Thesis (Ph. D.)--School of Chemical and Biomolecular Engineering, Georgia Institute of Technology, 2005. Directed by Amyn S. Teja. / Dr. Thomas H. Sanders, Committee Member ; Dr. Peter J. Ludovice, Committee Member ; Dr. J. Carson Meredith, Committee Member ; Dr. William J. Koros, Committee Member ; Dr. Amyn S. Teja, Committee Chair. Includes bibliographical references.

Thesis (Ph. D.)--University of Nebraska, 1933. / Bibliography: p. 32.

Thesis (Ph. D.)--University of Wisconsin--Madison, 1921. / Typescript. With this is bound: The heat of coagulation of ferric oxide hydrosol with electrolytes / By Frederick Lincoln Browne and J. Howard Matthews. Reprinted from Journal of the American Chemical Society, vol. XLIII, no. 11 (Nov. 1921), p. [2336]-2352. Includes bibliographical references.

Thesis (M.S.)--University of California, Berkeley, 1963. / "UC-4 Chemistry" -t.p. "TID-4500 (18th Ed.)" -t.p. Includes bibliographical references (p. 45-46).

Thesis (Ph. D.)--University of Wisconsin--Madison, 1958. / Typescript. Vita. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references (leaves 240-244).

No description available.

The mechanism of emplacement of ultramafic intrusions has been a controversial subject for many years. This thesis summarizes evidence favoring the intrusion of ultramafic rocks as magmas. Experiments were conducted to study the effect on the melting behavior or ultramafic rocks of carbon dioxide, sodium, sulphur and water at temperatures up to 925°C. and pressures up to 2125 atmospheres. No melts were produced but it is felt that the evidence presented justifies further work on the problem. / Applied Science, Faculty of / Mining Engineering, Keevil Institute of / Graduate

Values of thermodynamic stability constants at 25°C for the complexes of serine with the metal ions. Co^2+, Ni^2+, Cd^2+, Zn^2+, and Cu^2+ were obtained from pH titration data. All measurements were made in aqueous solution, and data were obtained at three different ionic strengths for each metal ion studied. It was assumed that the activity of the zwitterion is unity. The effect of metal ion hydrolysis upon the log K values was taken into account for the calculations. For all the metal ions studied, stability constants for MA^+, MA_2, and MA_3^- were reported with the exception of copper (II) which formed only MA^+ and MA_2 complexes. The stabilities of the complexes studied follow the sequence: Cd^2+ < Co^2+ < Zn^2+ < Ni^2+ < Cu^2+. The value of log K for each step of metal serine interaction, in all cases, increases in the order. K_3 < K_2 < K_1. Under the conditions studied, it was assumed that the metal ion coordinates through the amino nitrogen and the carboxyl oxygen of the serine only. There was no evidence that the hydroxyl group of serine took part in coordination with the metal ions. All calculations of stability constants were carried out using an IBM 7040 computer.

No description available.

Thèse : Physique : Faculté des sciences de Paris : 1853. Thèse : Chimie : Faculté des sciences de Paris : 1853. / Titre provenant de l'écran-titre.