The porosity and flow characteristics of macroporous polymer monoliths that may be used to prepare separation media, flow-through reactors, catalysts, or supports for solid-phase chemistry can be controlled easily during their preparation. Key variables such as temperature, composition of the pore-forming solvent mixture, and content of cross-linking divinyl monomer allow the tuning of average pore size within a broad range spanning 2 orders of magnitude. The polymerization temperature, through its effects on the kinetics of polymerization, is a particularly effective means of control, allowing the preparation of macroporous polymers with different pore size distributions from a single composition of the polymerization mixture. The choice of pore-forming solvent is also important, larger pores being obtained in a poor solvent due to an earlier onset of phase separation. Increasing the proportion of the cross-linking agent present in the monomer mixture not only affects the composition of the final monoliths but also decreases their average pore size as a result of early formation of highly cross-linked globules with a reduced tendency to coalesce. The synergy of different effects has also been observed under specific polymerization conditions using two monomer pairs, styrene−divinylbenzene and glycidyl methacrylate−ethylene dimethacrylate polymerized in close molds. Mercury intrusion porosimetry measurements, inverse size exclusion chromatography, and back pressure measured at different flow rates with the macroporous monoliths were used for the characterization of the porous properties. A good correlation between pore size and flow resistance that follows the Hagen−Poiseuille equation used previously to describe flow through a straight tube has been found.
President Shamsher Prakash, respected Dr. Jai Krishna, ladies and gantlemen, I am grateful to the Indian Society of Earthquake Technology for providing me with this opportunity to present the rasults of some of the research I have conducted in collaboration with my graduate students. The subject I have chosen to present to you is the earthquake response of concrete gravity dams. This choice has been motivated by two factors. Firstly, the early impetus for my resaarch on dams was provided by an earthquake experience familiar to most of you-the earthquake that occurred in 1967 close to Koyna Dam near Poona, India. As you know, the dam was overstressed by the earthquake motions and was damaged to an alarming degree. This experience with the earthquake performance of Koyna Dam, which was designed by the best available procedure of the time, indicated that concrete gravity dams are not immune to earthquake damage as had commonly been presumed. This realization led to much interest in developing improved procedures for analysis, design and safety evaluation of concrete gravity dams. Secondly, India Is one of the few countries whare naw concrete dams are still being built, so this should be a topic of Interest to reaearchers and engineer. here, Bec.use arch dams are rare in India, this presentation Is restricted to concrete gravity dams.
Publicado originalmente en la revista Sociology of Sport Journal , 9-3 (septiembre, 1992). Traduccion libre de Cesar Del Piccolo, con colaboracion de Gerardo Fittipaldi.
Abstract A global network of long‐term carbon and water flux measurements has existed since the late 1990s. With its representative sampling of the terrestrial biosphere's climate and ecological spaces, this network is providing background information and direct measurements on how ecosystem metabolism responds to environmental and biological forcings and how they may be changing in a warmer world with more carbon dioxide. In this review, I explore how carbon and water fluxes of the world's ecosystem are responding to a suite of covarying environmental factors, like sunlight, temperature, soil moisture, and carbon dioxide. I also report on how coupled carbon and water fluxes are modulated by biological and ecological factors such as phenology and a suite of structural and functional properties. And, I investigate whether long‐term trends in carbon and water fluxes are emerging in various ecological and climate spaces and the degree to which they may be driven by physical and biological forcings. As a growing number of time series extend up to 20 years in duration, we are at the verge of capturing ecosystem scale trends in the breathing of a changing biosphere. Consequently, flux measurements need to continue to report on future conditions and responses and assess the efficacy of natural climate solutions.