首页> 外文期刊>Fresenius Environmental Bulletin >DEFINITION OF FLOOD RISKY AREAS WITH CALCULATION OF STREAM WATER VELOCITY VIA USING NUMERICAL MODEL: CASE STUDY OF FILYOS RIVER, TURKEY
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DEFINITION OF FLOOD RISKY AREAS WITH CALCULATION OF STREAM WATER VELOCITY VIA USING NUMERICAL MODEL: CASE STUDY OF FILYOS RIVER, TURKEY

机译:用数值模型计算流域水速确定洪灾危险区:以土耳其菲利奥斯河为例

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The Filyos River is located geographically in the western part of the Black Sea region of Turkey, with a catchment area of about 13,300 km~2. In the region, on the Filyos River, frequently flooding resulting in high costs and loss of life occurs. In this study, the flood risky areas were determined from water velocity and slope of the river using MIKE 11 numerical model. Remote sensing system (RSS) and GIS techniques were used to display slope and velocity properties of the river. The river network plain was divided into 4 streams (Filyos, Arac, Yenice, and Devrek) which has 235 cross sections using over 5,000 data points. The simulation period was established from October 1, 1999 to May 30, 2000. The time step was set to 1 h, and the boundary conditions at downstream discharge area into the sea; defined with constant sea level. Flood events occurred mainly in the river where flow is supercritical (maximum velocity) in steep slope and, then, slope changes to mild slope or the cross section change because of the sediment accumulation. So, the slope, minimum and maximum velocities of the river were calculated to determine the flood risky areas. These results were associated and verified with floods occurred in the region. Results of the numerical model displayed the water velocities, and slope can be adequately used to evaluate the flood risky areas.
机译:Filyos河位于土耳其黑海地区的西部,集水面积约13,300 km〜2。在该地区的菲利奥斯河上,经常发生洪水,导致高昂的成本和生命损失。在这项研究中,使用MIKE 11数值模型从水流速度和河流坡度确定了洪灾危险区。遥感系统(RSS)和GIS技术用于显示河流的坡度和速度特性。河网平原分为4个流(Filyos,Arac,Yenice和Devrek),这些流具有235个横截面,使用了5,000多个数据点。模拟期为1999年10月1日至2000年5月30日。时间步长为1 h,下游向海排泄区的边界条件为1h。以恒定的海平面定义。洪水事件主要发生在陡坡上流量超临界(最大速度)的河流中,然后由于沉积物的堆积,坡度变为平缓坡度或截面变化。因此,计算了河流的坡度,最小和最大速度来确定洪水风险区域。这些结果与该地区发生的洪水有关并得到了验证。数值模型的结果显示了水的流速,坡度可以适当地用于评估洪水危险地区。

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