Browsing ELibrary by Author "Nagy K.L."
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Browsing ELibrary by Author "Nagy K.L."
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Bickmore B.R.; Rosso K.M.; Nagy K.L.; Cygan R.T.; Tadanier C.J. (2003)The atomic structure of dioctahedral 2:1 phyllosilicate edge surfaces was calculated using pseudopotential planewave density functional theory. Bulk structures of pyrophyllite and ferripyrophyllite were optimized using ...
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Fenter P.; Teng H.; Geissbuhler P.; Hanchar J.M.; Nagy K.L.; Sturchio N.C. (2000)In situ X-ray specular reflectivity and atomic force microscopy were used to determine the structure of the orthoclase (001) cleavage surface in contact with deionized water at 25°C. These are the first in situ measurements ...
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Nagy K.L.; Cygan R.T.; Hanchar J.M.; Sturchio N.C. (1999)New experimental data for gibbsite growth on powdered kaolinite and single crystal muscovite and published data for gibbsite growth on gibbsite powders at 80°C in pH3 solutions show that all growth rates obey the same ...
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Nagy K.L.; Lasaga A.C. (1993)Precipitation rates of kaolinite and gibbsite were measured in stirred-flow reactors with a mixed seed substrate of kaolinite plus gibbsite at 80°C and pH 3. Input solutions were supersaturated simultaneously to different ...
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Schlegel M.L.; Nagy K.L.; Fenter P.; Sturchio N.C. (2002)The structures of prismatic (100) and pyramidal (101) growth faces of natural quartz crystals, and their modification upon annealing at T =< 400°C were investigated ex situ by atomic force microscopy (AFM) and in water by ...
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Bickmore B.R.; Nagy K.L.; Gray A.K.; Brinkerhoff A.R. (2006)The influence of Al(OH)4- on the dissolution rate of quartz at pH 10-13 and 59-89 °C was determined using batch experiments. Al(OH)4- at concentrations below gibbsite solubility depressed the dissolution rate by as much ...
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