F
François M. M. Morel
Researcher at Princeton University
Publications - 267
Citations - 42608
François M. M. Morel is an academic researcher from Princeton University. The author has contributed to research in topics: Thalassiosira weissflogii & Carbonic anhydrase. The author has an hindex of 110, co-authored 267 publications receiving 40180 citations. Previous affiliations of François M. M. Morel include The New School & California Institute of Technology.
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Book
Surface Complexation Modeling: Hydrous Ferric Oxide
TL;DR: In this article, the generalized two-layer model is used to analyze the Coulombic effect of Hydrous Ferric Oxide, and anion and cation sorsption on HFOs are investigated.
Book
Principles and Applications of Aquatic Chemistry
TL;DR: The authors presents aquatic chemistry in a way that is truly useful to those with diverse backgrounds in the sciences Major improvements to this edition include a complete rewrite of the first three background chapters making them user-friendly.
Journal ArticleDOI
The chemical cycle and bioaccumulation of mercury
TL;DR: In this article, the methylmercury concentration in water is determined by the relative efficiency of the methylation and demethylation processes, and it is shown that anoxic waters and sediments are an important source of methylcury, apparently due to the methylating activity of sulfatereducing bacteria.
Journal ArticleDOI
Reduced calcification of marine plankton in response to increased atmospheric CO2.
Ulf Riebesell,Ingrid Zondervan,Björn Rost,Philippe D. Tortell,Richard E. Zeebe,Richard E. Zeebe,François M. M. Morel +6 more
TL;DR: It is suggested that the progressive increase in atmospheric CO2 concentrations may slow down the production of calcium carbonate in the surface ocean, as the process of calcification releases CO2 to the atmosphere.
Journal ArticleDOI
The biogeochemical cycling of elemental mercury: Anthropogenic influences☆
TL;DR: A review of the available information on global Hg cycling shows that the atmosphere and surface ocean are in rapid equilibrium; the evasion of Hg0 from the oceans is balanced by the total oceanic deposition of hg(II) from the atmosphere as mentioned in this paper.