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20th Anniversary of El Guapo Dam Failure

机译:漂亮的大坝失败20周年

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摘要

El Guapo Dam, which impounded a reservoir volume of over 32,000 acre-feet, was constructed from 1975 to 1980 on the Rio Guapo in the state of Miranda in northern Venezuela. Over about a two-week period in December 1999, heavy rainfall in the mountains of northern Venezuela were relentless. On December 14, 1999, the reservoir at El Guapo Dam rose to about 3 feet above normal pool, but still had an additional 15 feet of freeboard . However, due to additional heavy rainfall overnight and the extremely saturated ground conditions in the watershed, the reservoir levels quickly rose to within about 2 feet of the dam crest by the morning of December 15. By December 16, the reservoir rose to within a 1/2 foot of the dam crest. Due to the high-water surface elevation and increased runoff, the spillway chute sidewalls began to overtop from the record amount of discharge. Erosion of the fill behind the walls began to occur almost immediately. Within a matter of hours and with no means to further manage the enormous inflows, the areas below the dam were evacuated. The reservoir levels began to decrease as the morning progressed; however, additional rainfall in the afternoon caused the reservoir to rise again sharply. The spillway chute sidewalls continued to overtop, and the erosion quickly accelerated beneath and up the chute. As the chute failed into the scoured areas, the head cutting progressed and ultimately led to a breach of the spillway control section at about 5 PM on December 16. The failure of El Guapo Dam has many striking similarities to the recent spillway incident in Oroville Dam. This presentation will explore those similarities, reflect on emergency preparedness and response, and re-examine many of the potential failure modes and critical design and construction considerations for these structures.
机译:El Guapo大坝扣押了超过32,000英亩脚的储层体积,于1975年至1980年,于委内瑞拉北部米兰达的Rio Guapo建造。在1999年12月,北委内瑞拉山脉的大雨降雨量无情。 1999年12月14日,El Guapo Dam的水库上升到正常水池以上约3英尺,但仍有15英尺的干舷。然而,由于额外的大雨过夜和流域的极其饱和的地面条件,在12月15日上午,水库水平迅速升至大坝峰的大约2英尺内。到12月16日,水库升至1内/ 2脚的大坝嵴。由于高水面升高和径流增加,溢洪道斜壁侧壁开始从记录的放电量概述。墙壁后面的浸没开始发生几乎立即发生。在几个小时内,没有进一步管理巨大流入的方法,大坝以下的区域被疏散。随着早晨进展,水库水平开始减少;然而,下午的额外降雨导致水库急剧上升。溢洪道斜墙继续泛镜,侵蚀迅速加速在下面和斜槽下方。随着斜槽进入穿孔区域,头部切割进展并最终导致了12月5日下午5点突破了溢洪道控制部分。埃尔·郭坝大坝的失败与最近的奥洛维尔大坝的溢洪道有很多惊人的相似之处。本演示文稿将探讨这些相似之处,反映了应急准备和反应,并重新审查这些结构的许多潜在的失效模式和批判性设计和施工考虑。

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