Estimation of water inflows to reservoirs of irrigation dams in the Guinea Savannah ecological zone of Ghana

T. Adongo, F. K. Abagale
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Abstract

The study was carried out in the northern Ghana to estimate water inflows to nine reservoirs of irrigation dams for a period of 20 years (1999–2018) using the USDA Natural Resources Conservation Service Curve Number model. The key input parameters of the model were hydrologic soil group, rainfall amount, landuse/landcover, weighted curve number, antecedent moisture condition, and potential maximum soil moisture retention. The annual rainfall within the reservoir catchments was found to vary between 617.20 and 1,382.30 mm. The estimated annual runoff depths ranged from 54.10 to 125.55 mm. A high degree of positive correlation was found between rainfall and runoff depths with a coefficient of determination (R2) ranging from 79.80 to 90.70%. Hydrologic soil groups accounted for about 67.2 and 62.5% of the variation in runoff depth and percentage runoff, respectively. The estimated annual water inflows to the reservoirs ranged from 145,206 ± 125,814 m3/y at Gambibgo to 47,074,634 ± 4,395,860 m3/y at Tono. The variation in the annual water inflows and annual storage capacity recharge among the various reservoirs was noted to be influenced by reservoir size, catchment size, rainfall, and soil characteristics in the reservoir catchments.
加纳几内亚草原生态区灌溉大坝水库的进水量估算
该研究在加纳北部进行,利用美国农业部自然资源保护局的曲线数模型估算了 20 年内(1999-2018 年)九个灌溉大坝水库的进水量。该模型的主要输入参数包括水文土壤组、降雨量、土地利用/土地覆盖率、加权曲线数、先期水分状况和潜在最大土壤水分保持率。水库集水区的年降雨量介于 617.20 毫米和 1382.30 毫米之间。估计的年径流深度在 54.10 至 125.55 毫米之间。降雨量与径流深度之间存在高度正相关,决定系数 (R2) 在 79.80 至 90.70% 之间。水文土壤组别分别约占径流深和径流百分比变化的 67.2% 和 62.5%。据估计,水库的年进水量从甘比布戈的 145,206 ± 125,814 立方米/年到托诺的 47,074,634 ± 4,395,860 立方米/年不等。据指出,各水库的年入库水量和年库容补给量的变化受水库规模、集水区面积、降雨量和水库集水区土壤特性的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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