宝兴县两河口山体崩塌应急治理方案设计          下载免费PDF全文

袁鹏  赵大军  李佐春  陈仓  张佳兴  周宇  翟国兵  戚波 《探矿工程》2016,43(1):20-26

“4.20”四川芦山地震诱发了大量次生地质灾害,导致宝兴县两河口崩塌危岩体发育,威胁进出地震灾区的生命线工程省道S210,威胁周边企事业单位及居民人数超过500人,严重影响了抗震救灾和灾后的恢复重建。在充分考虑治理区自然情况的基础上,采取预应力锚索锚杆支护,桩板拦石墙与钢轨障桩联合治理,解除了在暴雨作用下,治理区危岩体顶部、崩坡积层和下部坡面上存在的危石灾害,解决了被动网立柱抗弯能力较弱的问题,形成障桩起保护作用。为宝兴县灾后重建赢得了时间。  相似文献   

青藏铁路沿线砾石方格固沙机理风洞模拟研究   总被引：3，自引：0，他引：3  

张克存  屈建军  牛清河  张伟民  韩庆杰 《地球科学进展》2010,25(3):284-289

通过对青藏铁路沿线砾石方格内风速特征、固沙效率的风洞模拟实验研究发现,当气流运行至砾石方格前缘,水平风速迅速降低,砾石方格对风速的削弱作用非常显著,达到50%左右。气流在沿砾石方格向下风向移动过程中,水平梯度风速逐渐减小,但其减小幅度比较缓慢。砾石方格中风速随高度的分布遵循对数规律,各方格间风速变化趋势相对稳定。砾石方格地表粗糙度在5.2cm左右,摩阻速度为2.4 cm/s。砾石方格中固沙量随着进口风速的增加而增加,在相同风速下,固沙量随离沙源距离的增加呈指数关系递减。  相似文献   

PRB技术在地下水污染修复中的研究进展   总被引：2，自引：0，他引：2  

崔海炜  孙继朝  向小平  张玉玺  刘景涛 《地下水》2010,32(3):81-83

在综合分析可渗透反应墙（PRB）修复污染技术基础上,提出了存在问题及发展趋势,进而理出需通过深入研究,提高修复系统性能及其可行途径。预计在不远的将来,PRB处理工艺的持续性也同样会有大幅度改进和发展。  相似文献   

Geochemical study of clays used as barriers in landfills   总被引：1，自引：0，他引：1  

AbdelIllah Bezzar  Denis François  Fouad Ghomari 《Comptes Rendus Geoscience》2010,342(9):695-700

This is a hydraulic and geochemical study on 2 materials: natural clay (AN) and a regenerated material made up of a sand-bentonite (SB) mixture. The hydraulic part allowed us to conclude that a 10% industrial bentonite content mixed with sand offers hydraulic properties that are similar to those of AN material and are lower than the required standards. The geochemical properties of both AN and SB matrixes are comparable with those of some of the synthetic leachates studied. Furthermore, the Langmuir model helped us to identify the adsorption capacities of both matrixes with the following selectivities: Pb > Cu > Cd > Zn.  相似文献   

Seasonal variation of the barrier layer in the PN section     

张媛  吴德星  林霄沛  山峰 《中国海洋湖沼学报》2009,27(2):192-201

In this paper, we use the conductivity-temperature-depth (CTD) observation data and a three-dimensional ocean model in a seasonally-varying forcing field to study the barrier layer (BL) in the PN section in the East China Sea (ECS). The BL can be found along the PN section with obviously seasonal variability. In winter, spring and autumn, the BL occurs around the slope where the cold shelf water meets with the warm Kuroshio water. In summer, the BL can also be found in the shelf area near salinity front of the Changjiang (Yangtze) River Dilution Water (YRDW). Seasonal variations of BL in the PN section are caused by local hydrological characteristics and seasonal variations of atmospheric forcing. Strong vertical convection caused by sea surface cooling thickens the BL in winter and spring in the slope area. Due to the large discharge of Changjiang River in summer, the BL occurs extensively in the shelf region where the fresh YRDW and the salty bottom water meet and form a strong halocline above the seasonal thermocline. The formation mechanism of BL in the PN section can be explained by the vertical shear of different water masses, which is called the advection mechanism. The interannual variation of BL in summer is greatly affected by the YRDW. In the larger YRDW year (such as 1998), a shallow but much thicker BL existed on the shelf area. Supported by National Basic Research Program of China (973 Program, No. 2005CB422303 and 2007CB411804), the Key Project of the International Science and Technology Cooperation Program of China (No. 2006DFB21250), the “111 Project” of the Ministry of Education (No. B07036), the Program for New Century Excellent Talents in University, China (No. NECT-07-0781)  相似文献   

高放处置罐铁释放诱发膨润土矿物相变研究进展          下载免费PDF全文

张明  谢敬礼 《岩石矿物学杂志》2021,40(4):778-785

作为高放废物处置罐候选金属材料,低碳钢在处置库服役期间,其腐蚀产物侵入缓冲屏障,导致缓冲材料矿物相变与性能变异,威胁多重屏障体系的长期安全稳定。本文详细综述了国内外处置库深部还原环境所处的弱碱性化学场与中低温度场的变化趋势,认为处置库深部化学-温度还原条件可导致处置罐Fe腐蚀释放Fe~(2+)。在处置库长期运行过程中,蒙脱石与Fe~(2+)接触发生矿物相变,一方面Fe~(2+)置换蒙脱石八面体晶格中的Al~(3+)和Mg~(2+),还原Fe~(3+)或直接占据空位,生成次生矿物;另一方面Fe~(2+)交换蒙脱石层间的Na~+、K~+和Ca~(2+),转化为铁基蒙脱石。矿物相变可诱发缓冲屏障性能变异甚至退化。基于"抗矿物转化"理念,提出了下一阶段缓冲材料矿物相变研究方向,为地下实验室碳素钢选型、缓冲屏障验证试验设计以及屏障体系安全评价提供科学依据。  相似文献   

2000—2021 年影响山东的北上台风分类及降水落区分析          下载免费PDF全文

王媛  郑丽娜 《沙漠与绿洲气象(新疆气象)》2023,17(2):162-169

将2000—2021年影响山东的15个台风，按大尺度环流形势进行分类，以台风登陆之后500 hPa中纬度是否存在槽进行分类，可以分为3类：（1）中纬度有槽且形成闭合中心，台风与槽结合，在山东产生暴雨以上量级的降水；（2）中纬度只有高空槽，降水范围最大；（3）中纬度无明显槽脊，降水量和降水范围最小。以西太平洋副热带高压（简称“副高”）的位置分类，可分为3类：（1）副高西伸脊点过120°E且北部边缘过40°N，台风沿副高外围移动，降水最少；（2）副高西伸脊点不过120°E且北部边缘过40°N，高空槽与副高在中国沿海交汇，降水范围广，山东降水与台风位置有关。位置偏西，降水范围大；位置偏东，降水主要集中在山东半岛地区；（3）副高西伸脊点不过120°E且北部边缘不过40°N，台风环流中心较强，降水最强。以700 hPa环流形势分类，分为3类：（1）700 hPa有高压坝，降水范围最小；（2）700 hPa无高压坝，东北地区有冷涡，山东降水量和降水范围最大；（3）700 hPa无高压坝，中纬度存在大槽，降水量均可达大暴雨量级。  相似文献