Amanote Research
Register
Sign In
Discover open access scientific publications
Search, annotate, share and cite publications
Publications by Rafael Gonçalves-Araujo
The Influence of Dissolved Organic Matter on the Marine Production of Carbonyl Sulfide (OCS) and Carbon Disulfide (CS<sub>2</sub>) in the Eastern Tropical South Pacific
Related publications
Quantifying the Vertical Transport of CHBr<sub>3</sub> And CH<sub>2</sub>Br<sub>2</sub> Over the Western Pacific
Significant Production of ClNO<sub>2</sub> And Possible Source of Cl<sub>2</Sub> From N<sub>2</Sub>O<sub>5</Sub> Uptake at a Suburban Site in Eastern China
Crystallization of Hydrosodalite Na<sub>6</Sub>[AlSiO<sub>4</Sub>]<sub>6</Sub>(H<sub>2</Sub>O)<sub>8</Sub> And Tetrahydroborate Sodalite Na<sub>8</Sub>[AlSiO<sub>4</Sub>]<sub>6</Sub>(BH<sub>4</Sub>)<sub>2</Sub> Inside the Openings of Wafer-Thin Steel Mes
Advances in Chemical Engineering and Science
Ion Exchange of Layer-Structured Titanate Cs<sub>x</Sub>Ti<sub>2</Sub>-≪i><sub>x</Sub></I>/≪sub>2</Sub>Mg<i><sub>x</Sub></I>/≪sub>2</Sub>O<sub>4</Sub> (≪i>x</I> = 0.70) and Applications as Cathode Materials for Both Lithium- And Sodium-Ion Batteries
Materials Sciences and Applications
Multiphase Reaction of SO<sub>2</sub> With NO<sub>2</sub> On CaCO<sub>3</sub> Particles. 1. Oxidation of SO<sub>2</sub> By NO<sub>2</sub>
Synthesis and Piezoelectric Properties of Pb<sub>0.98</Sub>Sm<sub>0.02</Sub>[(Zr<sub>y</Sub>,Ti<sub>1–y</Sub>)<sub>0.98</Sub>(Fe<sub>1/2</Sub><sup>3+</Sup>,Nb<sub>1/2</Sub><sup>5+</Sup>)<sub>0.02</Sub>]O<sub>3</Sub> Ceramics
Materials Sciences and Applications
Investigation of Viscosity's Effects on Continuous Casting of Steel Mold Powders Containing B<sub>2</Sub>O<sub>3</Sub>, Li<sub>2</Sub>O, TiO<sub>2</sub>, Fe<sub>2</Sub>O<sub>3</Sub>, ZnO and Na<sub>2</Sub>O
Engineering
Spectroscopic Studies of 50Bi<sub>2</Sub>O<sub>3</Sub>-(50 - X)B<sub>2</Sub>O<sub>3</Sub>-xSm<sub>2</Sub>O<sub>3</Sub> Glasses System
New Journal of Glass and Ceramics
Supplementary Material to &Quot;Significant Production of ClNO<sub>2</sub> And Possible Source of Cl<sub>2</Sub> From N<sub>2</Sub>O<sub>5</Sub> Uptake at a Suburban Site in Eastern China"