Comparative analysis and transformation relations between China and the US site classification systems in building seismic code provisions
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摘要: 本文依据分布于全国的6 824个钻孔数据,按照双参数的不同取值,将GB50011—2010《建筑抗震设计规范》(以下简称中国建抗规)的场地类别进一步划分为更加同质的子类,分析了双参数体系对场地分类结果的影响,建立了每个子类与美国《NEHRP对新建建筑和结构物的推荐地震条款》(National Earthquake Hazards Reduction Program Recommended Provisions for Seismic Regulations for New Buildings and Other Structures,以下简称美国建抗规)的场地类别的对应关系,并对比分析中、美建抗规的场地类别差异,在此基础上建立了中国建抗规与美国建抗规场地类别相互转换的概率表达。研究结果表明:用vS20近似表示中国场地分类标准的等效剪切波速并不可靠;中国建抗规中Ⅱ类场地和Ⅲ类场地内部不同子类与美国建抗规中场地类别的对应关系截然不同;中国建抗规中覆盖层厚度有效地区分了浅部波速类似而深部波速不同的场地;中国建抗规的Ⅱ类和Ⅲ类场地主体均对应美国建抗规的D类场地,中国Ⅱ类场地略偏对应美国C类场地,中国Ⅲ类场地略偏对应美国E类场地;中国Ⅳ类场地对应美国E类场地,绝大多数美国C类和D类场地均对应中国Ⅱ类场地,说明中国Ⅱ类场地的范围极宽。Abstract: In this study, based on 6 824 borehole profiles, we subdivide the site classes in GB 50011-2010 Code for Seismic Design of Buildings (Chinese code) into more homogeneous sub-classes by different values of the equivalent shear wave velocity (vSe) and site overlaying layers (D), and quantitatively analysis the effect of each parameters in the site classification schedule in the code. We build the relation between these sub-classes of the China code and classes of the US seismic design code National Earthquake Hazards Reduction Program Recommended Provisions for Seismic Regulations for New Buildings and Other Structures, carry out comparative analysis on two classification schedules, and build the probabilistic transformation relations for interconverting China site classes and the US site classes. The results show that: It is not appropriate to take the average shear wave velocity to a depth of 20 m (vS20) as the proxy for vSe in site classification of China code; for China site class Ⅱ and Ⅲ, different sub-classes have significantly different corresponding relations with the US site classes; the D effectively distinguishes the sites those velocity structures are similar at shallow layers while different at deeper layers; the main part of China site class Ⅱ and Ⅲ are both corresponding to the US site class D, the China site class Ⅱ leans to the US site class C, while the China site class Ⅲ leans to the US site class E; China site class Ⅳ is corresponding to the US site class E; most of the US site class C and D are both corresponding to China site class Ⅱ.It implies that the range of China site class Ⅱ is relatively vast.
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本目录中的地震参数来自“中国地震台站观测报告”(简称“月报”). 其中, 国内及邻区给出M≥4.7的事件, 全球给出M≥6.0的事件.“月报”由中国地震台网中心按月做出.
本目录中的发震时刻采用协调世界时(UTC); 为了方便中国读者, 也给出北京时(BTC). 震中位置除给出经纬度外, 还给出参考地区名, 它仅用作查阅参考, 不包含任何政治意义; 还给出测定震源位置的台数(n)和标准偏差(SD).
面波震级MS是用中周期宽频带SK地震仪记录, 采用北京台1965年面波震级公式MS=lg(AH/T)+1.66 lg(Δ)+3.5(1°<Δ<130°)求得. AH是两水平分向最大面波位移的矢量合成位移. MS7是对763长周期地震仪记录, 采用国际上推荐的面波震级公式MS7=lg(AV/T)+1.66 lg(Δ)+3.3(20°<Δ<160°)求得. AV是垂直向面波最大地动位移. mb是短周期体波震级, ML是近震震级. 为避免混乱, 震级之间一律不换算.为方便读者,还给出美国NEIC定出的面波震级MSZ和短周期体波震级mb.
