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It is well-known that quartz is essentially a stable oxide and hence no further oxidation can occur to it.
The latter is due to the formation of a dense chemically stable oxide scale, which retards further oxidation by suppressing the supply of oxide-forming metallic elements [2, 5].
During oxidation at 873 K, a thick, stable oxide layer is formed on the surface with a stoichiometry of PdO, beneath which a Pd-depleted (Pt-rich) layer exists.
It is also planned that the experimental identification of the condition to form the stable oxide layer (SiO2) for SiC layer on the oxidation-resistant graphite and on the SiC-TRISO fuel.
The alloying elements most commonly used for this purpose are chromium and aluminum, both of which form an adherent film of stable oxide on the surface that protects the metal from further oxidation.
CeO2 (where Ce is tetravalent) is the normal stable oxide form, while the oxides of praseodymium and terbium have the Pr6O11 and Tb4O7 stoichiometries containing both the tetra- and the trivalent states i.e., 4PrO2∙Pr2O3 and 2TbO2∙Tb2O3, respectively.
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These results reveal the importance of the formation of stable oxides on rGO to the catalysis of oxidation reactions, which is achieved by using 5 wt% of the doped transition metal, and demonstrated that Cr-rGO, Fe-rGO, and Co-rGO with +3 charge states are good catalysts for the oxidation of Cys.
Au and Pt were chosen as metal components in Si Me mixtures since both metals are believed to catalyze Si oxidation thus reducing the processing temperature, while neither Au nor Pt form stable oxides.
The sesquioxides are among the most stable oxides in the periodic table; the more negative the value of the free energy of formation (ΔGf0), the more stable the oxide.
These may be bricks or ram material made of highly stable oxides, such as magnesite, alumina, or the double oxides chrome-magnesite and dolomite.
The stable oxide-hydroxide film can be formed on the metal surface only in the solutions with the molar ratio of acid to water lower than 1 4.
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