P
Phoebe Z. Ray
Researcher at University of New Orleans
Publications - 7
Citations - 595
Phoebe Z. Ray is an academic researcher from University of New Orleans. The author has contributed to research in topics: Singlet oxygen & Isomerization. The author has an hindex of 7, co-authored 7 publications receiving 458 citations.
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Journal ArticleDOI
Inorganic nano-adsorbents for the removal of heavy metals and arsenic: a review
Phoebe Z. Ray,Heather J. Shipley +1 more
TL;DR: In this paper, the applicability of inorganic adsorbents at the nanoscale is examined, including iron oxide (hematite, magnetite and maghemite), carbon nanotubes (CNT), and metal oxide based (Ti, Zn) and polymeric nanoadsorbents.
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Photolytic and photocatalytic degradation of surface oil from the Deepwater Horizon spill.
TL;DR: The photochemical behavior of Deepwater Horizon oil collected from the surface of the Gulf of Mexico was studied, and toxicity of the aqueous layer was altered in the presence of photocatalysts added to the oil film.
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Sunlight creates oxygenated species in water-soluble fractions of Deepwater Horizon oil.
TL;DR: The increased abundance of higher-order oxygen classes in the irradiated samples relative to the dark samples indicates that photooxidized components of the Macondo crude oil become water-soluble after irradiation.
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Petroleum films exposed to sunlight produce hydroxyl radical
Phoebe Z. Ray,Matthew A. Tarr +1 more
TL;DR: This study illustrates that oil is a strong and important source of hydroxyl radical when exposed to sunlight, and the fate of oil and other dissolved species following oil spills will be heavily dependent on the formation and fate of hydoxyl radical.
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Solar production of singlet oxygen from crude oil films on water
Phoebe Z. Ray,Matthew A. Tarr +1 more
TL;DR: In this article, the authors measured the production of singlet oxygen from thin oil films over seawater and pure water using furfuryl alcohol as a selective chemical probe and found that the formation rate of 6-hydroxy(2H)pyran-3(6H)-one was 1.9 −±−0.4 −5 and 1.6 −± −0.3 −5