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Persistency of flow patterns in a water repellent sandy soil - Conclusions of TDR readings and a time-delayed double tracer experiment

机译:疏水性沙质土壤中流态的持久性-TDR读数的结论和延时双示踪剂实验

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On a former waste water disposal field with water repellent sandy soil under grass vegetation we analyzed the persistency of flow patterns on a 150 m x 25 m plot by (i) continuous TDR-measurements on a 2 m x 1 m transect combined with seasonal soil moisture sampling campaigns, and (ii) a time-delayed double tracer experiment on a second 3 m x 1 m transect. Here, we applied bromide under wettable soil conditions in spring and chloride under water repellent soil conditions in autumn. At the end of the tracer experiment, after a travel time of 328 days for Br and 87 days for Cl, respectively, the transect was excavated and sampled in high spatial resolution. Tracer concentration, water content, water drop penetration times (WDPT), and soil organic matter content (SOM) of each sample were analyzed in order to characterize flow patterns. The TDR readings were used to predict the effective cross section (ECS) of subsurface flow and flow shifts over the season. During summer, when ECS is low and consecutive precipitation events occur, flow paths - once created - persist over time. However, over longer times (from autumn to autumn), the spatial arrangements of the flow paths can change completely. The Cl distribution showed typical fingering structures with high concentrations in the less water repellent flow paths. In contrast, Br was found mostly in the dry, hydrophobic areas indicating that it was transported before the soil became water repellent. Consequently, the flow patterns generated in spring and early summer differ completely from those in autumn and winter because of water repellent structures established during the vegetative period. These structures could be identified using a critical water content (0(crit)) concept, considering both soil water content and SOM. As not all soil parts being active during to season, four flow categories could be identified: about 10% permanent (=stable flow paths), 45% periodic (i.e. water repellent in summer), 40% occasional (water repellent in summer and autumn), and 5% permanent water repellent.
机译:在草类植被下具有疏水性沙土的前废水处理场中,我们通过(i)在2 mx 1 m样带上进行连续TDR测量并结合季节性土壤水分采样,分析了150 mx 25 m地块上水流模式的持久性广告系列,以及(ii)在第二个3 mx 1 m样带上进行的延时双示踪实验。在这里,我们在春季在可湿性土壤条件下施用溴化物,在秋季在疏水性土壤条件下施用氯化物。在示踪剂实验结束时,Br的行进时间为328天,Cl的行进时间为87天,然后以高空间分辨率对断面进行了挖掘和采样。分析了每个样品的示踪剂浓度,水含量,水滴渗透时间(WDPT)和土壤有机质含量(SOM),以表征流动模式。 TDR读数用于预测地下流量的有效横截面(ECS)和整个季节的流量变化。在夏季,当ECS较低且发生连续的降雨事件时,流动路径(一旦创建)会随时间持续存在。但是,在较长的时间(从秋天到秋天)中,流路的空间布置可以完全改变。 Cl分布显示出在较少的疏水流动路径中具有高浓度的典型指状结构。相反,Br主要存在于干燥的疏水区域,这表明Br在土壤变得疏水之前就已被运输。因此,由于在营养期建立了憎水结构,因此春季和初夏产生的流型与秋季和冬季完全不同。考虑土壤含水量和SOM,可以使用临界含水量(0(临界))概念来识别这些结构。由于并非所有土壤部分在季节中都处于活动状态,因此可以确定四种流量类别:约10%的永久性(=稳定的流路),45%的周期性(即夏季的拒水),偶尔的40%(夏季和秋季的拒水) )和5%的永久防水剂。

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