基于可靠度理论的滑坡稳定性分析

基于可靠度理论,利用可靠度理论中的概率矩点估计法对延安市宝塔区卧虎山滑坡的稳定系数、可靠度和破坏概率进行了计算、分析。计算结果表明,基于可靠度理论滑坡稳定性计算能克服客观存在的土性参数的空间离散性、时间变异性,并把计算结果与传统稳定性计算结果进行了分析比较,证明了基于可靠度理论的滑坡稳定性计算方法的可靠性和可行性。     

Links between bacterial communities in marine sediments and trace metal geochemistry as measured by in situ DET/DGT approaches

Our current view about the relationship between metals and bacteria in marine sediments might be biased because most studies only use ex situ approaches to quantify metals. The aim of the present research was to compare ex situ and in situ methods of metal measurement (DET and DGT--diffusive equilibration or diffusive gradients in thin-films) and relate the results with two commonly used microbiological variables (bacterial biomass and bacterial diversity as revealed by DGGE). No previous studies have used such in situ approaches in microbial ecology. For biomass and most of the investigated trace metals (Ag, Cd, Sn, Cr, Ni, Cu, Pb, and Al) no significant correlations were found. The exceptions were Fe, Mn, Co, and As which behave like micronutrients. For bacterial diversity, no relevant relationships were found. We conclude that in situ methods are more adapted tools for microbial ecologists but that ex situ approaches are still necessary.     

塔中上奥陶统台缘带高频层序地层特征与储层纵向分布

利用钍/钾比分析技术,结合岩心与常规测井资料,可识别并划分对比塔中上奥陶统台缘带碳酸盐岩高频层序.分析表明,奥陶系碳酸盐岩呈明显米级旋回变化,在60 m井段识别出20个短周期旋回、4个长周期旋回,单个旋回厚度2~4 m.高频层序与礁滩体沉积旋回具很好对应关系,可用于沉积旋回精细划分与对比.礁滩体储层呈多旋回米级变化,长周期旋回顶部与优质储层对应非常好.高频层序与储层对比分析表明,优质储层主要发育在海平面向上变浅的米级旋回中,井间对比分析也呈相同特点.钻井分析表明,在3个海平面变浅的长周期旋回顶面均是优质储层发育段,3期长周期旋回的海平面下降期暴露面形成3套优质储层发育段.结果表明,高频层序与优质储层发育关系密切,准同生期溶蚀作用主要发育在相对海平面下降的米级旋回暴露期礁滩体中.     

地磁暴的危害

地磁暴是与太阳表面的扰动相联系的,地球磁场强烈的、有时还是迅速的波动。虽然这些短暂的磁扰动还未被广泛认识,但对人类和财产可造成重大的危害。许多人都知道,北极光的亮度在磁暴期间增强,但极少有人了解,这些磁暴会引起重大停     

西安地裂缝变形带中的剪切波速测试分析

文章依托西安地铁二号线工程,对跨地裂缝的地层进行剪切波速测试,通过对测试结果的分析确定了地裂缝变形带内的剪切波速变化规律,给出了地裂缝变形带地裂缝上盘影响带宽度小于3.5～5.7m,下盘影响带宽度小于2.0～3.3m,其结果与现行的相关规程中的参数吻合,为规程提供了强有力的科学依据。     

"8·16"暴雨过程的湿位涡诊断分析

本文利用实况资料和T213输出资料,对发生在2005年8月16日～17日的华北暴雨过程进行了湿位涡数值诊断分析,结果表明,强降水落在湿相对位涡的负值中心附近,且湿相对位涡场的特征主要取决于其正压项的贡献。在暴雨出现前期,湿对称不稳定主要在高层,湿位涡的下传可能是产生暴雨的重要原因之一。湿位涡的负值中心与中低层涡度的增大及暴雨的增强存在密切的关系。