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A conceptual model of daily water balance following partial clearing from forest to pasture

机译:从森林到牧场的部分砍伐后每日水平衡的概念模型

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A simple conceptual water balance model representing the streamflow generation processes on a daily time step following land use change is presented. The model consists of five stores: (i) Dry, Wet and Subsurface Stores for vertical and lateral water flow, (ii) a transient Stream zone Store (iii) a saturated Goundwater Store. The soil moisture balance in the top soil Dry and Wet Stores are the most important components of the model and characterize the dynamically varying saturated areas responsible for surface runoff, interflow and deep percolation. The Subsurface Store describes the unsaturated soil moisture balance, extraction of percolated water by vegetation and groundwater recharge. The Groundwater Store controls the baseflow to stream (if any) and the groundwater contribution to the stream zone saturated areas. The daily model was developed following a downward approach by analysing data from Ernies (control) and Lemon (53% cleared) catchments in Western Australia and elaborating a monthly model. The daily model performed very well in simulating daily flow generation processes for both catchments. Most of the model parameters were incorporated a priori from catchment attributes such as surface slope, soil depth, porosity, stream length and initial groundwater depth, and some were calibrated by matching the observed and predicted hydrographs. The predicted groundwater depth, and streamflow volumes across all time steps from daily to monthly to annual were in close agreement with observations for both catchments.
机译:提出了一个简单的概念性水平衡模型,该模型代表了土地利用变化后每天时间步长上的水流产生过程。该模型由五个存储组成:(i)用于垂直和横向水流的干,湿和地下存储,(ii)瞬态流区存储(iii)饱和地水存储。该模型最重要的组成部分是顶层土壤干湿存储中的土壤水分平衡,它表征了动态变化的饱和区域,这些区域负责地表径流,内流和深层渗流。地下商店描述了非饱和土壤的水分平衡,植被提取渗透水和地下水补给。地下水库控制着水流(如果有的话)和地下水对河流带饱和区的贡献。每日模型是通过向下分析方法开发的,方法是分析西澳大利亚州的Ernies(对照)和Lemon(已清除53%)流域的数据并制定月度模型。每日模型在模拟两个流域的每日流量生成过程中表现非常出色。大部分模型参数是根据集水区属性(例如地表坡度,土壤深度,孔隙度,溪流长度和初始地下水深度)预先合并的,其中一些参数是通过匹配观测到的和预测的水文图进行校准的。预测的地下水深度以及从每天到每月到每年的所有时间步长的流量与两个集水区的观测值都非常一致。

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