Zobrazeno 1 - 10 of 62 pro vyhledávání: '"J. A. Kittrick"'
4
Illite equilibria in solutions: I. Phase relationships in the system K2OAl2O3SiO2H2O between 25 and 250°C
Autor: Philip E. Rosenberg, J. A. Kittrick, Stephen U. Aja
Publikováno v: Geochimica et Cosmochimica Acta. 55:1353-1364
Natural illite from Marblehead, Wisconsin (MH), USA, has been equilibrated with 0.2 and 2.0M KCl/KOH and KCl/HCl solutions in the presence of excess kaolinite or microcline and quartz or amorphous silica at temperatures between 25 and 250°C and Pv =
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::338d3cc28c1a1c3049c3575597c7c736
https://doi.org/10.1016/0016-7037(91)90313-t
Zobrazit plný text záznamu
6
The mechanism of Zn2+ adsorption on calcite
Autor: J. A. Kittrick, John M. Zachara, James B. Harsh
Publikováno v: Geochimica et Cosmochimica Acta. 52:2281-2291
The adsorption of Zn2+ on calcite (CaCO3(s)) was investigated from aqueous solutions in equilibrium with CaCO3(s) and undersaturated with respect to Zn5(OH)6(CO3)2(s)). Zinc adsorption occurred via exchange with Ca2+ in a surface-adsorbed layer on ca
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::de0526e5b7f1b2bc54774cd5c6c70d72
https://doi.org/10.1016/0016-7037(88)90130-5
Zobrazit plný text záznamu
7
Chemical Partitioning of Cadmium, Copper, Nickel and Zinc in Soils and Sediments Containing High Levels of Heavy Metals
Autor: J. A. Kittrick, M. G. Hickey
Publikováno v: Journal of Environmental Quality. 13:372-376
Partage chimique de Cd, Cu, Ni et Zn dans 3 sols et un sediment ayant precedemment recu des additions massives de metaux lourds
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::81daaeb6c6211df8147c160329dd046f
https://doi.org/10.2134/jeq1984.00472425001300030010x
Zobrazit plný text záznamu
9
Stability diagram of CaNaK-plagioclase with authigenic minerals
Autor: J. A. Kittrick, Hinrich L. Bohn
Publikováno v: Chemical Geology. 43:181-186
Conventional stability diagrams are limited essentially to the equilibria of aqueous solutions with pure end-member minerals. These diagrams extend to natural minerals containing isomorphous ion substitutes and to solid solutions if moles of ion char
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::48bc5cd3e94f9c978ed311e84cc66a94
https://doi.org/10.1016/0009-2541(84)90147-5
Zobrazit plný text záznamu

Vyhledávací nástroje:

Upřesnit hledání

Omezení vyhledávání
Plný text Recenzováno Digitální knihovna AV ČR
Zdroje