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Method to quantitatively partition the temporal preferential flow and matrix infiltration in forest soil

机译:定量地分配林土中颞优先流量及矩阵浸润的方法

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Preferential flow is a major part of water infiltration, to partition the rainwater into the runoff generation and soil recharge in forest soil. A method is advanced in this study to measure soil matrix infiltration to verify its uniformity, before it was used to partition temporal preferential flow from the total infiltration employing two double-ring infiltrometers. A thin layer of fine sands were placed onto the nylon cloth in the inner ring and between the inner and outer rings of one double-ring infiltrometer to shelter the preferential paths and ensure that water infiltrates the soil matrix only. The other double-ring infiltrometer was directly inserted a shallow depth into soil to measure total infiltration at a nearby spot. Therefore, the difference of the total and the matrix infiltration is used to determine the preferential flow infiltration. Field experiments were conducted at five sites of a forested field in Tianshui Soil and Water Conservation Experimental Station, on the Loess Plateau, Gansu province of China. Experimental results indicated that the soil matrix infiltration processes at the five sites were roughly the same, thereby indicating that the matrix infiltration at one spot could be replaced by that of the nearby spot at the experimental site. The measured matrix infiltration can be used to partition the preferential infiltration from the total. The measured initial preferential flow infiltration rate (PIR) was 2.6-10.2 times of soil matrix infiltration rate (MIR) and the steady PIR was 2.3-4.9 times of that of the MIR. Preferential cumulative infiltration contributed 66-82% to total infiltration. These highlighted that preferential flow was a main part of forest soil infiltration at the experiment sites. This study provides a convenient method for fast determination of preferential flow infiltration in field conditions which is helpful for managing agricultural water resources and infiltration-related ecosystem service.
机译:优惠流动是水渗透的主要部分,将雨水分配到森林土壤中的径流生成和土壤补给。在该研究中提前进行方法以测量土壤基质渗透以验证其均匀性,以便从采用两个双环渗透仪的总渗透分配时间优先流量。将一层细砂岩放在内圈中的尼龙布上,一个双环渗透速度的内圈和外环之间,以遮住优先路径,并确保水仅渗透到土基质。另一个双环渗透表直接插入土壤中以测量附近斑点的全渗透。因此,使用总和和基质渗透的差异来确定优先流渗透。现场实验在天水水土和水资源实验站的五个地点进行了中国甘肃省黄土高原的天水水土保持实验站。实验结果表明,五个位点的土壤基质浸润过程大致相同,从而表明在实验部位的附近斑点中的基质浸润可能被替换。测量的基质渗透可用于分配总量的优先渗透。测得的初始优先流动渗透率(PIR)为土壤基质渗透率(miR)的2.6-10.2倍,稳定的PIR是MIR的2.3-4.9倍。优惠累积渗透促进66-82%至全渗透。这些突出显示,优惠流动是实验场所森林土壤渗透的主要部分。该研究提供了一种方便的方法,用于快速确定现场条件中优先流动渗透,这有助于管理农业水资源和渗透相关的生态系统服务。

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