Titlebook: Natural Language Processing and Text Mining; Anne Kao,Stephen R. Poteet Book 2007 Springer-Verlag London 2007 Matching.Processing.Signatur

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Razvan C. Bunescu,Raymond J. Mooneyon and monitoring of non-structural components is discussed with reference to a real case study. Data from a permanent monitoring system are collected and manipulated to simulate the effect of damage. Such data are used to assess the anomaly detection performance of the system and validate the promi

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Eni Mustafaraj,Martin Hoof,Bernd Freisleben of the deformed shape without directly computing the curvature. Also, many of the methods proposed in literature have been validated only on numerical models, due to the scarce availability of experimental data recorded on damaged structures. Recently data recorded on benchmark structures have beco

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Chutima Boonthum,Irwin B. Levinstein,Danielle S. McNamaraecommended to building owners (e.g., following the . 6.7 1994 Northridge, Calif., earthquake, approximately 300 buildings were subjected to costly inspection of connections (FEMA 352)). Using real-time data-driven computation of drift ratios as the parametric indicator of structural deformation and

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Philip M. McCarthy,Stephen W. Briner,Vasile Rus,Danielle S. McNamarabeing monitored by the procedures described in this article. A typical system consists of sensors, a local and a remote processing system, a robust data server and several communications media. The system provides information such as maximum response values, instrumental intensity, acceleration, vel

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Mauritius A. R. Schmidtler,Jan W. Amtrupeys in the determination of the most important energy parameter of a seismic source, namely, the magnitude M,. The relationship between M, and the body wave magnitude fI1t, is routinely employed in identification of underground nuclear explosions. Surface waves of hundreds of earthquakes recorded ev

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Janez Brank,Marko Grobelnik,Dunja Mladeni?eys in the determination of the most important energy parameter of a seismic source, namely, the magnitude M,. The relationship between M, and the body wave magnitude fI1t, is routinely employed in identification of underground nuclear explosions. Surface waves of hundreds of earthquakes recorded ev

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moment rate density function, which are proportional to the fault displacements, are consequently not resolved by the observations. To invert the source time functions, the inverse Radon kernel must be modified to properly treat information near zero-frequency and to prevent incoherent high-frequen

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