中国及邻区地震目录(2014年11—12月, M≥4.7)Catalog of earthquakes within and near China (November-December, 2014, M≥4.7)编号 发震时刻 地理坐标 深度/km 震级 标准偏差(SD) 使用台数(n) 地区 UTC BTC 日-时 纬度/°N 经度/°E MS MS7 ML mb MSZmb
(NEIC)月-日 时:分:秒 1 11-14 01:24:16.8 14-09 42.10 77.45 10 5.5 5.3 5.7 5.2 2.3 88 吉尔吉斯斯坦—新疆边境地区 2 14 23:03:16.2 15-07 37.12 103.74 9 4.9 4.7 4.8 4.7 2.4 65 甘肃省 3 19 01:56:48.0 19-09 42.78 105.43 3 4.7 4.4 5.1 4.7 2.7 61 蒙古 4 19 03:05:45.9 19-11 42.84 105.44 5 4.5 4.3 5.0 4.6 2.4 62 蒙古 5 19 17:46:21.4 20-01 24.95 122.05 10 5.4 5.2 5.4 4.9 1.6 91 台湾岛 6 21 03:29:08.6 21-11 20.55 120.10 10 5.9 5.7 5.2 2.1 101 菲律宾群岛地区 7 22 08:55:28.0 22-16 30.29 101.68 20 6.4 6.4 6.1 5.6 2.4 100 四川省 8 25 15:19:09.6 25-23 30.20 101.75 16 5.9 5.8 5.8 5.4 2.6 101 四川省 9 12-05 18:43:45.2 06-02 23.32 100.49 10 5.9 5.7 6.0 5.0 1.9 86 缅甸—中国边境地区 10 06 10:20:00.8 06-18 23.33 100.50 10 5.9 5.6 6.0 5.3 2.3 95 缅甸—中国边境地区 11 07 09:23:07.0 07-17 23.30 100.51 16 4.8 4.6 4.8 4.5 2.3 53 缅甸—中国边境地区 12 10 20:28:04.0 11-04 20.14 120.44 20 4.8 4.8 4.9 5.0 2.1 75 菲律宾群岛地区 13 10 21:03:38.1 11-05 25.45 122.40 260 6.1 1.7 98 台湾岛 14 18 15:32:08.4 18-23 27.77 86.47 14 4.8 4.6 4.8 1.5 73 尼泊尔 15 31 07:54:34.0 31-15 24.59 122.63 50 4.4 4.1 4.6 4.9 2.9 78 台湾地区 全球地震目录(2014年11—12月, M≥6.0)Catalog of earthquakes all over the world (November-December, 2014, M≥6.0)编号 发震时刻 地理坐标 深度/km 震级 标准偏差(SD) 使用台数(n) 地区 UTC BTC 日-时 纬度/°N 经度/°E MS MS7 mb MSZmb
(NEIC)月-日 时:分:秒 1 11-01 18:57:21.5 02-02 19.36S 177.46W 433 6.0 0.7 100 斐济地区 2 03 08:23:54.0 03-16 4.80N 32.80W 5 6.6 6.4 1.9 15 中大西洋中部海岭 3 03 08:48:28.0 03-16 41.72S 79.73E 11 6.4 6.2 5.3 1.2 83 中印度洋海丘 4 07 03:33:55.1 07-11 5.95S 148.25E 50 6.2 6.1 6.0 2.2 101 新几内亚东部地区 5 15 02:31:39.4 15-10 1.95N 126.55E 40 7.0 6.9 6.5 1.0 100 马鲁古海峡 6 15 03:07:59.2 15-11 0.58S 124.26E 88 5.7 5.6 6.0 1.1 86 苏拉威西(西里伯斯)岛 7 16 22:33:23.1 17-06 37.45S 179.50E 30 6.6 6.5 5.8 1.6 93 新西兰北岛东海岸远海 8 17 16:52:47.2 18-00 46.45S 33.70E 10 6.0 5.7 5.5 2.7 44 爱得华太子群岛地区 9 21 10:10:19.2 21-18 2.30N 127.15E 40 6.5 6.2 6.3 1.5 102 马鲁古海峡 10 22 08:55:28.0 22-16 30.29N 101.68E 20 6.4 6.4 5.6 2.4 100 四川省 11 22 13:08:17.1 22-21 36.55N 137.85E 10 6.8 