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Martin A.A. Schoonen

Researcher at Stony Brook University

Publications -  141
Citations -  11641

Martin A.A. Schoonen is an academic researcher from Stony Brook University. The author has contributed to research in topics: Pyrite & Aqueous solution. The author has an hindex of 50, co-authored 138 publications receiving 10503 citations. Previous affiliations of Martin A.A. Schoonen include Brookhaven College & State University of New York System.

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The absolute energy positions of conduction and valence bands of selected semiconducting minerals

TL;DR: In this article, the absolute energy positions of conduction and valence band edges were compiled for about 50 each semiconducting metal oxide and metal sulfide minerals, and the relationship between energy levels at mineral semiconductor-electrolyte interfaces and the activities of these minerals as a catalyst or photocatalyst in aqueous redox reactions were reviewed.
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The Structure of Ferrihydrite, a Nanocrystalline Material

TL;DR: Real-space fitting indicates structural relaxation with decreasing particle size and also suggests that second-order effects such as internal strain, stacking faults, and particle shape contribute to the PDFs.
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Reactions forming pyrite and marcasite from solution: II. Via FeS precursors below 100°C

TL;DR: In this paper, the formation of pyrite and marcasite from a FeS precursor has been examined experimentally and it was shown that pyrites and Marcasite formation proceed at a significant rate only if intermediate sulfur species (i.e., polysulfides, polythionates, or thiosulfate) are present in solution.
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Removal of dissolved oxygen from water: A comparison of four common techniques.

TL;DR: Four common techniques for the removal of dissolved oxygen from water have been examined: boiling at 1 atm, boiling under reduced pressure, purging with N(2) and sonication under reducing pressure.
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Reactions forming pyrite and marcasite from solution: I. Nucleation of FeS2 below 100°C

TL;DR: In this article, reaction paths for nucleation and growth of pyrite and marcasite from solution have been investigated experimentally, and conditions were chosen to avoid the precipitation of metastable Fe-S phases which can act as precursors for FeS2 formation.