Volume 40 Issue 4
Aug.  2026
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WANG Peng, LIU Xiaolei, ZHANG Bofu, ZHOU Shichong, WANG Lei. Seismic effects of construction sites in Binhai New Area[J]. GEOTECHNICAL ENGINEERING TECHNIQUE, 2026, 40(4): 526-533. doi: 10.20265/j.cnki.issn.1007-2993.2025-0077
Citation: WANG Peng, LIU Xiaolei, ZHANG Bofu, ZHOU Shichong, WANG Lei. Seismic effects of construction sites in Binhai New Area[J]. GEOTECHNICAL ENGINEERING TECHNIQUE, 2026, 40(4): 526-533. doi: 10.20265/j.cnki.issn.1007-2993.2025-0077

Seismic effects of construction sites in Binhai New Area

doi: 10.20265/j.cnki.issn.1007-2993.2025-0077
  • Received Date: 2025-02-25
  • Accepted Date: 2025-06-26
  • Rev Recd Date: 2025-04-14
  • Available Online: 2026-08-07
  • Publish Date: 2026-08-08
  • Based on the analysis of the regional geological background of the Binhai New Area, this paper statistically analyzed the equivalent shear wave velocity of foundation soils and the site overburden thickness from more than a hundred projects in the Binhai New Area. It also classified the site categories of the Binhai New Area and provided the distribution range and ground motion parameters for different architectural sites. Furthermore, the paper conducted liquefaction determination for 3932 geotechnical investigation boreholes in the Binhai New Area. By integrating the actual spouting sand investigation points from seismic surveys and the distribution of non-liquefaction investigation boreholes in the Binhai New Area, the paper delineated the distribution range and liquefaction grade zoning of the liquefiable soil layers. The study results indicate: (1) The equivalent shear wave velocity of foundation soil above 20 m depth is generally 140.0~170.0 m/s, corresponding to soft to medium-soft soils. The site overburden thickness is mostly 90~100 m. (2) Most areas in the Binhai New Area are categorized as Class Ⅳ sites, with only the northern Binhai Tourism Area, the western Airport Economic Area, and the area west of Beidagang Reservoir classified as Class Ⅲ sites. (3) Liquefiable zones are primarily distributed in parts of Hangu, Tanggu, and Dagang, with moderate liquefaction areas mainly in the Dagang District, southern Hangu District, Junliangcheng, and near the Haihe River in Tanggu. Severe liquefaction areas are only distributed near the Sino-Singapore Tianjin Eco-City.

     

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