漫湾库区生产恢复障碍及其原因

在对漫湾库区调查的基础上，总结了库区生产恢复现状，认为农业生产相应条件恢复不到位，影响土地的持续利用：土地生产力降低，单一的种植业结构和产业结构，经济林与畜牧养殖业因土地被淹没带来萎缩，渔业、旅游业等缺乏规划和移民的参与，表现出库区移民生活水平相对于远迁移民、全县(省)平均下降了。分析了漫湾库区生产恢复的障碍及其原因，并就生产恢复提出一些建议：(1)提升澜沧江梯级开发水电工程中对移民问题的重视，将漫湾电站纳人中央直属电站范畴，统筹安排移民遗留问题，给予资金支持；(2)重新整体规划漫湾库区的移民安置，控制库区土地人口压力；(3)调整产业结构，促成传统种植业人口向林、牧业，向第二、三产业转移；(4)理顺和明确移民方面的责、权、利关系，将生产恢复问题与安置区地方经济发展问题结合起来考虑；(5)建立公众积极参与的决策体制与决策执行机制。     

金矿尾矿库渗漏后治理措施的探寻

分析了金矿尾矿库发生渗漏的原因,重点介绍了尾矿库渗漏后的综合治理措施。通过治理措施的实施,不仅解决了尾矿库渗漏问题,而且为尾矿库的增高扩容提供了良好的条件。其成功经验可以为类似金矿企业所借鉴。     

淤地坝坝地淤积与侵蚀性降雨的灰色关联分析

水土流失是黄土高原地区重要的环境问题之一,淤地坝措施作为该区水土流失治理的重要工程措施之一发挥了巨大作用,但其淤积过程与水毁机理的研究较少.本文在全面调查黄土高原淤地坝的基础上,选取典型淤地坝,挖取剖面进行测量和分层取样,利用库容曲线和实测每个淤积层的淤积厚度求得每层淤积泥沙量,运用灰色关联分析法,系统地研究了侵蚀性降雨的4个指标(降雨侵蚀力R、降雨量P、最大30 min降雨强度,I30、平均降雨强度 I)与坝地泥沙淤积量之间的关联度.结果表明,降雨侵蚀力 R和坝地泥沙淤积量的发展趋势最为密切,呈幂函数关系;降雨量 P对淤积量的影响仅次于降雨侵蚀力,其关系呈指数型;最大30 min降雨强度,I30和平均降雨强度I对坝地泥沙淤积量的影响较小.     

基于GDEM-PDyna的尾矿库溃坝三维数值模拟分析研究*

为进一步探究尾矿坝溃决后特有泥石流运移规律,掌握坝体破坏前至溃坝结束全流程发展状态,依托广东省某案例尾矿库为研究对象,采用基于有限元与离散元耦合方法的GDEM-PDyna软件构建泥石流类流体下泄演化数值模型,开展尾矿坝溃决演化分析,动态模拟尾矿库溃决过程中泥砂运动规律及淹没范围,并与MIKE 21软件计算结果进行对比。研究结果表明:尾矿坝溃决后,泥石流类流体流速升高、持续时间较短且尾砂流量发展迅速,2种模拟方法对比结果表明溃坝后坝基位置下泄流量变化与下游敏感点溃坝淹没深度变化情况一致。研究结果可为实现尾矿库下游重点区域灾害评估提供量化支撑,可有效提高尾矿坝溃决后灾害影响评估的精准性。     

Reservoir Sedimentation Rates in the Little Washita River Experimental Watershed,Oklahoma: Measurement and Controlling Factors

Forty‐five flood control reservoirs, authorized in the Watershed Protection and Flood Prevention Act 1954, were installed by United States Department of Agriculture (USDA) between 1969 and 1982 in the Little Washita River Experimental Watershed (LWREW), located in central Oklahoma. Over time, these reservoirs have lost sediment and flood storage capacity due to sedimentation, with rates dependent on upstream land use and climate variability. In this study, sedimentation rates for 12 reservoirs representing three major land use categories within LWREW were measured based on bathymetric surveys that used acoustic profiling system. Physiographic and climate attributes of drainage area of surveyed reservoirs were extracted from publicly available data sources including topographic maps, digital elevation models, USDA Natural Resource Conservation Service soils, and weather station databases. Correlation, principal component analysis, and stepwise regression were utilized to analyze the relationship between normalized reservoir sedimentation rates (ReSRa) and the drainage area characteristics to determine the major variables controlling sedimentation within the LWREW. Percent of drainage area with extreme slopes, saturated hydraulic conductivity, and maximum daily rainfall event recorded in spring explained most of the variability in ReSRa. It was also found that percent reduction in reservoir surface area can be used as a surrogate for estimating ReSRa. The implications of the results are discussed.     

