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Sprinkler Irrigation Effects on Infiltration and Near-Surface Unsaturated Hydraulic Conductivity

机译:喷灌对入渗和近地表非饱和水导率的影响

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Sprinkler irrigation alters soil hydraulic properties both at and below the soil surface, yet its effects are not well characterized. We evaluated the effects of sprinkler irrigation on infiltration and near-surface hydraulic conductivity (K) measured under tension in a poorly structured, recently roller-harrowed Portneuf silt loam (Durinodic Xeric Haplocalcid). The experimental design was a randomized complete block with two treatments (pre- and post-irrigation) and four replications. We used two half-circle spray heads to apply 127 mm of water at 70 mm h -1 in one irrigation to duplicate 1 × 2 m plots. Unconfined (three-dimensional) infiltration rates at steady-state were measured at potentials of -55, -35, and -15 mm of water before and about 10 days after irrigation. Irrigation increased surface bulk density (0 to 34 mm) by 18% and increased the saturation ratio by 35%. At -15 mm, the unconfined infiltration rate was 53 mm h -1 before, but 16 mm h -1 after irrigation. At -35 and -55 mm, irrigation decreased infiltration by 68%. Irrigation also decreased infiltration nearly 5-fold through pores with diameters ranging from 0.55 to 0.86 mm. At each measured potential, irrigation tended to decrease hydraulic conductivity by 48%, on average. Sprinkler droplet impact consolidated unprotected soil and greatly reduced tension infiltration. Our findings provide useful input data regarding this and similar soils for models requiring hydraulic properties. In addition, our results provide valuable insight for managing infiltration and avoiding runoff during a growing season when surface properties change as recently tilled soils are sprinkler irrigated
机译:喷灌改变了土壤表面和土壤表面以下的土壤水力特性,但其效果尚未很好地表征。我们评估了喷头灌溉对结构不良,近期滚轮耙式泥沙壤土(Durinodic Xeric Haplocalcid)中在张力作用下测得的入渗和近地表水导水率(K)的影响。实验设计是一个随机完整块,有两种处理方法(灌前和灌后)和四次重复。我们使用两个半圆喷头在一次灌溉中以70 mm h -1 的水量施用127 mm的水,重复1×2 m的样地。在灌溉前和灌溉后约10天,在势能为-55,-35和-15 mm的水上测量稳态下的无限制(三维)渗透率。灌溉使表面堆积密度(0至34 mm)增加了18%,饱和比增加了35%。在-15 mm时,灌溉前的无限制渗透率是53 mm h -1 ,而在灌溉后是16 mm h -1 。在-35和-55 mm处,灌溉减少了68%的入渗。灌溉也使直径从0.55到0.86 mm的孔的渗透减少了近5倍。在每个测得的电位下,灌溉往往会使水力传导率平均降低48%。洒水液滴撞击固结了未保护的土壤,并大大减少了张力的渗透。我们的发现为需要水力特性的模型提供了有关此土壤和类似土壤的有用输入数据。此外,我们的结果为在生长季节(当最近灌溉的土壤洒水灌溉时表面特性发生变化)时的入渗管理和避免径流提供了宝贵的见解。

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