂土土壤導(dǎo)水率較大,向下滲漏過多,不適宜地下滴灌;安塞砂壤土、洛川中壤土、武功重壤土在相同灌水量下,供水壓力與滴孔孔徑對地下滴灌濕潤體形態(tài)影響微弱,但對滴孔出流量有較大影響,因此在地下滴灌工程設(shè)計時,只需根據(jù)田塊長度和滲水管損失設(shè)計孔徑和供水壓力,并采用較小供水壓力,降低供水水池高度,減小工程量;對武功重壤土,孔徑和供水壓力較大時地下滴灌滴孔處土壤易飽和板結(jié),宜采用較小的孔徑和供水壓力。

    Abstract:

    Based on unsaturated soil water movement theory, a three-dimensional mathematical model was developed to describe water flow movement under gravity subsurface drip irrigation (SDI). The effects of water supply pressure and dripper aperture on the soil wetting pattern, emitter charge and soil water potential with four typical soils from different subarea in Loess Plateau under gravity SDI were simulated and analyzed. The results indicate that the model can be used to analyze gravity SDI soil water infiltration characteristics and wetting pattern accurately. Gravity SDI is not suitable for Yulin area because of great deep leakage. Under the same irrigation quantity, pressure head and emitter diameter have slight effects on the wetting pattern but obvious effects on emitter effluent discharge in Ansai Sandy Loam, Luochuan Medium Loam and Wugong Heavy Loam. So the emitter aperture and water pressure can be decided only based on the field length and pipe infiltration loss for gravity SDI design. Meanwhile, it is necessary to adopt lower water pressure to reduce water supply pool height and the gravity SDI engineering investment. Especially for Wugong Heavy Loam, larger diameter dripper and higher water pressure will make the soil near drippers quick saturated and harden, therefore it should adopt the smaller diameter dripper and lower water pressure.

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康銀紅,馬孝義,李娟,王波雷.黃土高原重力式地下滴灌水分運動模型與分區(qū)參數(shù)研究[J].農(nóng)業(yè)機械學(xué)報,2008,39(3):90-95.[J]. Transactions of the Chinese Society for Agricultural Machinery,2008,39(3):90-95.

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