Potential Impacts of Climate Change on the Reliability of Water and Hydropower Supply from a Multipurpose Dam in South Korea

Future climate change is a source of growing concerns for the supply of energy and resources, and it may have significant impacts on industry and the economy. Major effects are likely to arise from changes to the freshwater resources system, due to the connection of energy generation to these water systems. Using future climate data downscaled by a stochastic weather generator, this study investigates the potential impacts of climate change on long‐term reservoir operations at the Chungju multipurpose dam in South Korea, specifically considering the reliability of the supply of water and hydropower. A reservoir model, Hydrologic Engineering Center‐Reservoir System Simulation (HEC‐ResSim), was used to simulate the ability of the dam to supply water and hydropower under different conditions. The hydrologic model Soil and Water Assessment Tool was used to determine the HEC‐ResSim boundary conditions, including daily dam inflow from the 6,642 km² watershed into the 2.75 Gm³ capacity reservoir. Projections of the future climate indicate that temperature and precipitation during 2070‐2099 (2080s) show an increase of +4.1°C and 19.4%, respectively, based on the baseline (1990‐2009). The results from the models suggest that, in the 2080s, the average annual water supply and hydropower production would change by +19.8 to +56.5% and by +33.9 to 92.3%, respectively. Model simulations suggest that under the new climatic conditions, the reliability of water and hydropower supply would be generally improved, as a consequence of increased dam inflow.     

筋带密度对尾矿坝漫顶破坏规律影响研究

基于相似理论和溃决侵蚀原理,进行不同加筋密度条件下尾矿坝洪水漫顶破坏模 型试验,探析了筋带密度对尾矿坝漫顶破坏影响规律。试验结果发现:①随着筋带密度 的增加显著提升了尾矿坝的力学强度,但也导致了坝体内的浸润线升高;②筋带密度的 增加使溃口由“Y”型逐渐向“H”型转变;③筋带密度的增加阻滞了漫坝破坏的发展, 坝体位移及内部应力变化量明显减小;④增加筋带密度提高了坝体的抗冲刷能力,减弱 了洪水对蚀沟两岸尾砂的拉拽作用,保证了蚀沟两翼坝体的稳定;⑤随着筋带密度增加 ,可有效减小坝体位移和溃口深度、宽度的发展,当筋带超过2层后,筋带层数的增加 对坝体溃口宽、深基本无影响。研究成果深入探析了筋带密度对漫顶破坏影响规律,在 尾矿坝加筋研究方面提供了科学依据。     

尾矿坝地震液化评价可靠度模型及应用

为适应计算参数本身具有的随机性和未确知性,将可靠度理论引入尾矿坝地震液化评价中。以测试数据的统计分析结果为基础,应用一次二阶矩法建立尾矿坝地震液化分析可靠度模型,探讨了可靠度指标与抗液化安全系数之间的关系,并将该模型应用到某尾矿坝地震液化分析中。结果表明,新建可靠度模型各参数的物理意义与统计指标明确,相比传统的确定性分析方法,不仅能判断液化的发生与否,还能给出液化发生的概率;可靠度理论在液化分析中能更好地考虑计算参数的变异性,进一步完善了尾矿坝地震液化分析理论,为进行基于风险分析的尾矿坝抗震设计和地震安全评价提供更全面的依据。     

排水沟渠炉渣与底泥对水中氮、磷截留效应

通过等温热力学吸附实验,将炉渣、炉渣+30%底泥、排水沟渠底泥对水中氨氮的去除效果进行比较,并采用Langmuir等温吸附方程对3种基质吸附氨氮、磷酸盐的量进行拟合;通过动力学实验,比较3种基质吸附速率.结果表明,炉渣、炉渣+30%底泥、排水沟渠底泥对氨氮的最大吸附量分别为0.49,1.03,1.75mg/g,对磷酸盐的最大吸附量分别为0.99,2.33,1.88mg/g;4h内基质吸附氨氮速率分别为:0.10,0.11,0.54mg/(g·h),2h内基质吸附磷酸盐速率分别为:0.048,0.051,0.096mg/(g·h).由于沟渠底泥较为松散、遇水冲刷易流失,故选择炉渣作为沟渠基质坝的填充物.基质坝能够减缓渠水流速,延长渠水的水力停留时间(HRT).     

尾矿库溃坝风险定量评价方法探讨

针对目前尾矿库安全评价中无定量评价尾矿库溃坝风险的现状,坝体稳定性计算中未考虑到坝体实际为非均质体的特点,本文提出将容重、内摩擦角和凝聚力三者视为随机变量,采用蒙特卡洛模型计算尾矿坝溃坝失效概率;综合运用水文学、水动力学、非牛顿流体的运动理论,建立尾矿库溃坝后尾矿下泄模型,以计算溃坝淹没范围;综合考虑尾矿库溃坝后生命损失、财政损失和环境损失,计算尾矿库溃坝风险损失度;最终确定尾矿库溃坝风险度,以期提高尾矿库安全评价技术、确保尾矿库安全健康运行.