首页> 外文会议>Association of State Dam Safety Officials annual conference >EXTREME SEDIMENTATION PLANNING- PROACTIVE DESIGN FOR LONG TERM PERFORMANCE OF THE SRS - NORTH FORK OF THE TOUTLE RIVER, WASHINGTON
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EXTREME SEDIMENTATION PLANNING- PROACTIVE DESIGN FOR LONG TERM PERFORMANCE OF THE SRS - NORTH FORK OF THE TOUTLE RIVER, WASHINGTON

机译:极端沉降计划-SRS长期性能的主动设计-华盛顿州通特河的北叉

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The May 18, 1980 eruption of Mount St. Helens dramatically altered the hydrologic, hydraulic and sedimentation regimes of the Cowlitz and Toutle rivers. This event resulted in persistent high sedimentation rates in the sand bed Cowlitz River and increased probability of flooding for communities along the reach. The USACE's Sediment Retention Structure (SRS) on the North Fork Toutle River is a primary component of the long term sediment management plan. The SRS traps sediment and reduces sedimentation in the Toutle and lower Cowlitz River. Completed in 1989, the SRS was expected to operate in three stages over time: 1) nearly all sand-sized and larger particles are trapped; 2) sands begin passing the SRS in significant quantities; 3) gravels begin to pass the SRS. Currently in phase two, the SRS is passing sand in sufficient quantities to aggrade the lower Cowlitz River and affect flood protection. As the valley slope upstream of the SRS increases due to aggradation in this phase, the trapping efficiency of the project decreases and higher quantities of larger-grained sand particles pass the structure. Understanding performance of the SRS during phase two is a key to developing a responsive long term sediment management strategy. A fully coupled two-dimensional hydrodynamic model was developed from available LIDAR surveys of the Toutle River and associated sediment plain. The model was supplied with 28-year projected water and sediment inflow hydrographs to simulate future sedimentation of the SRS and to quantify the expected SRS trapping efficiency through the current design horizon (present to 2035). The timing, magnitude, and predicted deposition patterns upstream from the SRS were also studied for two project alternatives that retain sediment high in the system, by either modifying the SRS or developing sediment retention projects within the sediment plain upstream of the SRS. The USACE, Portland District is using a 2-D sediment model to demonstrate the effectiveness of proposed sediment management alternatives. Lessons learned from the application of this 2-D hydrodynamic sedimentation model can be applied to the predictive management of sediment in reservoirs and dams over long-term time horizons and in all types of hydrologic and sedimentation conditions.
机译:1980年5月18日,圣海伦斯火山的喷发大大改变了库里兹河和图特尔河的水文,水力和沉积状况。此事件导致库里茨河沙床持续出现高沉积速率,并增加了沿河社区洪水的可能性。 USACE在北叉图特尔河上的沉积物保留结构(SRS)是长期沉积物管理计划的主要组成部分。 SRS可以捕集Toutle和Cowlitz河下游的泥沙,并减少泥沙淤积。 SRS预计于1989年完成,随着时间的流逝,它将分三个阶段运行:1)几乎所有沙粒大小的颗粒都被捕获; 2)沙子开始大量通过SRS; 3)砾石开始通过SRS。目前处于第二阶段,SRS正在输送足够数量的沙子以凝结库里兹河下游并影响防洪。随着SRS上游在该阶段的凝结而增加的谷底坡度,该项目的捕集效率降低,并且大量的大颗粒沙粒通过了该结构。了解第二阶段SRS的性能是制定响应性长期沉积物管理策略的关键。通过对Toutle河和相关沉积物平原进行的LIDAR勘测,开发了一个完全耦合的二维水动力模型。该模型提供有28年的预计水和泥沙流入水线图,以模拟SRS的未来沉积,并通过当前的设计范围(到2035年)量化预期的SRS捕集效率。还通过修改SRS或开发SRS上游沉积物平原内的沉积物保留项目,研究了SRS上游的时间,大小和预测的沉积方式,以研究两种将泥沙保留在系统中的方案,以期将沉积物保留在系统中较高的位置。波特兰区USACE正在使用二维泥沙模型来证明拟议的泥沙管理替代方案的有效性。从这种二维水动力沉降模型的应用中学到的经验教训可用于在长时期内以及在所有类型的水文和沉积条件下对水库和大坝中的沉积物进行预测管理。

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