标题: 石门水库垂直分层泥砂浓度监测技术研发及现场测试评估
Shihmen Reservoir suspended sediment concentration vertically layered monitoring technique development and field evaluation
作者: 林志平
钟志忠
国立交通大学 
关键字: 分层;异重流;水库; ;Layer-integrated;Density Current;Reservoir; 
公开日期: 2016
摘要: 为评估水库最佳防淤策略,水库的来水来砂特性为重要关键,对于洪水监测,各水库已施作多年,但泥砂监测资料目前仅石门、曾文与南化水库有较多资料,其他水库并不完整,且泥砂监测过程中问题颇多,故建立水库泥砂资料是目前水库整体防淤策略重要基本工作,依据“水库泥砂监测技术暨防淤操作策略研究”计画之水库入库泥砂监测技术初步规划,各水库泥砂浓度观测仪器设置之步骤,主要先从入库边界浑水明渠流之缓流区及各排放口开始,原因在于水库管理单位希望能掌握入库含砂浓度进而得知入库总砂量,以及得知各排放口或取水工附近高泥砂浓度变化情形,进而调整水库放水与取水时间。石门水库罗浮站在右岸斜坡建置分层抽水取样设施及悬浮质浓度自动化观测点,虽已提供较有根据的入库泥砂估计,但受边壁效应影响使其量测之河道泥砂浓度可能存在相当程度的变异性,如何获得断面代表性的含砂浓度,为河道输砂观测相当重要但较欠缺的一环。
因此本研究拟延续前期计画成果,评估既有罗浮测站与新建主深槽观测桩之差异性,精确量化入库泥砂浓度历线,建立全洪程水库水砂运移规律,有效掌握水库防淤操作时机及提升防淤效率同时进行探讨集水区崩坍面积与入库流木量及泥砂量之关系,跨域协调林业主管机关与水土保持主管机关联合预防土砂灾害,汇整土砂来源与林木资源化之参考。最后入库边界掌控集水区水砂资源控制站,提升水库稳定供水与防淤功能,整合集水区相关治理单位,确实掌握土砂主要源头,达到土砂管理与林木资源之分工合作。
 
To assess the best reservoir siltation prevention strategy, reservoir runoff sediment characteristic is the key to flood monitoring. This feature was monitored in various reservoirs but only Shihmen, Zhengwen and Nanhua reservoirs retained much more and complete monitoring information. Incomplete data and monitoring issues existed in other reservoirs, thus constructing a complete reservoir sediment database is the fundamental work in reservoir siltation prevention strategy. According to the preliminary planning in “Reservoir suspended sediment concentration monitoring technique and desiltation operation strategy research project”, suspended sediment monitoring equipment setup mainly begins from establishing monitoring stations at the flow buffer area of turbid water open channel flow and each outlet. This is mainly due to the reservoir management unit would wish to understand the inflow suspended sediment concentration to master the total sand inflow amount, and by knowing suspended sediment concentration variation of each discharge outlets or water, reservoir operation of water discharge or intake could be adjusted accordingly. Luofu monitoring station in Shihmen reservoir upstream had vertical layered water sampling equipment and automated suspended sediment concentration installed at the slope of the right embankment. Although there was relatively evidence-based sediment inflow estimation available currently, side boundary effect may induce substantial variation in river suspended sediment concentration measurement. Methods to gather representative sediment concentration at specific cross-sections are very important but yet lacking for river sediment transportation monitoring.
This study is hence a successor of previous research outcome, to evaluate the differences between current Luofu river bank monitoring station and newly established observation pole in main channel, to accurately acquire inflow sediment concentration historical data, to establish reservoir sediment migration pattern during flood events, to effectively master optimal timing of reservoir desiltation operation and enhance desiltation efficiency. While at the same time, this study investigates relationship between landslide area within catchment region and amount of inflow driftwood and sediment, which would assist in cross-border coordination between forestry authorities and soil-water conservation authorities to jointly prevent debris flow disaster, and to compile all sources of earth and soil and forest resources management as reference. Control station monitoring the end inflow boundary could master catchment area water and soil resources, which could enhance reservoir water supply stability and siltation prevention, integrating catchment area management related authorities, in turn to master main sand source and achieve collaboration between soil management and forestry resources fields.
 
官方说明文件#: MOEAWRA1050356 
URI: https://www.grb.gov.tw/search/planDetail?id=11839771&docId=483636
http://hdl.handle.net/11536/131757
显示于类别:Research Plans