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Analysis of the impact of conservation measures on stream flow regime in catchments of the Loess Plateau, China

机译:黄土高原流域保护措施对水流状况的影响分析

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Catchments in the Loess Plateau have been under the influence of human activities for centuries. In the last four decades, soil conservation measures have accelerated and intensified. These measures were designed to reduce soil erosion, improve agricultural productivity, and enhance environmental quality. It is important to evaluate the effects of these measures on hydrology in order to develop sustainable catchment management plans in the region. This study evaluated changes in stream flow data for four selected catchments in the Loess Plateau following large-scale soil conservation measures. The non-parametric Mann-Kendall test was used to identify trends in annual stream flow and the results showed significant downward trends in three of the four catchments. The Pettitt test indicated that a change point occurred in 1978 in these three catchments. Annual precipitation in all the catchments showed no significant trend during the period of record. Comparison of daily flow duration curves for two 20-year periods (1957-1978) and (1979-2003) showed significant changes in stream flow regime. Reduction in most percentile flows varied between 20 and 45%, and the reduction in low flows was greatest. Overall, the reductions in daily flow were increasing with time, with significant changes occurring in the 1990s. However, it is not clear whether these catchments have seen the full effects of the soil conservation measures, so the results of this study might underestimate the final impact of soil conservation on stream flow regime.
机译:黄土高原的集水区一直受到人类活动的影响。在过去的四十年中,水土保持措施得到了加速和加强。这些措施旨在减少水土流失,提高农业生产率并提高环境质量。重要的是评估这些措施对水文学的影响,以便制定该地区的可持续流域管理计划。这项研究评估了黄土高原四个大型集水区保护措施下的流域流量数据的变化。非参数Mann-Kendall检验用于确定年流量的趋势,结果表明四个流域中的三个流域均呈显着下降趋势。 Pettitt检验表明,这三个流域的变化点发生在1978年。在记录期间,所有流域的年降水量均未显示明显趋势。比较两个20年期间(1957-1978)和(1979-2003)的每日流量持续时间曲线,可发现流量变化规律。大多数百分比流量的减少幅度在20%至45%之间,而低流量的减少幅度最大。总体而言,日流量的减少量随着时间的推移而增加,在1990年代发生了重大变化。但是,目前尚不清楚这些流域是否已经看到了土壤保持措施的全部效果,因此本研究的结果可能低估了土壤保持对河流流态的最终影响。

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