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Response of Stream Discharge to Storm Depth in Gidan Kwano Inland Valley 0f Minna Nigeria

机译:Gidan Kwano内陆谷0f尼日利亚明娜的水流流量对风暴深度的响应

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Stream discharge and soil characteristics were evaluated on an experimental field for ten months. Calibrated rectangular weir was used to monitor stream discharge and sieve analysis was used to characterize the soil. Findings indicated a sandy loam, clay loam, and clay soil types at 0-60cm, 60-90cm, 90-120cm profile depths respectively .A range of 6.29 - 27.75%, 1.04 ¨C 1.80g/cm3 , 15.19 ¨C 49.42% and 8.38 ¨C 34.74% were established for moisture content, bulk density, porosity and available moisture content respectively down the profile ( 1 ¨C 120cm) .Infiltration decreased from 0.2 to 0.07 cm/min and 0.25 to 0.025 cm/min at lower and upper fringe of the valley respectively. Stream discharge is highest in October with peak value of 41.897l/s and monthly average of stream discharge was 12.641l/s with only 67.7% of the storm depth translating to stream discharge. The discharge hydrograph exhibits a close nested multi-peak. These finding therefore, are viable information system for irrigation and drainage practices on land and also useful in land and water resources planning.
机译:在一个实验场上对溪流排放和土壤特性进行了十个月的评估。使用校准的矩形堰来监控水流,并使用筛分分析来表征土壤。结果表明,分别在0-60cm,60-90cm和90-120cm的剖面深度处为沙壤土,粘土壤土和粘土类型。范围为6.29-27.75%,1.04-1.80g / cm3、15.19-49.42%在剖面(1℃〜120cm)下的含水量,堆积密度,孔隙率和有效含水量分别确定为8.38℃和34.74%。在较低和较低的条件下,入渗量分别从0.2降低至0.07cm / min和0.25至0.025cm / min。山谷的上部边缘。十月河溪流量最高,达到峰值41.897l / s,月平均河溪流量为12​​.641l / s,只有风暴深度的67.7%转化为河溪流量。排放水位图显示出一个紧密嵌套的多峰。因此,这些发现是用于土地灌溉和排水实践的可行信息系统,并且在土地和水资源规划中也很有用。

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