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Derivation of low flow frequency distributions under human activities and its implications

机译:人类活动下低流量分布的推导及其影响

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Low flow, refers to a minimum streamflow in dry seasons, is crucial to water supply, agricultural irrigation and navigation. Human activities, such as groundwater pumping, influence low flow severely. In order to derive the low flow frequency distribution functions under human activities, this study incorporates groundwater pumping and return flow as variables in the recession process. Steps are as follows: (1) the original low flow without human activities is assumed to follow a Pearson type three distribution, (2) the probability distribution of climatic dry spell periods is derived based on a base flow recession model, (3) the base flow recession model is updated under human activities, and (4) the low flow distribution under human activities is obtained based on the derived probability distribution of dry spell periods and the updated base flow recession model. Linear and nonlinear reservoir models are used to describe the base flow recession, respectively. The Wudinghe basin is chosen for the case study, with daily stream flow observations during 1958-2000. Results show that human activities change the location parameter of the low flow frequency curve for the linear reservoir model, while alter the frequency distribution function for the nonlinear one. It is indicated that alter the parameters of the low flow frequency distribution is not always feasible to tackle the changing environment. (C) 2017 Elsevier B.V. All rights reserved.
机译:低流量,是指干燥季节的最小流流,对供水,农业灌溉和导航至关重要。人类活动,如地下水泵送,严重影响低流量。为了获得人类活动下的低流量分布功能,本研究将地下水泵送和作为衰退过程中的变量返回流量。步骤如下:(1)假设没有人类活动的原始低流量遵循Pearson型三个分布,(2)气候干法术期的概率分布是基于基础流量衰退模型的推导,(3)基于人类活动更新基础流量衰退模型,(4)基于干法术期的衍生概率分布和更新的基本流量衰退模型获得人类活动下的低流量分布。线性和非线性储层模型用于分别描述基础流量衰退。选择的盆地盆地被选为案例研究,每日流动流动观察在1958 - 2000年期间。结果表明,人类活动改变了线性储库模型的低流量频率曲线的位置参数,同时改变了非线性的频率分布函数。表示改变了低流量分布的参数并不总是可行的,以解决变化的环境。 (c)2017年Elsevier B.V.保留所有权利。

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