D-R model

Lichen biomass from Parmelina and Cladonia genera have resulted good biosorbents of Pb(II), Cr(III), and Ni(II) ions. The Langmuir, Freundlich, and Dubinin-Radushkevich (D-R) models... 

Topham, D.R. Modelling of hydrocarbon bubble plumes to include gas hydrate formation. Chem. 

Burnham, K.P., and Anderson, D.R. Model selection and multimodel inference A practical information-theoretic approach. Springer-Verlag, New York, 2002. 

Fomes, T. D. and Paul, D. R. Modeling properties of nylon 6/clay nanocomposites using composite theories. Polymer, 44,4993-5013 (2003). 

Wood, G O., "Review and Comparisons of D/R Models of Equilibrium Adsorption of Binary Mixtures of Organic Vapors on Activated Carbons," Carbon. 2002 40 231 239. 

Fournier R and Salahub D R 1990 Chemisorption and magnetization A bond order-rigid band model Surf. Sol. 238 330-40... 

MlynarskI P and Salahub D R 1991 Looal and nonlooal density funotlonal study of Nl and Nig olusters. Models for the ohemisorptlon of hydrogen on (111) and (100) niokel surfaoes J. Chem. Phys. 95 6050-6... 

Roohefort A, Andzelm J, Russo N and Salahub D R 1990 Chemisorption and diffusion of atomlo hydrogen In and on oluster models of Pd, Rh, and bimetalllo PdSn, RhSn, and RhZn oatalysts J. Am. Chem. Soo. 112 8239-47... 

Duarte H A and Salahub D R 1998 Embedded cluster model for chemisorption using density functional calculations oxygen adsorption on the AI(IOO) surface J. Chem. Phys. 108 743... 

N. E. Bowne, R. J. Londergan, R. J. Minott, D. R. Murray, "Preliminary Results from the EPRI Plume Model VaUdafion Project— Plains Site,"... 

Killus, J. P., Meyer, J. P., Durran, D. R., Anderson, G. E., Jerskey, T. N., and Whitten, G. Z., "Continued Research in Mesoscale Air Pollution Simulation Modeling," Vol. V, "Refinements in Numerical Analysis, Transport, Chemistry, and Pollutant Removal," Report No. ES77-142. Systems Applications, Inc., San Rafael, CA, 1977. 

McNeil, T.J., Weed, D.R. and Estrin, J., 1978. A note on modelling laboratory batch crystallizers. American Institution of Chemical Engineers Journal, 24(4), 728-731. 

For either experiment we can consider that irradiated protons to flip back and forth between their two spin-states so rapidly that they no longer couple with other protons in the same molecule. An alternative rationale can be couched in terms of the decoupling field equalizing the populations of the two energy levels of the irradiated protons, which is qualitatively equivalent to saturating that resonance. (Although neither of these two models is strictly correct, they do at least provide a simple rationale for the N.M.D.R. experiment.)... 

The model is supported by the fact that in the absence of magnesium bromide 4-methoxyben-zylmagnesium chloride reacts with nitrone 2 at 0°C in THF with an inverse diastereoselectivity [3a/3b d.r. (2R,35,4R)/(25,35,4R) 40 60]I6. 

Chittleborough, G. D., Treagust, D. R, Mocerino, M. (2002). Constraints to the development of first year university students mental models of chemical phenomena. Teaching and Learning Forum 2002, Focusing on the Student. Retrieved January 30, 2004, from http //www.ecu.edu.au/conferences/tlf/2002/pub/docs/Chittleborough.pdf. 

Grime, J.P. (1988). The C-S-R model of primary plant strategies - origins, implications and tests. In Plant Evolutionary Biology, ed. L.D. Gottlieb and K. Jain, pp. 371-93. London Chapman Hall. 

Ballal, D. R. and Lefebvre, A. H., A general model of spark ignition for gaseous and liquid fuel-air mixtures. 

Warna, J., Flores Geant, M., Salmi, T., Hamunen, A., Orte, J., Hartonen, R., and Murzin, D. (2006) Modelling and scale-up of sitosterol hydrogenation process from laboratory slurry reactor to plant scale. Ind. Eng. Chem. Res., 45, 7067-7076. 

Janecky, D.R. and Seyfried, W.E. Jr. (1984) Formation of massive sulfide deposits on oceanic ridge crests incremental reaction models for mixing between hydrothermal solutions and seawater. Geochint. Cosmochim. Acta, 48, 2723-2738. 

Janecky, D.R. and Shanks, W.C. Ill (1988) Computational modeling of chemical and sulfur isotopic reaction processes in seafloor hydrothermal systems, chimney, massive sulfides, and subjacent alteration zones. Can. Mineral, 26, 805—826. 

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