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HISTORIC DAM―INNOVATIVE UPGRADE OF SPILLWAY

机译:截止雪路的历史大坝 - 创新升级

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Black rock dam is an embankment dam built between 1904 and 1908 on the Zuni Indian Reservation in western New Mexico (United States of America), on the Zuni river. The dam site is a narrow gorge, 24.3 m deep, created by undermining outflows of water impounded by ancient basalt lava flows across the Zuni river. The intensely jointed basalt, overlain by several feet of unconsolidated surface deposits, forms the upper 9.1 to 12.1 m feet of the abutments. Beds of clayey sand and gravels underlie the basalt. The original spillway was excavated in the left abutment basalt. During the first filling in 1909, reservoir water flowed through fractures in the basalt, eroding the underlying soils, resulting in settlements of up to 2.7 m of the basalt blocks, the partial collapse of the spillway and near failure of the left abutment of the dam. Repairs to the abutment and a new spillway were completed in 1912. Despite attempts to limit flows through the basalt, the left abutment nearly failed from the same cause in 1932 and 1936. More recent inspections by the US Bureau of Reclamation under their Safety Evaluation of Existing Dams (SEED) program classified Black Rock dam as high hazard, and identified significant dam safety deficiencies of excessive seepage, inadequate spillway capacity, and poor condition of the outlet works. The outlet works improvements consist of a new intake structure, grouting a steel liner in the existing conduit, and a new terminal structure. Excessive seepage is controlled by construction of a 22.86 m deep cutoff trench through the upstream face of the dam, extending several hundred feet into each abutment. Spillway capacity is increased by modifying the existing spillway, and constructing a new auxiliary spillway. The estimated probable maximum flood (PMF) inflow peak is 1853.2 m~3/s 65,400 (cfs), and the routed outflow is 1800 m~3/s 63,500 (cfs). The spillway capacity before improvements was about 170 m~3/s 6,000 (cfs). Several spillway alternatives for passing the PMF were evaluated. The selected alternative consists of a movable crest in the existing spillway and constructing an auxiliary spillway on the left abutment. Fusegates were selected due to their low maintenance requirements, and their ability to pass normal flows as a service spillway while tipping at prescribed reservoir elevations to pass large floods without depending on mechanical equipment. In addition, an auxiliary spillway channel was excavated in the left abutment, left of the service spillway. The service spillway passes 907 m~3/s 32,000 (cfs) and the auxiliary spillway passes 892.6 m~3/s 31,500 (cfs), totaling the required outflow of 1800 m~3/s (63,500) (cfs).
机译:黑岩坝是1904年和1908年之间建在新墨西哥州西部(美国)祖尼印第安人保留地的土石坝,在祖尼河。坝址是一个狭窄的峡谷24.3米深,通过破坏的古代玄武岩熔岩蓄水流出创建跨祖尼河流。的强烈接合玄武岩,由松散表面沉积物的几英尺覆,形成基台的上9.1至12.1米脚。粘土砂床和砾石背后的玄武岩。原溢洪道在左坝肩开挖玄武岩。期间在1909年第一填充,水库水在玄武岩通过裂缝流动,侵蚀底层土壤,从而导致了的住区至2.7微米的玄武岩块,大坝的左侧邻接的溢洪道和邻近故障的部分塌陷。修复基台和一个新的溢洪道是在1912年完成尽管试图限制流经玄武,左坝肩来自同一原因下的安全性评价几乎未能在1932年和1936年更近的检查由美国垦务局现有水坝(SEED)计划分为黑岩大坝为高风险和过度渗漏,溢洪道泄洪能力不足的标识显著大坝安全缺陷,并出口工程的条件很差。出口作品的改进包括一个新摄取的结构,灌浆在现有管道中的内胆,并且一个新的终端结构。过度渗漏是由结构的22.86米深截止沟槽的通过大坝的上游面控制,几百英尺延伸到每个邻接。溢洪道容量增加通过修改现有溢洪道,构建一个新的辅助溢洪道。所估计的可能最大洪水(PMF)流入峰1853.2米〜3次/ s 65400(CFS),并且路由流出是1800米〜3次/ s 63500(CFS)。改进之前溢洪道容量为约170 M〜3次/ s 6000(CFS)。为使PMF几个溢洪道方案进行评估。所选择的替代方案在于在现有溢洪道的可动波峰和构建在左边邻接的辅助溢洪道的。 Fusegates是由于它们的低的维护要求选择,其通过正常流作为服务溢洪道而翻倒在规定的储存器的高度是通过大洪水,而不依赖于机械设备的能力。此外,辅助通道溢洪道被挖掘的左邻接,离开了服务溢洪道。服务溢洪道传递907米〜3次/ s 32000(CFS)和辅助溢洪道传递892.6米〜3次/ s 31500(CFS),共计1800米〜3次/ s(63,500)(CFS)所需的流出。

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