无压根区地下灌溉技术试验研究

    Experiment of non-pressure subsurface drip irrigation

    • 摘要: 对局部控水灌溉——无压根区地下灌溉技术从理论上进行了分析,并给出了其边界条件下的土壤水分运动方程。通过大田试验和室内机理试验,研究分析了无压灌溉不同孔径孔口出水规律和根区局部湿润状况。试验结果表明:无压孔口出水规律与孔口孔径、地温和土壤含水率等因素有关;出水孔口孔径和初时土壤含水率对湿润锋推进速度影响较大,孔径和初始土壤含水率越大,湿润锋推进速度越快;适宜的出水孔径条件下,沿管道长度方向出水均匀,5~35 cm土壤含水率变化无明显差异。试验证明输水管埋深为20 cm时,出水孔径为3×Φ4 mm的出水量能够满足根系分布在这一深度范围内的蔬菜作物需水要求。

       

      Abstract: The experiment of non-pressure subsurface drip irrigation was conducted. The non-pressure subsurface drip irrigation, a kind of local water control irrigation. The law of outlet flow rate at different aperture diameters and the soil water status under the condition of non-pressure irrigation were studied. The results indicated that the outlet flow rate of non-pressure aperture was related to aperture diameter, soil temperature and soil water content, etc; The moving velocity of wetting front was influenced mostly by aperture diameter and initial soil water content; The larger aperture diameter and initial soil water content were, the faster moving velocity of wetting front was; The outlet flow rate was uniform under the condition of aperture diameter from 5 to 35 cm along the pipeline, and the soil water content was also not significantly changing with depth. It was proved that the outlet flow rate of 3×Φ4 mm aperture diameter at non-pressure subsurface drip irrigation could fulfill the water requirement of vegetable crop when root-age depth was 20 cm soil layer.

       

    /

    返回文章
    返回