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Published on: March 12, 2021
Variable-baseline disparity matching for 3D measurement and buried pipeline depth estimation
Ryota Tanabe1, Riko Okano2, Yuki Kominami2
1Degree Programs in Systems and Information Engineering, University of Tsukuba, Tsukuba, 305-8577, Japan. tanabe@cmu.iit.tsukuba.ac.jp.
This study introduces a fast, wide-area 3D ground mapping method using aerial images for disaster zones. It accurately estimates buried pipeline depth after earthquakes, overcoming limitations of current techniques.
Area of Science:
- Geomatics Engineering
- Geotechnical Engineering
- Remote Sensing
Background:
- Existing underground pipeline surveys are costly, time-consuming, and limited in scope.
- Accurate 3D ground surface data is crucial for post-earthquake infrastructure assessment.
- Monitoring buried pipelines before and after seismic events is challenging.
Purpose of the Study:
- To develop a rapid 3D ground surface measurement technique using aerial imagery.
- To estimate the depth of shallow buried pipelines post-earthquake.
- To overcome limitations of traditional underground pipeline detection methods.
Main Methods:
- Utilized disparity matching of two aerial images to create 3D ground surface maps.
- Developed a small-scale observation system to simulate seismic events and measure pipeline responses.
- Applied Random Forest Regression for estimating buried pipeline depth from 3D ground data.
Main Results:
- Achieved ground displacement measurement errors under 2 mm and ground height errors under 1 cm.
- Demonstrated fast, wide-area 3D mapping capability in simulated disaster-affected regions.
- Obtained a pipeline depth prediction error of less than 5 mm using regression analysis.
Conclusions:
- The proposed aerial imaging method offers an efficient solution for 3D ground mapping in disaster areas.
- The system enables unprecedented data acquisition for pre- and post-earthquake pipeline monitoring.
- This approach significantly improves the accuracy and efficiency of assessing buried infrastructure after seismic events.
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