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首页> 外文期刊>International Journal of Tropical Agriculture >Study of In-Situ Wetting Pattern of Drip Irrigation System under Different Emitter's Discharge and Different Soil
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Study of In-Situ Wetting Pattern of Drip Irrigation System under Different Emitter's Discharge and Different Soil

机译:不同发射器排放和不同土壤下滴灌系统的原位润湿模式研究

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摘要

The wetting pattern is an important factor to consider for designing and managing a drip irrigation system. The dimensions of the wetting pattern are imperative in selecting the right spacing between emitters and the suitable distance between laterals. The field experiments with surface drip irrigation involving three discharge rates (2 lph, 4 lph and 8 lph). The experiment carried in on two different soil sandy clay loam and clay loam after determining various physical property of soil like moisturecontent, bulk density, field capacity. The experiments were conducted by drip emitters of different discharge rates on separate laterals on different beds for one hour. The horizontal spreading and vertical depth of infiltration of the water into soil was measured. The experiment concluded that when discharge rate increased from 2 lph to 4 lph then maximum horizontal distance was found to be increased by 44.4% and from 2 lph to 8 lph maximum horizontal spreading was found to be increased by 111.1%. While when discharge rate increased from 2 lph to 4 lph then maximum vertical distance was found to be decreased by 4.76% and from 2 lph to 8 lph maximum vertical distances was found to be decreased by 14.28%. Therefore, more is the discharge rate less is the vertical movement and vice-versa. It was also observed that the lateral movement of water is more for clay loam soil than the sandy clay loam soil while the vertical distance is greatest for sandy clay loam than the clay loam. Thus, the more is the sandy nature of the soil more is the vertical movement of water and comparatively less in lateral movement.
机译:润湿模式是考虑设计和管理滴灌系统的重要因素。润湿图案的尺寸在选择发射器之间的右间距和侧向之间的合适距离方面是势在必行的。表面滴灌的现场实验涉及三个放电速率(2磅,4磅和8磅)。在确定湿润的土壤的各种物质之后,实验在两种不同的土壤砂土壤土和粘土壤土上进行的实验。通过不同放电速率的DRIP发射器在不同床上的单独横向上进行实验1小时。测量水渗透到土壤中的水平扩展和垂直深度。该实验得出结论,当放电率从2LPH增加到4LPH时,发现最大水平距离增加44.4%,从2LPH到8LPH,发现最大水平展示增加111.1%。虽然当放电速率从2Lph增加到4lph时,发现最大垂直距离被发现减少4.76%,并且在2Lph至8Lph的最大垂直距离被发现减少14.28%。因此,更少的放电率较少是垂直运动,反之亦然。还观察到,水的横向运动比粘土壤土土壤更多,而垂直距离比粘土壤土最大,垂直距离最大。因此,土壤的沙质性质越多是水的垂直运动,并且在横向运动中相对较少。

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