Journal of Jilin University(Earth Science Edition) ›› 2019, Vol. 49 ›› Issue (4): 1200-1208.doi: 10.13278/j.cnki.jjuese.20180250

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Comparison of 3D Geological Modeling Based on Two Different Interpolation Methods

Feng Bo1, Chen Mingtao1, Yue Dongdong2, Li Shengtao1,2, Jia Xiaofeng2, Song Dan1   

  1. 1. Key Laboratory of Groundwater Resources and Environment(Jilin University), Ministry of Education, Changchun 130021, China;
    2. Center for Hydrogeology and Environmental Geology, China Geological Survey, Baoding 071051, Hebei, China
  • Received:2018-09-27 Online:2019-07-26 Published:2019-07-26
  • Supported by:
    Supported by National Key Research and Development Plan Project (2018YFB1501802), Joint Project Between Jilin Province and Jilin University (SXGJSF2017-5), Project of China Geological Survey (DD20179621) and Project of Jilin Provincial Department of Education (JJKH20170807KJ)

Abstract: In the process of 3D geological modeling, interpolation algorithm has a significant influence on the accuracy of the model. In order to evaluate the influence of different interpolation algorithms on 3D modeling, the inverse distance weight interpolation and the natural neighborhood interpolation methods were selected to make a comparative study. Through theoretical analyses and case studies, these two methods were analyzed and compared in aspects of statistics, interpolation errors,and visualization. The results show that the inverse distance weight interpolation method has higher accuracy and wider adaptation area in modeling. Compared to the natural neighborhood interpolation method, the inverse distance weight interpolation method is, at first, more applicable to the area where some strata lack seriously, and can better retain characteristics of the lacked strata. Next,the method is able to handle fault structures and perform better for the fault fluctuation of strata. Finally, its result has a smaller error in sedimentary strata, and is closer to the actual situation.

Key words: 3D geological modeling, groundwater modeling system, the inverse distance weight interpolation method, natural neighborhood interpolation method

CLC Number: 

  • P628+.3
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