The pseudo-inverse for the calculation of the shift vector in equation (4.67) has been computed traditionally as J+= (J Jp1 J. Adding a certain number, the Marquardt parameter mp, to the diagonal elements of the square matrix J J prior to its inversion, has two consequences (a) it shortens the shift vector 8p and (b) it turns its direction towards steepest descent. The larger the Marquardt parameter, the larger is the effect. In matrix formulation, we can write ... [Pg.156]

Amount of aqueous Ca(OH)j added" Solubilization region Transformation to calcite k (X 10-6 s l)... [Pg.400]

J AD Ministr of Aircraft Production (Brit) 7 MDPC rsel mite- diiiitrcphcuo 3 crcsylitc (Fr expl contg PA,DNPh TNCi... [Pg.753]

Watson, R. T. Ozone Trends Panel Prather, M. J. Ad Hoc Theory Panel Kurylo, M. J. NASA Panel for Data Evaluation. Present State of the Knowledge of the Upper Atmosphere 1988 An Assessment Report National Aeronautics and Space Administration Washington, DC, 1988 NASA Reference Publication 1208. [Pg.192]

Kaltenecker-Commercon JM,Ward TC, Gungor A, McGrath JE (1994) Water resistance of poly(imide siloxane) adhesives diffusion coefficients by gravimetric sorption. J Ad hes 44 1,85... [Pg.102]

© 2019 chempedia.info