镜泊湖火山台网防雷地网的建设

镜泊湖火山台网位于崇山峻岭之中,经常遭到强雷电袭击。为了使台网设备稳定高效运转,减轻雷电地干扰,我们对台网的防雷设施进行了建设,取得了非常好的防雷效果。     

Early Diagenetic Dolomite as a Potential Archive of Paleo-redox Fluctuations in an Early Tonian Marine Basin?

The Tonian Period witnessed important environmental changes and critical evolutionary innovations. Published iron speciation data suggest a global redox transition of mid-depth seawaters from euxinic to ferruginous in early Tonian, but details of this transition remain unknown. This study explores Tonian stromatolitic carbonates as a possible archive of paleoenvironmental changes, through the investigation of dolomitic limestones and dolostones associated with stromatolites of the Weiji Formation in the Huaibei region of North China. Three types of dolomitization are recognized on the basis of petrographic and geochemical data. Type I and II dolomitization resulted in dolomitic limestones characterized by LREE depletions, MREE enrichments, positive yttrium anomalies, and a lack of europium anomalies, indicating early diagenetic dolomitization, possibly in the iron reduction zone and under the influence of bottom seawater. The lack of cerium anomalies in these carbonates suggests anoxia in shallow marine environments. The coexistence of ferroan/non-ferroan dolomite crystals and overgrowth bands is interpreted as possible evidence for rapid fluctuations between iron-rich and iron-depleted conditions in pore-waters or seawaters. In contrast, type III dolomitization resulted in pervasively dolomitized stromatolitic carbonates and likely represents late diagenetic processes. This study highlights the potential of early diagenetic dolomite as an archive for paleoenvironmental investigations.     

Communicating geomorphology: global challenges for the twenty‐first century

The British Society for Geomorphology (BSG), established as the British Geomorphological Research Group (BGRG) in 1960, is considering how best to represent geomorphology and geomorphologists in the light of recent changes in the nature of communication. These changes provide the BSG and other academic societies with challenges and opportunities. Seven drivers of communication change are outlined: the changing position of geomorphology in higher education, the nature of academic interaction, the means of communication available, a transformation in the nature of geomorphological research, changes in funding support, the government role in resource allocation, and developments in quantifying international research impact. Challenges arising from changing communications are identified as occurring beyond the ‘academy’, in the nature of publication within the ‘academy’, and associated with meetings of the ‘academy’. Although national societies now have to contemplate significantly different purposes to provide for their members than in the twentieth century, there are opportunities available that cannot be fulfilled by international organizations alone. Copyright © 2013 John Wiley & Sons, Ltd.     

Geochemistry of rare earth elements in the mid-late Quaternary sediments of the western Philippine Sea and their paleoenvironmental significance

Based on a δ18O chronology,rare earth elements(REE) and other typical elements in sediments from core MD06-3047 in the western Philippine Sea were analyzed to constrain the provenances of the sediments and investigate quantitative changes in the Asian eolian input to the study area over the last 700 ka.Among the competing processes that might affect REE compositions,sediment provenance is the most important one.Provenance analysis suggests that the study sediments have two provenance end-members;local volcanic sources are dominant,and eolian dust from the Asian continent has a smaller contribution.During glacial periods,eolian input to the western Philippine Sea was enhanced.In contrast,material supply from local volcanics increased during interglacial periods.Changes in eolian input to the study area were probably related to the strength of the East Asian winter monsoon(EAWM) as well as aridity in the Asian continent on an orbital time scale,and were partly influenced by local control factors on shorter time scales.Therefore,we propose that the present study expands the application of the REE-based method for quantitatively estimating the eolian component from the mid-latitude northern Pacific to the low-latitude western Pacific.Additionally,the study preliminarily confirms the influence of EAWM-transported eolian material on sedimentation in the western Philippine Sea since 700 ka.     