6.5 5.5 1.8 104 本州岛 12 26 14:33:44.0 26-22 2.00N 126.45E 50 6.7 6.6 6.3 1.1 100 马鲁古海峡 13 12-02 05:11:31.4 02-13 6.15N 123.15E 620 6.1 1.7 97 西里伯斯海 14 06 17:21:52.0 07-01 8.00N 82.70W 34 6.2 5.9 2.0 77 哥斯达黎加海岸远海 15 06 22:05:08.1 07-06 6.15S 130.80E 120 6.0 0.9 100 班达海 16 07 01:22:01.0 07-09 6.45S 154.45E 20 6.6 6.5 5.9 1.9 101 新不列颠地区 17 07 12:11:34.0 07-20 13.80N 91.40W 40 6.0 5.7 1.5 56 危地马拉海岸近海 18 07 21:16:37.0 08-05 13.80N 91.30W 30 6.2 5.9 1.8 58 危地马拉海岸近海 19 08 08:54:52.1 08-16 8.00N 82.70W 10 6.9 6.8 2.4 81 哥斯达黎加海岸远海 20 10 21:03:38.1 11-05 25.45N 122.40E 260 6.1 1.7 98 台湾岛 21 17 06:10:07.0 17-14 3.70S 100.40E 10 6.5 6.4 5.5 1.6 98 苏门答腊西南以远地区 22 21 11:34:12.7 21-19 2.25N 126.80E 50 6.2 6.2 5.9 1.3 100 马鲁古海峡 23 26 23:52:15.0 27-07 6.60N 82.40W 10 6.0 5.8 2.6 40 巴拿马以南地区 24 29 09:29:39.3 29-17 8.60N 121.50E 40 6.3 6.0 5.7 1.2 101 棉兰老岛 -
图 2 6 824个钻孔的各子类的D-vse分布
括号前的编号为本文定义的子类编码,括号内的数字为钻孔落在这个子类中的数量,vSe在500 m/s以上的部分为地面表层波速vS
Figure 2. 6 824 boreholes plotted on the D-vSe graph
The codes at left of the parentheses are the sub-classes codes defined in this article, The numbers in the parentheses are the numbers of boreholes belonged to these sub-classes,the ordinate value exceed 500 m/s represents instantaneous velocity at the surface layer instead of vSe
表 1 美国建抗规的场地分类(除F类外)
Table 1 Site classification in the US NEHRP provisions (without class F)
场地类别 VS30/(m·s−1) A >1500 B (760,1500] C (360,760] D (180,360] E ≤180 表 2 GB50011—2010《建筑抗震设计规范》场地子类划分标准表
Table 2 Sub-site classification schedule of the GB 50011—2010 Code for Seismic Design of Building
Vse/(m·s−1) Ⅰ 0 Ⅰ 1 Ⅱ Ⅲ Ⅳ Ⅰ 1b Ⅰ 1c Ⅰ 1d Ⅰ 1e Ⅱ c1 Ⅱ c2 Ⅱ d1 Ⅱ d2 Ⅱ e Ⅲ d Ⅲ e1 Ⅲ e2 ≤150 D<3 D∈ [3,15] D∈ [15,20) D∈ [20,80) D> 80 (150,250] D<3 D∈ [3,20) D∈ [20,50] D>50 (250,500] D<5 D∈ [5,20) D≥20 (500,800] D=0 >800 D=0 注:D为覆盖层厚度,单位m。 表 3 Dai等(2013)的外推模型在5 m,10 m和15 m深度位置的回归系数和均方根误差
Table 3 The coefficients and RMSEs of extrapolation model (Dai et al,2013) at depth of 5 m,10 m,and 15 m
深度
d/m回归系数 RMSE a b 5 0.728 0.737 0.061 10 0.784 0.707 0.042 15 0.616 0.774 0.027 表 4 中国建抗规的场地子类与美国建抗规范场地类别的对应关系
