scholarly journals 2A2-O04 High-Speed and High-Sensitiveity Sensor for Slip Detection : Examination of Slip Detection Mechanism(Tactile and Force Sensing (1))

2011 ◽  
Vol 2011 (0) ◽  
pp. _2A2-O04_1-_2A2-O04_4
Author(s):  
Seiichi Teshigawara ◽  
Ryuho Morita ◽  
Satoru Shimizu ◽  
Yosuke Suzuki ◽  
Aiguo Ming ◽  
...  
Author(s):  
Carsten Schürmann ◽  
Matthias Schöpfer ◽  
Robert Haschke ◽  
Helge Ritter

2012 ◽  
Vol 12 (9) ◽  
pp. 2910-2916 ◽  
Author(s):  
Yue H. Yin ◽  
Yong Xu ◽  
Zhen H. Jiang ◽  
Qian R. Wang
Keyword(s):  

2008 ◽  
Vol 2008 (0) ◽  
pp. _1A1-H11_1-_1A1-H11_2
Author(s):  
Seiichi Teshigawara ◽  
Tomohiro Nishinaga ◽  
Masatoshi Ishikawa ◽  
Makoto Shimojo

2011 ◽  
Vol 2011 (0) ◽  
pp. _2A2-O03_1-_2A2-O03_3
Author(s):  
Seiichi Teshigawara ◽  
Naoya Akimoto ◽  
Satoru Shimizu ◽  
Yosuke Suzuki ◽  
Aiguo Ming ◽  
...  

2021 ◽  
Vol 13 (12) ◽  
pp. 2281
Author(s):  
Yi-An Chen ◽  
Chung-Pai Chang ◽  
Wei-Chia Hung ◽  
Jiun-Yee Yen ◽  
Chih-Heng Lu ◽  
...  

Land subsidence is a significant problem around the world that can increase the risk of flooding, damage to infrastructure, and economic loss. Hence, the continual monitoring of subsidence is important for early detection, mechanism understanding, countermeasure implementation, and deformation prediction. In this study, we used multiple-sensor observations from the Continuous Global Positioning System (CGPS), the small baseline subset (SBAS) algorithm, interferometric synthetic-aperture radar (InSAR), precise leveling, multi-layer compaction monitoring wells (MLCWs), and groundwater observation wells (GWs) to show the spatial and temporal details of land subsidence in the Choushui River alluvial fan (CRAF), Taiwan, from 1993 to 2019. The results showed that significant land subsidence has occurred along the coastal areas in the CRAF, and most of the inland subsidence areas have also experienced higher subsidence rates (>30 mm/yr). The analysis of subsidence along the Taiwan High Speed Rail (THSR) revealed a newly formed subsidence center between Tuku and Yuanchang Townships in Yunlin, with high subsidence rates ranging from 30 to 70 mm/yr. We propose a map showing, for the first time, the distribution of deep compactions occurring below 300 m depth in the CRAF.


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