纸质出版:2003
移动端阅览
[1]陈新民,严三保,阎长虹,罗国煜,刘义怀,陈家伟.场地断裂活动效应的风险分析与评价——以宿迁三线船闸为例[J].防灾减灾工程学报,2003(01):29-33.
陈新民, 严三保, 阎长虹, et al. Risk Analysis and Evaluation of Site Fault Activity Effects——A Case Study of Suqian Ship Lock Group[J]. 2003, (1): 29-33.
断裂研究是区域和场地稳定性评价以及工程抗震设计中的一项重要的基础性工作。对于有断裂通过的工程场地
从断裂、场地土层和工程三者相互作用的角度出发
开展有针对性的场地断裂活动效应及地震稳定性研究
对保证工程的安全建设和可靠运行有着极为重要的现实意义。本文试以宿迁三线船闸的建设为例
对场地断裂活动效应的风险进行分析与评价。
Suqian ship lock group locates in the mid-south segment of famous Tancheng-Lujiang Fault
where a large earthquake of M8. 5 once occurred in history. From the view of interaction among fault
site and construction
the fault activity and seismic stability in the site of Suqian ship lock group are studied for the risk analysis and evaluation of site fault activity.The geological survey of the site shows that the main site fault across Suqian ship lock group affects the soil layers to a depth of 20 m or more which is 5 ?5 m under the base of lock chambers. The fault will not be exposed when the soil is excavated for building lock
whereas the distribution of faults provides a favourable tectonic condition for earthquake occurence. When the buried depth of fault exceeds a critical value
the surface dislocation caused by earthquake can be neglected. The survey data shows that the top of main fault of the site is 15 m below the base of lock chambers
therefore the possibility of surface dislocation and its influence on ship locks are relatively little.In the further analysis and evaluation of the risk of site fault activity effects
the elaspse rate and activity (in terms of average rate and seismic period) of fault and the seismic fragility of geological factors are taken into account. The formula for evaluating the risk of site fault activity effects is given as follows:HD = E×M/8 × [(x1+…+xn)/n]where HD is hazard degree of site fault activity effects
E is elapse rate of fault (ranging from 0 to 1)
M is the activity of fault represented in earthquake magnitude (M≥8)
.r
is the seismic fragility of geological factor represented in index of earthquake hazard (ranging from 0 to 1)
and n is the number of considered geological factors. HD ranges from 0 to 1
the larger the value of which is
the higher the risk of fault activity will be.Although the geological background of ship lock group and the global environment of the site are not favourable
it is found after the analysis of the mode of interaction among fault
site structure and ship lock group that the upper site soil layers connected the most closely with the ship lock have not been affected by main fault
which will ensure the ship lock running in safety. It is found after the synthetical analysis of the large amount of borehole data that there are stable silty clay and clay layers at the depth of 5. 5 m to 8. 5 m. It is suggested that the foundation of ship locks should lay on such layers
in order to obtain higher degree of safety.
宿迁新城区地质缺陷分析与基础类型探讨 [J]. 朱云鹤,周广如,赵建军. 岩土工程学报 . 2000(02)
发震断裂的安全距离规定简介──《建筑抗震设计规范》修订简介(五) [J]. 董津城. 工程抗震 . 1999(02)
活动断裂安全距离的研究 [J]. 汤淼鑫. 工程抗震 . 1999(01)
郯庐断裂带潍坊—嘉山段全新世活断层的活动方式与发震模式 [J]. 晁洪太,李家灵,崔昭文,赵清玉. 地震研究 . 1997(02)
唐山东矿区地震易损性分析 [J]. 王立功. 地震地质 . 1982(03)
城市环境岩土工程[M]. 南京大学出版社 , 罗国煜等编著, 2000
高层建筑基础分析与设计[M]. 中国建筑工业出版社 , 宰金珉,宰金璋著, 1993
活断层及其工程评价[M]. 地震出版社 , 李起彤 编著, 1991
中国活动断裂[M]. 地震出版社 , 中国地震学会地震地质专业委员会 编辑, 1982
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