scispace - formally typeset
G

George A. Parks

Researcher at Stanford University

Publications -  75
Citations -  7895

George A. Parks is an academic researcher from Stanford University. The author has contributed to research in topics: X-ray absorption fine structure & Sorption. The author has an hindex of 46, co-authored 75 publications receiving 7597 citations. Previous affiliations of George A. Parks include United States Geological Survey.

Papers
More filters
Journal ArticleDOI

In Situ X-ray Absorption Study of Surface Complexes: Selenium Oxyanions on α-FeOOH

TL;DR: In this article, in situ extended x-ray absorption fine structure (EXAFS) measurements of adsorbed selenate and selenite ions at the α-FeOOH(goethite)-water interface have been performed; these measurements show that selenates forms a weakly bonded, outer-sphere complex and that Selenite forms a strongly bonded, inner-spheres complex.
Journal ArticleDOI

Quantitative arsenic speciation in mine tailings using X-ray absorption spectroscopy

TL;DR: X-ray absorption fine structure spectroscopy (XAFS) was used to determine arsenic (As) oxidation state, local coordination (to a radius of nearly equal Aa around As), and the relative proportion of different As species in model compounds and three California mine wastes as discussed by the authors.
Book ChapterDOI

Characterization of Aqueous Colloids by Their Electrical Double-Layer and Intrinsic Surface Chemical Properties

TL;DR: In this paper, the development of surface charge and potential, the zeta potential of the solid, the conductivity of the sol, electrolyte adsorption densities, and related properties are modeled.
Journal ArticleDOI

Silica Diagenesis, I. Solubility Controls

TL;DR: In this article, the diagenetic sequence of silica is examined in terms of several thermodynamic and kinetic concepts, and the relationship between solubility and surface area or particle size is explained.
Journal ArticleDOI

Dissolution kinetics of magnesium silicates

TL;DR: In this article, the parabolic exchange kinetics of surface magnesium ions with hydrogen ions were investigated and it was shown that the amount of silicon and magnesium dissolved is proportional to t and congruent.