Numerical modeling and simulation of pile in liquefiable soil     

Zhao Cheng  Boris Jeremić 《Soil Dynamics and Earthquake Engineering》2009,29(11-12):1405-1416

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宁夏数字地震观测网络项目之网络设计与综合评价   总被引：3，自引：3，他引：0  

吉祥  赵静  张淑贤  吴晓燕  谢辉  沈宁 《震灾防御技术》2009,4(3):355-361

宁夏数字地震观测网络项目信息服务分项项目组作为整个网络系统集成组,在信息网络系统的建设过程中,依据不同地震观测项目对信道速率、连续率、实时性、网络延时等通信要素的不同要求,考虑到不同节点的基础通信条件的差异,在采用平面星型网络拓扑结构作为总的通信策略的同时,实地考察、科学分析、统一规划、综合布局,对不同类型的节点分别采用不同的通信信道组合策略作为节点的接入方式,采用以OSPF为主要路由协议的多路由协议集成,全面解决了宁夏数字地震观测网络项目的整体通信和路由融合问题,同时也为其他观测项目的数据传递和汇聚提供了可靠的通信网络平台。  相似文献   

Geochemical, Sr–Nd and zircon U–Pb–Hf isotopic studies of Late Carboniferous magmatism in the West Junggar, Xinjiang: Implications for ridge subduction?     

Hongyan Geng  Min Sun  Chao Yuan  Wenjiao Xiao  Weisheng Xian  Guochun Zhao  Lifei Zhang  Kenny Wong  Fuyuan Wu 《Chemical Geology》2009,266(3-4):373-398

Voluminous granitic intrusions are distributed in the West Junggar, NW China, and they can be classified as the dioritic rocks, charnockite and alkali-feldspar granite groups. The dioritic rocks (SiO₂ = 50.4–63.8 wt.%) are calc-alkaline and Mg enriched (average MgO = 4.54 wt.%, Mg^# = 0.39–0.64), with high Sr/Y ratios (average = 21.2), weak negative Eu (average Eu/Eu = 0.80) and pronounced negative Nb–Ta anomalies. Their Sr–Nd and zircon Hf isotopic compositions ((⁸⁷Sr/⁸⁶Sr)_i = 0.7035–0.7042, ε_Nd(t) = 4.5–7.9, ε_Hf(t) = 14.1–14.5) show a depleted mantle-like signature. These features are compatible with adakites derived from partial melting of subducted oceanic crust that interacted with mantle materials. The charnockites (SiO₂ = 60.0–65.3 wt.%) show transitional geochemical characteristics from calc-alkaline to alkaline, with weak negative Eu (average Eu/Eu = 0.75) but pronounced negative Nb–Ta anomalies. Sr–Nd and zircon Hf isotopic compositions ((⁸⁷Sr/⁸⁶Sr)_i = 0.7037–0.7039, ε_Nd(t) = 5.2–8.0, ε_Hf(t) = 13.9–14.7) also indicate a depleted source, suggesting melts from a hot, juvenile lower crust. Alkali-feldspar granites (SiO₂ = 70.0–78.4 wt.%) are alkali and Fe-enriched, and have distinct negative Eu and Nb–Ta anomalies (average Eu/Eu = 0.26), low Sr/Y ratios (average = 2.11), and depleted Sr–Nd and zircon Hf isotopic compositions ((⁸⁷Sr/⁸⁶Sr)_i = 0.7024–0.7045, ε_Nd(t) = 5.1–8.9, ε_Hf(t) = 13.7–14.2). These characteristics are also comparable with those of rocks derived from juvenile lower crust. Despite of the differences in petrology, geochemistry and possibly different origins, zircon ages indicate that these three groups of rocks were coevally emplaced at ~ 305 Ma.A ridge subduction model can account for the geochemical characteristics of these granitoids and coeval mafic rocks. As the “slab window” opened, upwelling asthenosphere provided enhanced heat flux and triggered voluminous magmatisms: partial melting of the subducting slab formed the dioritic rocks; partial melting of the hot juvenile lower crust produced charnockite and alkali-feldspar granite, and partial melting in the mantle wedge generated mafic rocks in the region. These results suggest that subduction was ongoing in the Late Carboniferous and, thus support that the accretion and collision in the Central Asian Orogenic Belt took place in North Xinjiang after 305 Ma, and possibly in the Permian.  相似文献   

Rocky desertification and its causes in karst areas: a case study in Yongshun County,Hunan Province,China   总被引：9，自引：0，他引：9  

Y.?J.?Xiong  G.?Y.?QiuEmail author  D.?K.?Mo  H.?Lin  H.?Sun  Q.?X.?Wang  S.?H.?Zhao  J.?Yin 《Environmental Geology》2009,57(7):1481-1488

