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Spatio Temporal Soil Moisture Dynamics and Runoff under Different Soil Cover Conditions in a Semiarid Representative Basin in Brazil

机译:巴西半干旱代表性盆地不同土壤覆盖条件下的时空土壤水分动态和径流

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Abstract. Hydrological studies in small basins are essential forinvestigating the role of distinct processes on water resources conservationand to assess the impact of the natural ecosystems on improving watersecurity especially in semiarid environments. In Brazil, the cooperativehydrological Network REHISA (“REde de HIdrologia do Semiárido”)comprises hydrologists from several universities of Brazil, focusing onfield measurements, monitoring and modeling activities in well instrumentedexperimental rural catchments located at different regions and biomes inSemiarid environment. Water scarcity is a common aspect among thecatchments, as well as risks of soil and water degradation. The objective ofthis work is to present assessments of near surface soil moisturespatial-temporal distribution, and to evaluate the impact of soilconservation techniques in reducing runoff, using small-scale experimentalplots in a representative catchment of the Pernambuco State, Brazil. Thestudy catchment is located in Alto Ipanema River Basin (AIRB) (with an areaof 150km ~(2) ), which is located at the semiarid region of the S?oFrancisco River (area of 641000km ~(2) ). Soil and water monitoring wasperformed in experimental plots with different soil cover conditions (Baresoil plots; Plots with natural cover – Caatinga Biome vegetation; Plots withcactus Palma barriers; and Plots with mulch cover – Dry grass mulch at 4tha ~(?1) ), where probes were installed for high resolution soil moistureassessment. In addition, regular soil moisture monitoring campaigns wereconducted at 7 different locations, using a capacitance probe, with arborealand shrub Caatinga vegetation, pasture and bare soil, predominantlyBrachiaria decumbens. Mulch cover runs close to the Caatinga cover, butstill with higher runoff generation, and presenting lower soil moisturetemporal mean values. Caatinga was highly effective in terms of soil andwater conservation at the small basin scale for both the dry and the wetseason, resulting in a positive nexus between vegetation and wateravailability at the region.
机译:抽象。小盆地的水文研究对于调查不同过程在水资源保护中的作用以及评估自然生态系统对改善水安全(特别是在半干旱环境中)的影响至关重要。在巴西,合作水文网络REHISA(“塞德里亚德海德罗伊德海德罗德”)由来自巴西几所大学的水文学家组成,致力于在塞米利德环境中不同地区和生物群落中的仪器良好的农村集水区进行野外测量,监测和建模活动。缺水是流域中的一个普遍问题,也是水土流失的风险。这项工作的目的是在巴西伯南布哥州的一个有代表性的流域使用小规模的试验场,对近地表土壤水分时空分布进行评估,并评估土壤保护技术对减少径流的影响。研究集水区位于Alto Ipanema流域(AIRB)(面积150 km〜(2)),位于S?oFrancisco河的半干旱地区(面积641000 km〜(2))。在具有不同土壤覆盖条件的试验区中进行水土监测(裸露土壤区;具有自然覆盖区的地块– Caatinga Biome植被;具有仙人掌帕尔马屏障的地块;以及具有覆盖物的地块– 4tha〜(?1)处的干草覆盖物),其中安装了用于高分辨率土壤湿度评估的探头。此外,使用电容探针在7个不同的地点进行了常规的土壤湿度监测活动,其中包括树木灌木灌木Caatinga植被,牧场和裸露的土壤,主要为Brachiaria decumbens。覆盖覆盖层靠近Caatinga覆盖层,但仍具有较高的径流生成量,并呈现较低的土壤湿度时间平均值。在干旱和湿季的小流域尺度上,Caatinga在水土保持方面非常有效,从而导致该地区的植被和水利用度之间呈正相关关系。

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