基于(SCS - CN)方法的Qalachwalan流域径流水文估算(2000 - 2020)

Aram Dawood Abbas, Khalel Karim Muhammed
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摘要

地表水是研究区流域气候和地形条件的反映,影响着流域内地表径流量的估算。也有可能测量盆地中流动水量并知道增加的时期,以及这一数量的水资源短缺,另一方面,利用所有领域和用途的水。Qalachwalan盆地是位于苏莱曼尼亚市北部的一个盆地,面积为876.1平方公里,其所有水源都在伊拉克库尔德斯坦地区的边界内。因此,由于近年来降雨不稳定和强降水,有必要进行一些研究,了解径流的大小和数量,并看看是否有可能从中受益,为研究区域的开发和投资。因此,采用土壤保持服务曲线数(SCS - CN)方法估算年径流深度和流量。从这项研究中,我们清楚地看到,该地区有七种用途:水体、茂密的森林、农田、草原、住宅用地、荒地、铺砌的道路。径流量最大的地区为草地,为588523320 m3,最小的地区为森林,为4442480 m3。因此,我们发现流域水量总量约为(700141140)m3。最后,我们的数据对当地政府和利益相关者未来如何处理该流域特别是不稳定降水非常重要。
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Hydrological Estimation for the Runoff of Qalachwalan Basin Using Hydrological Estimation for the Runoff of Qalachwalan Basin Using (SCS – CN) Method (2000 – 2020)
The surface water is a reflection of the climatic and topographical conditions of the basin in the study area, and affects the estimation of the amount of runoff water on the surface inside the basin. It is also possible to measure the amount of running water in the basin and know the periods of increase, and water scarcity in this quantity, on the other hand, take advantage from water for all fields and uses. Qalachwalan basin is one of the water basins located at north of the city of Sulaymaniyah with an area of (876.1) km2, and all of its water sources are within the borders of the Kurdistan Region of Iraq. Due to unsteady rain and heavy precipitation in the recent years, therefore, it was necessary to conduct some researches to know the size and amount of runoff, besides, to see if it is possible to benefit from it for the development and investment of the study areas. Accordingly, Soil Conservation Service- Curve Number (SCS – CN) Method has been used used to estimate the depth and amount of the annual runoff. From this study it became clear to us that the area has seven uses )Bodies of water, dense forests, agricultural lands, grasslands, residential lands, barren lands, paved roads. Besides, it appeared that the greatest amount of runoff, which lies in the grassland equals to (588523320) m3, and the smallest amount with (4442480) m3 lies in the forest area. So, we discover that the total amount of the basin water reached about (700141140) m3. Finally, our data are very vital for the local government and stakeholders in the future to how to deal with this water basin especially with unsteady precipitations.
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