盾构隧道实测土压力分布规律及影响因素研究

以大量现场实测土压力为基础,分析了影响盾构隧道衬砌土压力的一些主要因素,总结出不同地层地铁盾构隧道长期稳定土压力的分布规律,并探讨了盾构施工期土压力随时空的变化情况。研究得出,地下水位高低对稳定土压力大小及分布影响较大;作用在管片上的长期土压力大小与地层衬砌刚度系数有关,当地层衬砌刚度系数为1.5时,管片竖向及水平土压力都较小;盾构施工期临时荷载对管片土压力影响不可忽视,无论是黏土地层还是砂土地层,大的注浆压力及注浆率将导致作用在管片上的稳定土压力分布不均;管片土压力可按时空分为4个阶段,拼装阶段、同步注浆阶段、浆液凝固阶段及后期稳定阶段,其中同步注浆阶段管片周边最大土压力为稳定阶段的2～3倍。     

刚性桩复合地基侧向土压力试验研究

通过室内模型试验,实测得到试验条件下,天然地基和刚性桩复合地基作用在不允许有位移的刚性挡土墙上的侧向土压力;通过与天然地基对比分析,获得了刚性桩复合地基的侧向土压力特性及分布规律。结果表明,刚性桩复合地基中桩的参与（包括桩的荷载深层传递作用、桩负摩擦区的影响和桩体对桩间土水平附加应力的“遮拦”作用等）使复合地基侧向土压力大小和分布规律明显区别于天然地基;在给定荷载水平下,刚性桩复合地基的侧向土压力值低于天然地基,侧向土压力影响范围较天然地基作用位置更深;在试验条件下,刚性挡土墙距离建筑物0.35～1.4 m范围内,当荷载水平达到地基承载力特征值时,刚性桩复合地基作用在刚性挡土墙上的总土压力和附加土压力约为天然地基的43.3%～80.1%和15.9%～59.8%。     

竖向稳定渗流条件下的地震主动土压力分析

基于库仑土压力理论的基本假定和拟动力法的分析思路,以无黏性填土的刚性挡土墙为研究对象,考虑填土中存在竖向稳定渗流的两种工况,推导了地震主动土压力和修正土压力系数的计算表达式。通过程序求解问题并进行参数讨论,分析结果表明,主动土压力随水平地震加速度的增大而明显增大,竖向地震加速度对土压力影响较小,可以忽略不计。墙土摩擦角较小时,土压力随填土摩擦角的增大而单调减小,但当墙土摩擦角增大后,土压力随填土摩擦角的增大出现先减小后增大的情况。渗流方向向下时,土压力随水力梯度的增大而减小;渗流方向向上时,变化规律则相反。与已有的理论方法对比,计算结果基本吻合,验证了该理论方法的正确性。     

稀土元素地球化学分析在地质学中的意义

稀土元素在地质学中具有重要的示踪意义,通过对稀土元素的地球化学特征进行研究,可以很好地解释一些地质现象,揭示矿物甚至矿床的成因,指导找矿,为地质学的发展提供有力的技术支撑.     

四川前陆盆地上三叠统须家河组物源区分析及其地质意义

为了深入认识四川前陆盆地须家河组沉积物源方向及物源区构造背景,对该盆地次级构造单元内须家河组砂岩碎屑组分、岩屑类型、重矿物组合特征、稀土元素和微量元素进行了分析。结果表明,盆地中的碎屑物源主要来自再旋回造山带,部分可能来自造山之前的混合区,不同的构造单元和层位存在不同物源区的特点：川西坳陷物源主要受龙门山逆冲推覆带控制;川东北坳陷物源主要受米仓山-大巴山逆冲推覆带控制;川东南坳陷物源受雪峰古陆控制,而川中古隆起物源则主要来自南部峨眉瓦山古陆。物源区具有大陆边缘向大陆岛弧转化的构造演化特点,须四期龙门山的逆冲推覆活动明显强于须二期。