XIU Zongxiang, LIU Baohua, XIE Qiuhong, LI Xishuang, LIU Chenguang, PEI Yanliang, ZHENG Yanpeng. Assessment of structural stability in Bohai Sea area based on AHP-GDM model[J]. Acta Oceanologica Sinica, 2013, 32(4): 41-48. doi: 10.1007/s13131-013-0297-1
Citation:
XIU Zongxiang, LIU Baohua, XIE Qiuhong, LI Xishuang, LIU Chenguang, PEI Yanliang, ZHENG Yanpeng. Assessment of structural stability in Bohai Sea area based on AHP-GDM model[J]. Acta Oceanologica Sinica, 2013, 32(4): 41-48. doi: 10.1007/s13131-013-0297-1
XIU Zongxiang, LIU Baohua, XIE Qiuhong, LI Xishuang, LIU Chenguang, PEI Yanliang, ZHENG Yanpeng. Assessment of structural stability in Bohai Sea area based on AHP-GDM model[J]. Acta Oceanologica Sinica, 2013, 32(4): 41-48. doi: 10.1007/s13131-013-0297-1
Citation:
XIU Zongxiang, LIU Baohua, XIE Qiuhong, LI Xishuang, LIU Chenguang, PEI Yanliang, ZHENG Yanpeng. Assessment of structural stability in Bohai Sea area based on AHP-GDM model[J]. Acta Oceanologica Sinica, 2013, 32(4): 41-48. doi: 10.1007/s13131-013-0297-1
The First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China;Key Laboratory of Marine Sedimentology and Environmental Geology, Qingdao 266061, China
The AHP-GDM model is used for the assessment of structural stability, with the Bohai Sea area as an example. In this model, the credit degree of each expert is calculated through the assessment matrix based on the similarity and diversity of vector. The comprehensive opinions of expert panel are quantitatively obtained by considering the effect of credit degree. According to the geological structural setting, the Bohai Sea is divided into twelve assessment zones of structural stability by non-uniform element method. The structural stability grade of each zone is obtained on the basis of the latest geophysical data, earthquake statistical data, and the information of fault activities, current stress field and crustal deformation. The results show that there are one relatively stable area, three relatively sub-stable areas, six relatively sub-unstable areas and two relatively unstable areas. The assessment results of non-uniform element method are very close with those of uniform grid method with size of 0.25° in longitude direction and 0.14° in latitude direction. However the workload of non-uniform element method is only 1/16 of the latter. Compared with traditional assessment methods of structural stability, a more objective and reliable assessment result can be obtained by combining non-uniform element method and AHP-GDM model.