Sunday, November 30, 2008
Fusion Nuclear
Thermonuclear fusion depends on high energies, and the possibility of low-energy, low-temperature nuclear fusion has generally been discounted. Early in 1989, however, two electrochemists started the scientific world and aroused great public interest when they declared that they had achieved room temperature fusion in a simple laboratory experiment. The scientist, Stanley Pons of the University of Utah and Martin fleischmann of the University of Southampton, England, described their experiment as involving an electrochemical cell in which palladium and platinum electrodes were immersed in heavy water. They claimed that the cell produced more heat than could be accounted for by a chemical reaction alone and that they had observed certain typical fusion by product in the course of the process. According to their theory, deuterium was absorbed by the palladium electrode and fused there, releasing the extra heat.
Various laboratories around the world tried to duplicate the process, with conflicting but generally negative results. Scientists nevertheless continued to explore this possibility of “cold fusion.”
Friday, November 14, 2008
Chemical Reactor
An industrial chemical reactor is a complex device in which heat transfer, mass transfer, diffusion, and friction may occur along with chemical reaction, and it must be safe and controllable. In large vessels, questions of mixing of reactants, flow distribution, residence time distribution, and efficient utilization of the surface of porous catalysts also arise. A particular process can be dominated by one of these factors or by several of them; for example, a reactor may on occasion be predominantly a heat exchanger or a mass-transfer device. A successful commercial unit is an economic balance of all these factors.
Monday, November 3, 2008
Sulfur
Sulfur or sulphur is a naturally occurring, yellow, water insoluble solid element. Its chemical symbol is S, its atomic number is 16 and its atomic weight is 32.064 sulfur is nonmetal and a member of the oxygen family of elements, which constitutes Group VIA of the periodic table. The discovery of sulfur predates recorded history, and the element has been used since ancient times. The early medical books of Dioscorides of Greece and Pliny the Elder mention sulfur, and fumes from burning sulfur were used in religious ceremonies and for fumigation. Alchemists recognized sulfur as a mineral substance that can be melted and burned. It was first classified as an element by Antonie Lavoisier in 1777.
On earth, sulfur is widely distributed in its elemental state as a secondary mineral or as a volcanic deposit, as well as in combination with a number of metals. Large sedimentary deposits of the almost pure element, mainly of Tertiary age, are found in the coastal regions of Texas and Lousiana, on the Isthmus of Tehuantepec, Mexico, and in Sicily, Sulfur occurs in some fossil fuels, most motably coal, in chemical combination with carbon and other elements, its removal is difficult. Sulfur is prevalent in the sulfide ores of iron (pyrite), zinc (sphalerite), and lead (galena). It also occurs as calcium sulfate (gypsum) and barium sulfate (barite). The magnesium and sodium sulfates are present in ocean water and in many mineral waters.