Rocky desertification, a process of land degradation characterized by soil erosion and bedrock exposure, is one of the most serious land degradation problems in karst areas, and is regarded as an obstacle to local sustainable development. It is well known that human activities can accelerate rocky desertification; however, the effects of climate change on rocky desertification in karst areas are still unclear. This study focused on the effects of temperature and precipitation changes and human activities on rocky desertification in karst areas to determine the impacts of climate change and human disturbances on rocky desertification. Areas of different level of rocky desertification were obtained from Landsat TM (1987) and Landsat ETM+ (2000) images. The results show that, although the total desertification area increased by only 1.27% between 1987 and 2000, 17.73% of the slightly desertified land had degraded to a moderate or intense level, 2.01 and 15.71%, respectively. Meanwhile, between 1987 and 2000, the air temperature increased by 0.7°C, and precipitation increased by 170 mm. Statistical results indicate that the increase in precipitation was caused by heavy rainfall. In addition, under the interactive influences of heavy rainfall and temperature, the average karst dissolution rate was about 87 m³ km⁻² a⁻¹ during the 14 years in the study area. Further analysis indicated that rocky desertification was positively related with the increase in temperature and precipitation and especially with the heavy rainfall events. Climate change accelerated rocky desertification in the karst areas. Electronic supplementary material  The online version of this article (doi:) contains supplementary material, which is available to authorized users.  相似文献   

Synthesis,algal inhibition activities and QSAR studies of novel gramine compounds containing ester functional groups     

李霞  于良民  姜晓辉  夏树伟  赵海洲 《中国海洋湖沼学报》2009,27(2):309-316

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从鄂尔多斯盆地油气勘查历程谈李四光找油气思想的发展   总被引：2，自引：0，他引：2  

赵文津 《地学前缘》2011,18(2):242-257

鄂尔多斯盆地正在以苏里格大气田为基础建设中国第二个大庆油田--"陕蒙大庆".鄂尔多斯盆地油气勘查经历了一个复杂曲折过程,人们曾多次对这一盆地的找油气的前景产生怀疑,经过近30年的探索,在1970年发现庆阳三叠系油田以后才开始取得了重要进展.1988年发现了下古生界的靖边气田,2000年苏6井揭示了苏里格大气田,盆地的勘...  相似文献   

CYP1A mRNA expression in redeye mullets (Liza haematocheila) from Bohai Bay, China     

An L  Hu J  Yang M  Zheng B  Wei A  Shang J  Zhao X 《Marine pollution bulletin》2011,62(4):718-725

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震害评估系统中的宏观经济指标的网格化技术及实现   总被引：1，自引：0，他引：1  

刘双庆  赵国敏  姚兰予 《震灾防御技术》2011,6(1):59-68

国内当前的地震灾害应急评估系统基础数据库以具有空间面属性的乡镇级行政区为最小统计单元,乡镇人口及各类房屋建筑面积在评估时一般按照行政区面积进行了平均化处理,而未考虑实际人口分布的差异.本文采用前人在人口密度与城乡空间分布及城乡GDP分布之间的统计模型,以及基于宏观经济指标的地震灾害快速评估思路,深入探讨了以乡镇行政区为...  相似文献   

气候变暖对刚察县采暖气象指标的影响及节能潜力分析   总被引：1，自引：0，他引：1  

朱宝文  侯俊岭  哈承智  宋理明  赵泽 《气象科技》2011,39(6):736-740

利用青海省刚察县1961—2008年逐日气温资料,运用数理统计等方法,分析了该地区采暖期气象条件变化及节能潜力。结果表明,1961—2008年间,刚察县采暖期平均气温上升,负积温减少,采暖初日推迟、终日提前,采暖长度明显缩短;采暖度日与采暖期平均气温关系密切,采暖度日呈极显著下降趋势,特别是1994年气温突变后,下降趋势更加明显,冬季寒冷程度有所减弱,能耗需求量减小;该县采暖能源需求异常偏多主要分布在20世纪60年代,偏多年份以70—80年代为主,偏少年份出现在80年代中期以后,主要集中在2000年以后。气候变暖所致采暖节能率为7%,这对节约能源、减少大气污染和温室气体排放较为有利。  相似文献   

重庆市伏旱时空变化特征   总被引：3，自引：0，他引：3  

李梗  刘晓冉  刘德  唐红玉  叶钊 《气象科技》2011,39(1):27-32

利用1961—2008年重庆34个台站的逐日降水资料,采用主成分分析、旋转主成分分析等方法对重庆伏旱变化的时空特征进行了分析。结果表明：重庆中西部是伏旱高频区,约10年7遇,且多重伏旱。重庆伏旱的第1载荷向量场表明重庆伏旱变化具有很好的整体一致性。重庆伏旱空间异常可分为4个区,即西部区、东北部区、东南部区和中部区。西部伏旱在1960—1970年代最强,东北部伏旱在90年代最强,其次是70年代,中部伏旱在70年代最强,其次是2000年以后,东南部伏旱的年代际变化趋势不明显,且伏旱整体较轻。  相似文献