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Natural and anthropogenic controls on the frequency of preferential flow occurrence in a wastewater spray irrigation field

机译:自然和人为控制废水喷灌场中优先流动发生频率的方法

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To quantify the frequency of preferential flow (PF) occurrence and its controls, and to examine the interactions of soils and irrigation on water flow dynamics, soil moisture was monitored at six depths every two minutes at four sites in a wastewater spray irrigation field from 2009 to 2011. Two irrigated sites - one cropped and another forested - were compared with two corresponding non-irrigated sites. Activation of preferential flow pathways was determined from the sequences of soil moisture responses at various depths for a total of 633 water input events, including 82 irrigation events. The results showed that the overall averaged frequencies of PF at the non-irrigated sites were 24.9% at the cropped site and 24.7% at the forested site. By contrast, the averaged frequencies at the irrigated sites were 47.1% at the cropped site and 45.0% at the forested site. The temporal stability of PF frequency was evaluated, showing that the overall frequency of PF stabilized after 70 events at non-irrigated sites, while the irrigated sites took as many as 105 events (24 of which were irrigations). Associations between 20 possible controls related to water input, moisture response, and season were quantified using the Student's t-test between each parameter and PF detection. The most influential factors were water inputs, especially the total input and peak input intensity. Antecedent soil moisture and response slope (maximum 2-min increase in moisture content during the response) were also significant in some but not all cases. Soil horizonation influenced soil water storage and dynamics by restricting flow and causing perched water tables. Irrigated sites experienced saturated conditions for as much as 38% of the monitoring time at some depths, compared to a maximum of 3% at non-irrigated sites. Preferential flow was not only more likely to occur during irrigation events, but also during natural events at the irrigated sites, suggesting that the irrigated soils have physically adapted to accommodate large volumes of water, after decades of spray irrigation. The results of this study have implications for understanding hydrology and contaminant fate in anthropogenically-altered landscapes as well as implementing sustainable management practices. (C) 2016 Elsevier B.V. All rights reserved.
机译:为了量化优先流(PF)的发生频率及其控制,并检查土壤和灌溉对水流动力学的相互作用,从2009年开始在废水喷灌场的四个地点每两分钟对六个深度的土壤湿度进行监测。到2011年。将两个灌溉地点(一个种植了另一个森林)与两个相应的非灌溉地点进行了比较。从不同深度的土壤水分响应序列确定了优先流动途径的激活,总共进行了633次水输入事件,包括82次灌溉事件。结果表明,非灌溉点的PF总平均频率在种植点为24.9%,在森林点为24.7%。相比之下,灌溉地点的平均频率在种植地点为47.1%,在森林地点为45.0%。评估了PF频率的时间稳定性,表明在非灌溉地点发生70次事件后PF的整体频率稳定了,而灌溉地点发生了105次事件(其中24次为灌溉事件)。使用学生t检验在每个参数和PF检测之间对与水输入,湿度响应和季节有关的20种可能控制之间的关联进行了量化。影响最大的因素是水的输入,尤其是总输入和峰值输入强度。在某些情况下,但并非所有情况下,土壤前期的水分和响应斜率(响应过程中水分最多增加2分钟)也很重要。土壤层位通过限制水流并导致地下水位过高来影响土壤水的储存和动力学。在某些深度,灌溉地点经历了长达38%的监视时间的饱和条件,而在非灌溉地点则达到了3%的最大值。优先流量不仅在灌溉事件期间更可能发生,而且在灌溉地点自然事件期间更可能发生,这表明经过数十年的喷灌,灌溉土壤在物理上已经适应了容纳大量水的需求。这项研究的结果对于理解人为改变景观中的水文学和污染物命运以及实施可持续管理实践具有重要意义。 (C)2016 Elsevier B.V.保留所有权利。

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