{"title":"基于可持续水资源管理的下河川流域水量与水量平衡模型","authors":"","doi":"10.33922/j.ujet_v5i1_8","DOIUrl":null,"url":null,"abstract":"The use of hydrologic models to predict the relevant processes occurring within a catchment will serve as a veritable tool for water managers and planners for a sustainable management of water resources especially in the absence of quality and reliable data. The Soil and Water Assessment Tool (SWAT), a physically based semi-distributed hydrological model interfaced with MapWindows GIS software was used to simulate the different components of water balance and estimation of water yield of the Lower Benue River Basin in Nigeria. Climate data of three weather stations; Lokoja, Makurdi and Ibi located close to the catchment were used to simulate the stream flow of the catchment. The model was calibrated and validated using measured streamflow at Makurdi gauging station and subsequently used to predict the water balance and water yield of the catchment. Model evaluation gave R2 value of 0.79 and RSR of 0.45 for the calibration period, while R2 of 0.74 and RSR of 0.51 were recorded for validation of the model indicating a reasonable agreement between the measured and simulated flows. The prediction of water balance showed that more than a third of the water loss from the catchment is due to evapotranspiration. Sub-surface flow accounted for over 50% of the water balance simulation, while stream flow yielded only 10% as a result of the shallow slopes of the study area. The maximum water yield recorded in the study area occurred in 2009 with a value of 162,862mm representing 8.74% for the 20 year period while the lowest water yield for the period occurred in 2015 with 45,458mm representing 2% of the total water yield for the period. Overall, results show a progressive reduction in streamflow and precipitation since 2012 in the catchment and 2015 recorded the least values for the period of study. These findings show that SWAT is a viable tool for predicting future scenarios for water resources management in the catchment.","PeriodicalId":151670,"journal":{"name":"UMUDIKE JOURNAL OF ENGINEERING AND TECHNOLOGY","volume":"1 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"MODELING WATER YIELD AND WATER BALANCE OF LOWER BENUE RIVER BASIN FOR SUSTAINABLE WATER MANAGEMENT\",\"authors\":\"\",\"doi\":\"10.33922/j.ujet_v5i1_8\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The use of hydrologic models to predict the relevant processes occurring within a catchment will serve as a veritable tool for water managers and planners for a sustainable management of water resources especially in the absence of quality and reliable data. The Soil and Water Assessment Tool (SWAT), a physically based semi-distributed hydrological model interfaced with MapWindows GIS software was used to simulate the different components of water balance and estimation of water yield of the Lower Benue River Basin in Nigeria. Climate data of three weather stations; Lokoja, Makurdi and Ibi located close to the catchment were used to simulate the stream flow of the catchment. The model was calibrated and validated using measured streamflow at Makurdi gauging station and subsequently used to predict the water balance and water yield of the catchment. Model evaluation gave R2 value of 0.79 and RSR of 0.45 for the calibration period, while R2 of 0.74 and RSR of 0.51 were recorded for validation of the model indicating a reasonable agreement between the measured and simulated flows. The prediction of water balance showed that more than a third of the water loss from the catchment is due to evapotranspiration. Sub-surface flow accounted for over 50% of the water balance simulation, while stream flow yielded only 10% as a result of the shallow slopes of the study area. The maximum water yield recorded in the study area occurred in 2009 with a value of 162,862mm representing 8.74% for the 20 year period while the lowest water yield for the period occurred in 2015 with 45,458mm representing 2% of the total water yield for the period. Overall, results show a progressive reduction in streamflow and precipitation since 2012 in the catchment and 2015 recorded the least values for the period of study. 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引用次数: 0
摘要
利用水文模型预测集水区内发生的有关过程将成为水管理人员和规划人员可持续管理水资源的真正工具,特别是在缺乏高质量和可靠数据的情况下。利用基于物理的半分布式水文模型SWAT (Soil and Water Assessment Tool, SWAT)与MapWindows GIS软件相结合,模拟了尼日利亚贝努埃河下游流域水平衡的不同组成部分,并对水量进行了估算。3个气象站气候资料;利用靠近集水区的Lokoja、Makurdi和Ibi来模拟集水区的水流。该模型使用马库尔迪测量站测量的流量进行了校准和验证,随后用于预测集水区的水平衡和水量。模型评估的R2值为0.79,RSR为0.45,而模型验证记录的R2值为0.74,RSR为0.51,表明实测流量和模拟流量之间的合理一致。对水平衡的预测表明,汇水区超过三分之一的水分损失是由于蒸发蒸腾。由于研究区坡度较浅,地下流量占水量平衡模拟的50%以上,而河流流量仅占10%。研究区记录的最大出水量发生在2009年,为162,862毫米,占20年期间的8.74%,而该期间的最低出水量发生在2015年,为45,458毫米,占该期间总出水量的2%。总体而言,研究结果表明,自2012年以来,该流域的流量和降水逐渐减少,2015年的数值最小。这些发现表明SWAT是预测流域水资源管理未来情景的可行工具。
MODELING WATER YIELD AND WATER BALANCE OF LOWER BENUE RIVER BASIN FOR SUSTAINABLE WATER MANAGEMENT
The use of hydrologic models to predict the relevant processes occurring within a catchment will serve as a veritable tool for water managers and planners for a sustainable management of water resources especially in the absence of quality and reliable data. The Soil and Water Assessment Tool (SWAT), a physically based semi-distributed hydrological model interfaced with MapWindows GIS software was used to simulate the different components of water balance and estimation of water yield of the Lower Benue River Basin in Nigeria. Climate data of three weather stations; Lokoja, Makurdi and Ibi located close to the catchment were used to simulate the stream flow of the catchment. The model was calibrated and validated using measured streamflow at Makurdi gauging station and subsequently used to predict the water balance and water yield of the catchment. Model evaluation gave R2 value of 0.79 and RSR of 0.45 for the calibration period, while R2 of 0.74 and RSR of 0.51 were recorded for validation of the model indicating a reasonable agreement between the measured and simulated flows. The prediction of water balance showed that more than a third of the water loss from the catchment is due to evapotranspiration. Sub-surface flow accounted for over 50% of the water balance simulation, while stream flow yielded only 10% as a result of the shallow slopes of the study area. The maximum water yield recorded in the study area occurred in 2009 with a value of 162,862mm representing 8.74% for the 20 year period while the lowest water yield for the period occurred in 2015 with 45,458mm representing 2% of the total water yield for the period. Overall, results show a progressive reduction in streamflow and precipitation since 2012 in the catchment and 2015 recorded the least values for the period of study. These findings show that SWAT is a viable tool for predicting future scenarios for water resources management in the catchment.