Your new experience awaits. Try the new design now and help us make it even better

ORIGINAL RESEARCH article

Front. Earth Sci.

Sec. Solid Earth Geophysics

Volume 13 - 2025 | doi: 10.3389/feart.2025.1616895

Application of time-lapse seismic full waveform inversion method in the detection of karst cave grouting

Provisionally accepted
Jinglan  XingJinglan Xing1Xiaochuan  HanXiaochuan Han1Jinliang  BaiJinliang Bai2Yaohui  LiuYaohui Liu2*Lemin  LiuLemin Liu1Chuanqi  QuChuanqi Qu2Qinggang  LiQinggang Li1Ziming  LiZiming Li1
  • 1Shandong Expressway Infrastructure Construction Co., Ltd., Jinan, China
  • 2China University of Mining and Technology, Xuzhou, China

The final, formatted version of the article will be published soon.

Grouting is a widely used method for addressing the issue of karst caves in geotechnical engineering. However, the extent and reinforcement effectiveness of grout after injection remain unclear in practical applications. To evaluate the grouting effect in karst caves, time-lapse seismic full waveform inversion (FWI) was employed in a series of field tests in Guizhou Province. The FWI results indicate that the horizontal range of the cave extends from 15 m to 25 m, with a depth range of 6 m to 12 m. These findings are consistent with the drilling results, which show a burial depth of 6.2 m to 12.4 m. The experimental results demonstrate that FWI can accurately determine the location and size of karst caves. The dispersion energy image of surface waves provides valuable input for the initial FWI model. The karst cave was also detected after grouting, and a wave velocity difference map was obtained. The results suggest that time-lapse FWI is more effective than direct inversion in eliminating the influence of the surrounding environment and highlighting changes in the slurry. The solidification range of the slurry after the second grouting closely matches the shape of the karst cave, suggesting that the cave has been completely filled with slurry. This conclusion is further supported by the drilling and subsequent construction results. Additionally, a comparison of the S-wave and P-wave inversion results shows that S-waves velocity models are more accurate than P-wave ones. These findings provide valuable insights for grouting detection in practical engineering applications.

Keywords: Geotechnical engineering, Karst cave, Surface wave method, Time-lapsegeophysics, Full waveform inversion

Received: 23 Apr 2025; Accepted: 25 Aug 2025.

Copyright: © 2025 Xing, Han, Bai, Liu, Liu, Qu, Li and Li. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

* Correspondence: Yaohui Liu, China University of Mining and Technology, Xuzhou, China

Disclaimer: All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article or claim that may be made by its manufacturer is not guaranteed or endorsed by the publisher.