中国地震
中國地震
중국지진
EARTHQUAKE RESEARCH IN CHINA
2009年
2期
140-150
,共11页
高孟潭%陈学良%肖和平%燕为民%欧阳承新%温增平
高孟潭%陳學良%肖和平%燕為民%歐暘承新%溫增平
고맹담%진학량%초화평%연위민%구양승신%온증평
湖南中强震区%Ⅱ类场地%场地效应%3个水准
湖南中彊震區%Ⅱ類場地%場地效應%3箇水準
호남중강진구%Ⅱ류장지%장지효응%3개수준
Hunan moderate earthquake area Type II site Site amplification effect Three levels
利用工程场地地震安全性评价工作中大量实际钻孔和土工实验资料,建立了实际工程场地模型,在50年超越概率为63%、10%、2%共3种地震动输入下,采用SHAKE91和ELSSRA两种等效线性化方法,研究了湖南省Ⅱ类场地土层的放大效应.计算结果表明:湖南省50年超越概率10%的场地效应放大因子为1.30,若使用<中国地震动参数区划图(GB18306-2001)>认定的1.25系数,将低估湖南中强地震活动地区的场地放大效应.湖南省50年超越概率63%、10%、2%这3个设定水准的场地效应放大因子满足1.10:1.00:0.95的关系.这些结果有益于为湖南省提供更为合理的抗震设防标准.
利用工程場地地震安全性評價工作中大量實際鑽孔和土工實驗資料,建立瞭實際工程場地模型,在50年超越概率為63%、10%、2%共3種地震動輸入下,採用SHAKE91和ELSSRA兩種等效線性化方法,研究瞭湖南省Ⅱ類場地土層的放大效應.計算結果錶明:湖南省50年超越概率10%的場地效應放大因子為1.30,若使用<中國地震動參數區劃圖(GB18306-2001)>認定的1.25繫數,將低估湖南中彊地震活動地區的場地放大效應.湖南省50年超越概率63%、10%、2%這3箇設定水準的場地效應放大因子滿足1.10:1.00:0.95的關繫.這些結果有益于為湖南省提供更為閤理的抗震設防標準.
이용공정장지지진안전성평개공작중대량실제찬공화토공실험자료,건립료실제공정장지모형,재50년초월개솔위63%、10%、2%공3충지진동수입하,채용SHAKE91화ELSSRA량충등효선성화방법,연구료호남성Ⅱ류장지토층적방대효응.계산결과표명:호남성50년초월개솔10%적장지효응방대인자위1.30,약사용<중국지진동삼수구화도(GB18306-2001)>인정적1.25계수,장저고호남중강지진활동지구적장지방대효응.호남성50년초월개솔63%、10%、2%저3개설정수준적장지효응방대인자만족1.10:1.00:0.95적관계.저사결과유익우위호남성제공경위합리적항진설방표준.
Real models of engineering site are constructed on the basis of the quantitative data of real boreholes and soil tests in Safety Assessment Work. Under 63.2%, 10% and 2% exceedance probability in 50 years, amplification effects of Type II sites in Hunan Province are studied in detail by 2 equivalent linear seismic response methods, SHAKE91 and ELSSRA respectively. The results indicate that the amplification effect of Type II sites in Hunan Province on condition of 10% exceedance probability in 50 years is 1.30 against the previous coefficient 1.25 in National Standard "The Zonation Map of Earthquake Ground Motion Parameters in China (GB18306-2001)", which will underestimate site effects in moderate earthquake areas such as Hunan. 63.2%, 10% and 2% exceedance probability in 50 years in terms of amplification effects of Type II sites in Hunan accord with the relations at the levels of 1.10:1.00:0.95. All these results are helpful for more reasonable standards of engineering aseismic design in Hunan Province.