Authors:L. Mendes, R. Abrigo, V. Ramos, and P. Pereira
of compatibility can be reached [ 5 , 14 – 17 ].
The aim of this work was to investigate the effect of PC with different melt flow rates and cobalt catalyst as modifier agents of thermal and rheologicalproperties of PET/PC reactive blending
Authors:J.C. Spada, L.D.F. Marczak, I.C. Tessaro, and N.S.M. Cardozo
, N. , Biasutti , M. , Venir , E. , Spaziani , M. & Marchesini , G. ( 2009 ): Effect of high-pressure homogenization on droplet size distribution and rheologicalproperties of ice cream mixes . J. Dairy Sci. , 92
Authors:Karina Ilona Hidas, Csaba Németh, Lien Phuong Le Nguyen, Anna Visy, Adrienn Tóth, László Friedrich, and Ildikó Csilla Nyulas-Zeke
freezing to determine which concentration is the most effective to reduce the gelation. The pH, colour, and rheologicalproperties of the samples were examined over the storage period. Materials and methods The methods and measurements in this work were
Authors:W. Ciesińska, J. Zieliński, and T. Brzozowska
Coal-tar pitch was modified by addition of polystyrene, poly(ethylene terephthalate), unsaturated polyester and coumarone-indene
resin. The optimum conditions for production of homogeneous binary pitch-polymer blends containing 10% w/w of the polymer were established. Softening points, contents of toluene and quinoline-insoluble matters and rheological properties
of the blends were determined. The yield of solid fraction in semi-coking the blends was also found. The effect of polymers
on the coal-tar pitch blend properties was evaluated. Some pitch-polymer blends were then carbonized to carbon sorbents used
for purification of water and wastewater.
Authors:L. L. A. Vermeersen, R. Riva, and R. Sabadini
The 3D quasi-static displacements during and following an earthquake provide a wealth of information on the internal structure and rheological properties of the Earth. If an earthquake occurs in a region that has shallow-viscosity zones inside the crust or at the top of the mantle (asthenosphere), then post-seismic displacements of the crust on the order of millimeters per year are possible. These can be detected by means of permanent GPS stations in the years following a faulting event. In this paper we systematically study the influence of viscoelastic simulation model restrictions on co- and post-seismic deformation. Examples include stratification of the Earth model, modeling of the seismic source, influence of compressibility, effects of position and viscosities of shallow low-viscosity layers. It will be shown that some of these model restrictions or assumptions can have non-negligible influences on the simulated 3D co- and post-seismic displacements.