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Influence of drainage system maintenance on storm runoff from a reforested, waterlogged mountain catchment

机译:排水系统维护对造林,涝渍山地集水区暴雨径流的影响

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The maintenance of a drainage system in a waterlogged mountain catchment impacted by earlier harvesting operations was assessed on the basis of a hydrological analysis (hydrological balance, three linear reservoirs method). To restore pre-harvest hydrological conditions, the water-saturated localities were experimentally drained both by restoration of existing ditches and digging of additional open ditches. The rainwater retention of the soil was illustrated by two comparable storm flow events occurring before and after the draining treatment. Pedohydrological analysis revealed the important involvement of static retention in capillary pores in the rainfall-runoff process during rainstorm events. Restoration and addition of the drainage system yield more favourable generation and better proportioned distribution of storm flow discharge. There would be no danger of water depletion in the catchment during dry periods in connection with the draining treatment. In comparison with the state before drainage system maintenance, the static retention after draining treatment became greater than zero. Both the dynamic retention (detention) and static retention helped balancing storm flows in terms of flood and drought control. The successive drop of the raised water table level following drainage system maintenance resulted in changes of actual retention and subsequent runoff. The drainage procedure proved its positive influence on reforestation and the environment, as no negative impact on soil and stream hydrology was found.
机译:根据水文分析(水文平衡,三个线性水库方法)评估了受早期采伐作业影响的涝灾山区流域的排水系统维护。为了恢复收获前的水文条件,通过恢复现有的沟渠和挖掘更多的开放式沟渠,实验性地抽干了含水饱和的地方。在排水处理之前和之后发生的两个可比较的暴雨流事件说明了土壤的雨水保留。水文学研究表明,在暴雨期间降雨径流过程中,毛细孔中静态滞留的重要参与。排水系统的恢复和增加可产生更有利的发电量,并更好地分配暴雨流量。在干燥期间,与排水处理相关的集水区不会有枯竭的危险。与排水系统维护前的状态相比,排水处理后的静态保持力大于零。动态保留(保留)和静态保留都有助于在洪水和干旱控制方面平衡风暴潮。排水系统维护后,地下水位的连续下降导致实际滞留量和后续径流的变化。排水程序证明了其对造林和环境的积极影响,因为没有发现对土壤和溪流水文学的负面影响。

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