PPT-1 Texture, Microstructure & Anisotropy

AD Rollett Vectors Matrices Rotations Axis Transformations Most of the material in these slides originated in lecture notes by Prof Brent Adams now emeritus at BYU Last revised 9 Nov 11. 2 Incontrovertible anisotropy waves should show a characteristic crisscross pattern in a common-shot gather as illustrated in Figure 4a (here for a homogeneous layer). On the common-depth gather the s vs. GZK . …. … heavy composition . vs. anisotropies. Martin Lemoine. Institut d’Astrophysique de Paris. CNRS, Université Pierre & Marie Curie. M. . Lemoine & E. Waxman, . arXiv:0907.1354. nments (outdoor environments and virtual environments). In Experiment 1 it was found that depth extents of up to 7 m are indeed perceptually compressed relative to frontal extents in an outdoor enviro The quality of dried food is affected by a number of factors including quality of raw material, initial microstructure, and drying conditions. The structure of the food materials goes through deformations due to the simultaneous effect of heat and mass transfer during the drying process. Shrinkage and changes in porosity, microstructure and appearance are some of the most remarkable features that directly influence overall product quality. Porosity and microstructure are the important material properties in relation to the quality attributes of dried foods. Fractal dimension (FD) is a quantitative approach of measuring surface, pore characteristics, and microstructural changes [1]. However, in the field of fractal analysis, there is a lack of research in developing relationship between porosity, shrinkage and microstructure of different solid food materials in different drying process and conditions [2-4]. Establishing a correlation between microstructure and porosity through fractal dimension during convective drying is the main objective of this work.. Pankaj Jain . I.I.T. Kanpur. Introduction. Universe is assumed to be homogeneous and isotropic at large distance scales. No preferred position or direction . . of the . Moment Tensor. :. M. ij . = M. ji. Now assume the earthquake is a pure double couple, that means there is . no net volume. change, which means . trace must be 0. .. M11 + M22 + M33 = 0. That means independent elements can be represented by 5 independent parameters: . Katherine McCaffrey. PhD Candidate, Fox-Kemper Research Group. Department of Atmospheric and Oceanic Sciences. Cooperative Institute for Research in Environmental Sciences. 1. Thank you to my advisor and collaborators:. Texture and its Effect on Anisotropic Properties. Tony (A.D.) Rollett, Carnegie Mellon Univ. .. Last revised. : . 12. th. . Jan. 2014. 2. Microstructure-Properties Relationships. Microstructure. Properties. Richard . Essery. Anna . Kontu. , Samuel Morin, Martin . Proksch. , Mel . Sandells. MicroSnow2 Workshop, Columbia MD, 13 – 15 July 2015. Uses of microstructure in snow models. Grain size, shape and surface area measures . Why linearized Einstein’s equations may be enough. Wilke. van der Schee. Universitat de Barcelona,. March 22, 2012. Work with Michał Heller, David Mateos and Diego Trancanelli, 1202.0981. Outline. 1 . , P.Krkotic. 2. , J. O’Callaghan. 3. , F. Perez. 2. , M. Pont. 2. , X. Granados. 1 . , S. Calatroni. 4. , M. Taborelli. 4 . and T. Puig. 1. 1 . Institut. de . Ciència. de Materials de Barcelona, CSIC, . nments outdoor environments and virtual environments In Experiment 1 it was found that depth extents of up to 7 m are indeed perceptually compressed relative to frontal extents in an outdoor environme From Mays, 2011, Ground and Surface Water Hydrology. Effective conductivity . that represents aggregate effect of flow through a layered system. Effective conductivity is . different. parallel to than perpendicular to the layers. A.D. (Tony) Rollett,. . S. R. Wilson. Rodrigues. . vectors. ,. unit . Quaternions. Last revised: . 2. nd. Jan. 2015. Briefly describe rotations/orientations. Introduce Rodrigues-Frank vectors. Introduce .