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Erodibility and hydrology of arid burned soils: Soil type and revegetation effects

机译:干旱土壤的侵蚀性和水文学:土壤类型和植被恢复效应

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A set of experiments with a rainfall simulator was performed in the field to evaluate the efficiency of parallel contour seeding as a post-fire restoration strategy in the arid central Ebro Valley (NE Spain). Rainfall simulations were conducted in spring, after seeded plant development, on calcareous and gypsiferous soils, with the same experimental design (two-soil treatments-seeded and nonseeded-per two soil types and per nine replicates). The parallel contour seeding treatment increases soil cover and soil surface roughness, which significantly ameliorates the hydrological and erosional response of both calcareous and gypsiferous burned soils. Seeding decreased soil loss, both in calcareous (23- fold) and gypsiferous soils (4- fold). In addition, it decreased the sediment concentration of runoff for calcareous (6- fold) and gypsiferous soils (2- fold) and the runoff coefficient for calcareous (3.5- fold) and gypsiferous soils (1.5- fold). On the other hand, seeding increased the steady state infiltration rate (3- fold), as well as surface soil moisture (1.2- fold) and wetting front depth (2- fold), with a similar order of magnitude for both soils. Time to runoff and runoff quality (electrical conductivity [EC] and pH) were not affected by seeding. Gypsiferous soils had a higher soil loss, runoff coefficient, and EC flow and a lower time to runoff, steady state infiltration rate, and wetting front depth than calcareous soils. Some of these differences were directly related to differences in soil gypsum and carbonate content (i. e., EC and pH of water runoff) and others are related to the proportion of surface soil protection, an indirect effect of soil characteristics. The results suggest that parallel contour seeding is an effective restoration measure with a short-term response that allows conservation of water and soil on recently burned arid lands, especially in situations of high erosion risk as occurs with soils with low plant cover.
机译:在野外进行了一系列降雨模拟器实验,以评估平行轮廓播种作为干旱中部埃布罗河谷(西班牙东北部)火灾后恢复策略的效率。在播种植物后,在钙质和石膏状土壤上,在春季进行了降雨模拟,并采用了相同的实验设计(每两种土壤类型分别播种和不播种两种土壤,每九种重复一次)。平行等高线播种处理可增加土壤覆盖率和土壤表面粗糙度,从而显着改善石灰性和石膏状燃烧土壤的水文和侵蚀响应。在石灰性土壤(23倍)和石膏状土壤(4倍)中,播种减少了土壤流失。此外,它降低了钙质(6倍)和石膏状土壤(2倍)的径流沉积物浓度以及钙质(3.5倍)和石膏状土壤的径流系数(1.5倍)。另一方面,播种增加了稳态渗透率(3倍),表层土壤水分(1.2倍)和湿润前沿深度(2倍),两种土壤的数量级相似。种子播种不会影响径流时间和径流质量(电导率[EC]和pH)。石膏质土壤比钙质土壤具有更高的土壤流失,径流系数和EC流量,且径流时间,稳态渗透率和湿润前沿深度更短。这些差异中的一些直接与土壤石膏和碳酸盐含量(即水的EC和pH值)的差异有关,另一些与表面土壤保护的比例有关,这是土壤特性的间接影响。结果表明,平行等高线播种是一种有效的短期恢复措施,可以保护最近被烧过的干旱土地上的水和土壤,特别是在植物覆盖率低的土壤发生高侵蚀风险的情况下。

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