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Movement Epenthesis Generation for Video Synthesis of Sign Language Chung-Hsien Wu 
Individuals with hearing/speech impairment generally have problems in communication skill learning. Since deaf people have difficulty in speaking, many communication-aided approaches, such as sign language, finger spelling, lip-reading, and ...read more... |
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Thermal Induced SiC Nanoparticles Formation from Si/C/Si Multilayer Deposited by Ion Beam Sputtering Chen-Kuei Chung 
Nanoparticles have been widely studied in the fabrication and characterization because of their specific properties for quantum confinement effects and the promising application. ...read more... |
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Designing a molecularly imprinted polymer as an artificial receptor for the specific recognition of creatinine in serums Mei-Jywan Syu 
In this study, molecularly imprinted polymers (MIP) synthesized from two different functional monomers, β-cyclodextrin (β-CD) and 4-vinylpyridine (4-Vpy), were prepared. ...read more... |
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A mathematical programming method for formulating a fuzzy regression model based on distance criterion Liang-Hsuan Chen 
In the real world, often human estimation is influential in the decision-making processes, and the data provided will be fuzzy in nature. Therefore, instead of the traditional statistical regression analysis, various fuzzy regression models are presented in both applications and methodologies. ...read more... |
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Efficient reactivation of latent herpes simplex virus from mouse central nervous system SH Chen 
Herpes simplex virus (HSV) infects approximately 90% of the world’s population. After infection, two distinct lifecycles can be distinguished. First is a productive phase of 1 to 2 weeks, ...read more... |
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Coseismic source model of the 2003 Mw 6.8 Chengkung earthquake, Taiwan, determined from GPS measurements Ruey-Juin Rau 
Earthquake creates seismic waves and is the result of a sudden release of stored energy along the fault plane. On the contrary, creep (or aseismic slip) is a different type of fault motion, which is characterized by a slow, more or less continuous motion occurring on faults due to ongoing tectonic deformation. ...read more... |
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