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Dou Jie Yunus Ali P. Xu Yueren Zhu Zhongfan Chen Chi-Wen Sahana Mehebub Khosravi Khabat Yang Yong Pham Binh Thai 《Natural Hazards》2019,97(2):579-609
Natural Hazards - This study investigated the characteristics of rainfall-triggered landslides during the Typhoon Bilis in the Dongjiang Reservoir Watershed, China. The comparative shallow... 相似文献
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Characterization of liquefaction resistance in gravelly soil: large hammer penetration test and shear wave velocity approach 总被引：2，自引：0，他引：2
Ping-Sien Lin Chi-Wen Chang Wen-Jong Chang 《Soil Dynamics and Earthquake Engineering》2004,24(9-10):675
Gravelly soil is generally recognized to have no liquefaction potential. However, liquefaction cases were reported in central Taiwan in the 1999 Chi-Chi Taiwan earthquake and in the 1988 Armenia earthquake. Thus, further studies on the liquefaction potential of gravelly soil are warranted. Because large particles can impede the penetration of both standard penetration test and cone penetration test, shear wave velocity-based correlations and large hammer penetration tests (LPT) are employed to evaluate the liquefaction resistance of gravelly soils. A liquefied gravelly deposit site during the Chi-Chi earthquake was selected for this research. In situ physical properties of soil deposits were collected from exploratory trenches. Instrumented LPT and shear wave velocity (Vs) measurements were performed to evaluate the liquefaction resistance. In addition, large-scale cyclic triaxial tests on remolded gravelly soil samples (15 cm in diameter, 30 cm in height) were conducted to verify and improve LPT-based and Vs-based correlations. The results show that the LPT and shear wave velocity methods are reasonably suitable for liquefaction assessment of gravelly soils. 相似文献
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This study applied the soil water index (SWI), which can represent the conceptual soil water contents as influenced by present and antecedent rainfall, for analyzing rainfall-induced mass movements in Taiwan. The SWI has been used in Japan for nationwide mass movement warnings. This study examined whether the SWI can be also applied to Taiwan, which has a climatic condition and high-relief topography similar to Japan. We used data for mass movements for 2006–2012 (n = 263) for the main analyses and those for 2013 (n = 19) for verification. The SWI values before the rainfall events that triggered mass movements were used as the indicator of the antecedent rainfall condition. We found that when SWI values before rainfall events increased from <17.5 to >35, the upper threshold of rainfall conditions needed for triggering mass movements significantly decreased. The mass movements in 2013 support this finding. We classified rainfall conditions for triggering mass movements into two types, short duration–high intensity (SH) and long duration–low intensity (LL), based on a principal component analysis (PCA). The SH type is associated with a rapid increase in SWI, and the LL type is associated with a gradual rise and subsequent constancy of SWI except in some extremely long rainfall events. Based on this result, we modeled the general trend of the time series changes in SWI for the two types, which was verified using the mass movements in 2013. 相似文献
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Chi-Wen Chen Hongey Chen Lun-Wei Wei Guan-Wei Lin Tomoyuki Iida Ryuji Yamada 《Landslides》2017,14(5):1793-1801
This study analyzed 267 landslide landforms (LLs) in the Kumamoto area of Japan from the database of about 0.4 million LLs for the whole of Japan identified from aerial photos by the National Research Institute for Earth Science and Disaster Resilience of Japan (NIED). Each LL in the inventory is composed of a scarp and a moving mass. Since landslides are prone to reactivation, it is important to evaluate the sliding-recurrence susceptibility of LLs. One possible approach to evaluate the susceptibility of LLs is slope stability analysis. A previous study found a good correlation (R 2 = 0.99) between the safety factor (F s ) and slope angle (α) of F s = 17.3α ?0.843. We applied the equation to the analysis of F s for 267 LLs in the area affected by the 2016 Kumamoto earthquake (M j = 7.3). The F s was calculated for the following three cases of failure: scarps only, moving mass only, and scarps and moving mass together. Verification with the 2016 Kumamoto earthquake event shows that the most appropriate method for the evaluation of LLs is to consider the failure of scarps and moving mass together. In addition, by analyzing the relationship between the factors of slope of entire landslide and slope of scarp for LLs and comparing the results with the Aso-ohashi landslide, the largest landslide caused by the 2016 Kumamoto earthquake, we also found that morphometric analysis of LLs is useful for forecasting the travel distance of future landslides. 相似文献
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Evaluating differences in spatial visual attention in wayfinding strategy when using 2D and 3D electronic maps 总被引：1，自引：0，他引：1
With the evolution of mapping technology, electronic maps are gradually evolving from traditional 2D formats, and increasingly using a 3D format to represent environmental features. However, these two types of spatial maps might produce different visual attention modes, leading to different spatial wayfinding (or searching) decisions. This study designs a search task for a spatial object to demonstrate whether different types of spatial maps indeed produce different visual attention and decision making. We use eye tracking technology to record the content of visual attention for 44 test subjects with normal eyesight when looking at 2D and 3D maps. The two types of maps have the same scope, but their contents differ in terms of composition, material, and visual observation angle. We use a t test statistical model to analyze differences in indices of eye movement, applying spatial autocorrelation to analyze the aggregation of fixation points and the strength of aggregation. The results show that aside from seek time, there are significant differences between 2D and 3D electronic maps in terms of fixation time and saccade amplitude. This study uses a spatial autocorrelation model to analyze the aggregation of the spatial distribution of fixation points. The results show that in the 2D electronic map the spatial clustering of fixation points occurs in a range of around 12° from the center, and is accompanied by a shorter viewing time and larger saccade amplitude. In the 3D electronic map, the spatial clustering of fixation points occurs in a range of around 9° from the center, and is accompanied by a longer viewing time and smaller saccadic amplitude. The two statistical tests shown above demonstrate that 2D and 3D electronic maps produce different viewing behaviors. The 2D electronic map is more likely to produce fast browsing behavior, which uses rapid eye movements to piece together preliminary information about the overall environment. This enables basic information about the environment to be obtained quickly, but at the cost of the level of detail of the information obtained. However, in the 3D electronic map, more focused browsing occurs. Longer fixations enable the user to gather detailed information from points of interest on the map, and thereby obtain more information about the environment (such as material, color, and depth) and determine the interaction between people and the environment. However, this mode requires a longer viewing time and greater use of directed attention, and therefore may not be conducive to use over a longer period of time. After summarizing the above research findings, the study suggests that future electronic maps can consider combining 2D and 3D modes to simultaneously display electronic map content. Such a mixed viewing mode can provide a more effective viewing interface for human–machine interaction in cyberspace. 相似文献
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