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Complexities of Flood Mapping in a Sinkhole Area

机译:污水区洪水映射的复杂性

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Many of the flooding problems in Bowling Green, Kentucky are associated with sinkholes. Many existing sinkhole flood zones are approximate and do not conform to surface topography. An effort to update flood maps and calculate flood elevations for four large sinkholes was begun to assist the City of Bowling Green. Problems with the mapping were encountered for two of the sinkholes that lie along Nashville Road. For these two sinkholes, flood elevations based on topographically delineated watersheds were far below observed elevations. Sources of flood elevations higher than predicted could arise from two sources, 1) flooding and spillover from uphill sinkholes, and 2) back flooding from the subterranean Lost River. This project addressed the first of these two causes. The larger of the two sinkholes, Nashville Road North had direct runoff from 11 hectares, but when spillover was considered, the drainage area grew to more than 520 hectares. GIS was used to determine volumes of sinkholes at the elevation of spill points. It was found that the volume held had little correlation with the catchment draining directly to the sinkhole. The EPA Storm Water Management Model (SWMM 5.0) was used to calculate runoff and hydraulics for this complex of sinkholes. To calibrate the model with a large storm that occurred in April 1998, it was necessary to increase the losses from the runoff to a level significantly higher than recommended. This is justifiable for Bowling Green because of numerous stormwater injection wells that receive part of the runoff.
机译:许多鲍灵格林的水浸问题,肯塔基州与落水洞有关。许多现有的天坑洪泛区是近似值,不符合表面形貌。以更新洪水地图和四个大落水洞计算洪水高程的努力是开始协助市鲍灵格林的。遇到了两个沿纳什维尔路躺在落水洞与映射的问题。对于这两个天坑的基础上,划定地形流域洪水高程远远低于海拔观察。洪水隆起的源头高于预测可以从两个来源,1)水浸和从上坡落水洞溢出,和2产生)从地下迷失河回泛滥。该项目解决了第一,这两个原因。两个落水洞较大,纳什维尔北路有直接径流量的11万公顷,但是当外溢被认为是,流域面积发展到520余公顷。 GIS用在溢油点的高程确定落水洞卷。结果发现,持有量曾与集水直接排放到污水池关联度不大。所述EPA雨水管理模型(SWMM 5.0)用于计算径流和液压此复杂落水洞。要校准与发生在1998年4月大的风暴模型,有必要增加从径流损失显著高于建议的水平。这是因为收到径流的一部分众多雨水注入井正当的鲍灵格林。

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