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首页> 外文期刊>Open Journal of Soil Science >Why Does the Repaired Len Small Levee, Alexander County, Illinois, US Continue to Breach during Major Flooding Events?
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Why Does the Repaired Len Small Levee, Alexander County, Illinois, US Continue to Breach during Major Flooding Events?

机译:为什么在重大洪水事件中,美国伊利诺伊州亚历山大县的Len堤坝修复后仍继续遭到破坏?

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摘要

One only needs to study the soil and geologic history and location of the ancient Mississippi and Ohio Rivers to understand why Len Small levee if patched will continue to fail. Much of Dogtooth Bend located in Alexander County, Illinois was originally in the ancient Ohio River valley ( Figure 1 ) alluvial sediments north and east of the confluence with the ancient Mississippi River. The ancient Ohio River valley soils underlain by alluvial sediments and have been easily eroded by the re-aligning modern Mississippi River which now travels through the bedrock controlled Thebes Gap ( Figure 2 ) and into the Ancient Ohio river valley. The primary objectives of this paper are: 1) to explain why Len Small levee, Alexander County, Illinois, US will continue to breach during major flooding events if repaired and 2) to develop a new combined raised causeway and levee system which will provide a Mississippi River floodwater bypass, be sustainable, encourage and fund a land use change, restore the degraded highway road beds, protect remaining Dogtooth Bend farmsteads and farmland that have not yet been degraded by past flooding events and provide floodwater storage during major flooding events at the confluence of the Mississippi and Ohio Rivers.
机译:只需研究古代密西西比河和俄亥俄河的土壤和地质历史以及位置,就可以理解为什么如果修补了Len Small堤坝,它将继续失败。位于伊利诺伊州亚历山大县的Dogtooth Bend大部分位于原始的俄亥俄州河谷(图1)与古代密西西比河汇合处以北和东部的冲积物。古老的俄亥俄河河谷土壤被冲积沉积物所覆盖,并且很容易被重新排列的现代密西西比河侵蚀,现在密西西比河穿过基岩控制的底比斯峡(图2)进入古老的俄亥俄河河谷。本文的主要目标是:1)解释为什么美国伊利诺伊州亚历山大县的Len Small堤防在维修过程中会在重大洪水事件中继续遭到破坏,以及2)开发新的加高堤道和堤防系统,从而提供密西西比河洪水旁路,是可持续的,鼓励和资助土地用途的变化,恢复退化的公路路基,保护尚未被过去洪水事件破坏的Dogtooth Bend农庄和农田,并在大型洪水事件期间提供洪水存储密西西比河和俄亥俄河的交汇处。

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