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首页> 外文期刊>Journal of Hydrology >Simple equations to represent the volume-area-depth relations of shallow wetlands in small topographic depressions
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Simple equations to represent the volume-area-depth relations of shallow wetlands in small topographic depressions

机译:表示地形小洼地浅层湿地体积-面积-深度关系的简单方程式

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Small topographic depressions have important functions in hydrology and ecology because they store water in the form of shallow lakes, wetlands or ephemeral ponds. The relations between the area A, the volume V, and the depth h of water in depressions are important for evaluating water and dissolved-mass balances of the system. The A-h and V-h relations are usually determined from fine-resolution elevation maps based on detailed survey data. Simple equations are presented in this paper, which can be used to: (1) interpolate A-h and V-h data points obtained by a detailed survey; (2) approximate unknown A-h and V-h relations of a depression from a minimal set of field data without a time-consuming elevation survey; and (3) serve as a geometric model of depressions in simulation studies. The equations are simple power functions having two constants. The first constant s is related to the size of the depression, and the second constant p is related to the geometry of the depression. The power functions adequately represent A-h and V-h relations of all 27 wetlands and ephemeral ponds examined in this paper, which are situated in the northern prairie region of North America. Assuming that the power functions are applicable for other similar topographic depressions, an observer only needs to measure A and h twice to determine the two constants in the equation. The equations will be useful in field studies requiring approximate A-h and V-h relations and in theoretical and modeling studies. (C) 2000 Elsevier Science B.V. All rights reserved. [References: 17]
机译:小型地形洼地在水文学和生态学中具有重要作用,因为它们以浅湖,湿地或临时池塘的形式储存水。凹陷中的面积A,体积V和水深h之间的关系对于评估系统中的水和溶解质量平衡非常重要。 A-h和V-h关系通常是根据详细的勘测数据从高分辨率的高程图确定的。本文提出了简单的方程式,可用于:(1)对通过详细调查获得的A-h和V-h数据点进行插值; (2)在不进行费时的高程测量的情况下,从最小的一组现场数据中近似估计出一个凹陷的未知的A-h和V-h关系; (3)在模拟研究中作为凹陷的几何模型。这些方程是具有两个常数的简单幂函数。第一常数s与凹陷的大小有关,第二常数p与凹陷的几何形状有关。幂函数足以表示本文研究的所有27个位于北美北部大草原地区的湿地和临时池的A-h和V-h关系。假设幂函数可用于其他类似的地形凹陷,则观察者只需测量两次A和h即可确定方程中的两个常数。这些方程将在需要近似A-h和V-h关系的野外研究以及理论和模型研究中很有用。 (C)2000 Elsevier Science B.V.保留所有权利。 [参考:17]

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