Table 4 The relation between sub-classes in the Chinese code for seismic design of building and classes in the US NEHRP code
场地子类 子类
孔数子孔
占比vS30
孔数A类场地 B类场地 C类场地 D类场地 E类场地 总比例 备注* 孔数 比例 孔数 比例 孔数 比例 孔数 比例 孔数 比例 Ⅰ 0 7 0.10% 6 0 0 6 100% 0 0 0 0 0 0 100% 2,15 m;4,10 m Ⅰ 1b 10 0.15% 0 0 0 0 50.0% 0 50.0% 0 0 0 0 100% 无VS30 Ⅰ 1c 107 1.57% 27 0 0 5 18.5% 22 81.5% 0 0 0 0 100% 23,15 m Ⅰ 1d 46 0.67% 6 0 0 1 16.7% 5 83.3% 0 0 0 0 100% 4,15 m Ⅰ 1e 6 0.09% 3 0 0 1 33.3% 2 66.7% 0 0 0 0 100% 3,5 m Ⅱ c1 1415 20.7% 98 0 0 0 0 87 88.8% 11 11.2% 0 0 100% 实测VS30 Ⅱ c2 1790 26.2% 972 0 0 0 0 111 11.4% 861 88.6% 0 0 100% 实测VS30 Ⅱ d1 880 12.9% 52 0 0 0 0 24 46.2% 28 53.8% 0 0 100% 实测VS30 Ⅱ d2 1180 17.3% 907 0 0 0 0 0 0 869 95.8% 38 4.2% 100% 实测VS30 Ⅱ e 58 0.85% 30 0 0 0 0 1 3.3% 29 96.7% 0 0 100% 25,15 m Ⅲ d 838 12.3% 838 0 0 0 0 0 0 758 90.4% 80 9.6% 100% 实测VS30 Ⅲ e1 19 0.28% 14 0 0 0 0 0 0 14 100% 0 0 100% 13,15 m Ⅲ e2 272 3.99% 257 0 0 0 0 0 0 3 1.17% 254 98.8% 100% 实测VS30 Ⅳ 196 2.87% 196 0 0 0 0 0 0 0 0 196 100% 100% 实测VS30 全部分类 6824 100% 3406 0 13 252 2573 568 100% 注:备注中数字表示中国建抗规场地子类钻孔应用浅孔估计的vS30数据,逗号前的数字表示采用了估计值的钻孔数,逗号之后的数字表示应用的浅孔最小孔深,为了保证结果的可靠性,只有当估计vS30的上下两倍均方根误差均落在美国建抗规同一场地类别时,此vS30和相应的场地类别才会被采用。 表 5 中国建抗规场地类别与美国建抗规场地类别的换算关系
Table 5 The transformation table for converting Chinese code for seismic design of building site classes to the US NEHRP code site classes
中国场地分类 美国场地分类 A B C D E Ⅰ 0 100.00% Ⅰ 1 20.40% 79.60% Ⅱ 35.11% 63.97% 0.93% Ⅲ 69.10% 30.90% Ⅳ 100.00% 表 6 美国建抗规场地类别与中国建抗规场地子类的换算关系
Table 6 The relation between classes in the US NEHPR code and sub-classes in the Chinese code for seismic design of building
美国场地分类 中国场地分类 Ⅰ 0 Ⅰ 1b Ⅰ 1c Ⅰ 1d Ⅰ 1e Ⅱ c1 Ⅱ c2 Ⅱ d1 Ⅱ e Ⅱ d2 Ⅲ d Ⅲ e1 Ⅲ e2 Ⅳ B 16.9% 12.0% 47.8% 18.5% 4.8% C 0.3% 4.3% 1.9% 0.2% 62.7% 10.2% 20.3% 0.1% D 3.8% 37.9% 11.3% 1.3% 27.0% 18.1% 0.5% 0.1% E 8.3% 13.5% 45.2% 33.0% 表 7 美国建抗规场地类别与中国建抗规场地类别的换算关系
Table 7 The transformation table for converting the US NEHPR code site classes to Chinese code site classes
美国场地
分类中国场地分类 Ⅰ 0 Ⅰ 1 Ⅱ Ⅲ Ⅳ B 16.88% 83.13% C 6.72% 93.28% D 81.36% 18.64% E 8.32% 58.70% 32.98% -
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