Examples of using Feo in English and their translations into Russian
{-}
-
Official
-
Colloquial
Within her family she was called Feo.
Tico Feo: a lively eighteen-year-old man from Cuba, who has blonde hair and blue eyes.
Another anomaly: the presence of microscopic particles Fe. FeO. Fe2O3, in the soil.
This is an evidence of FeO reducing in the melt with forming the fluid Fe phase.
Rust consists of hydrated iron(III) oxides Fe2O3·nH2O and iron(III)oxide-hydroxide FeO(OH), Fe(OH)3.
Increasing of temperature leads to FeO concentration decreasing and Al2O, MgO increasing.
In 1719 Feo wrote La forza della virtù(The Power of Virtue), and then his opera seria Teuzzone in 1720.
The three main iron compounds are wustite(FeO), hematite(Fe2O3), and magnetite Fe3O4.
It is known that FeO has a black/gray color, Fe3O4 is black, Fe2O3 in the form of a powder is red.
Scale is a mixture of iron oxides:wuistite(FeO), magnetite(Fe3O4) and hematite Fe2O3.
Lowering of the contents(FeO) carries to increase in an angle of wettability and with approximation to 5% an angle"reaches" to 90.
Our equation reproduces Haughton's data,as well as the dependence of sulfur concentration on the content of FeO Fig. 3, 4.
Experiments with high and low FeO contents are well reproduced, and even overlapped on the plot Fig. 5.
With limited dissolved oxygen, iron(II)-containing materials are favoured,including FeO and black lodestone or magnetite Fe3O4.
Otherwise, if insufficient oxygen is present, tetracalcium alumino ferrite does not form;instead Fe2O3 is reduced to FeO.
In a letter to the Crown Princess, Queen Victoria described her as"sweet little Feo, who is so good and I think grown quite pretty.
We have characterized the nature and quantified the abundance of N- andH-compounds dissolved in a model silicate melt NaAlSi3O8 80% wt+ FeO 20% wt.
The following parameters were taken as an example by De Feo et al.: p prime for the key exchange with wA 2, wB 3, eA 63, eB 41, and f 11.
The unique grey orgreen celadon glaze is a result of iron oxide's transformation from ferric to ferrous iron(Fe2O3→ FeO) during the firing process.
Unlike the method of De Feo, Jao, and Plut, the method of Rostovtsev and Stolbunov used ordinary elliptic curves and was found to have a subexponential quantum attack.
Multispectral images obtained from these missions showed that this basin contains more FeO and TiO2 than typical lunar highlands, and hence has a darker appearance.
It is set that in case of the contents(FeO) more than 25% a wettability angle in case of the contents(MgO)- 6-7% less than 10, that is aren't enough wettability practically isn't present.
When this proved successful, he was enrolled in 1725 at the Conservatorio di Santo Onofrio a Capuana in Naples,where he studied under Ignazio Prota alongside Tomaso Prota and Francesco Feo.
Condensation from FeO and SiO2 rich vapor was considered[7] to be the most efficient at late stages of expansion of a vapor cloud when evaporation was terminated by cooling.
The difference between these two magma series can be seen on an AFM diagram,a ternary diagram showing the relative proportions of the oxides Na2O+ K2O(A), FeO+ Fe2O3(F), and MgO M.
The composition of chromites from the upper sample on average(wt.%: Al2O3- 5.3,TiO2- 2.9, FeO- 26.5, MgO- 1.9; Cr/(Cr+Al)=88) corresponded to the composition of chromites from the fossil meteorites and ordinary chondrites.
If we increase only the concentration of one of the oxides, without changing the proportions of the other components, we obtain a significant positive dependence of sulfur concentration on TiO2,Al2O3 and FeO, and the negative dependence on SiO2, MgO, CaO.
The main peculiarity of the chemical composition of glasses is a decrease of FeO concentrations from 18 mass%, that corresponds to the FeO content in the starting material, to 0.3 mass% at the lower Δlg fO2(IW) values equal to- 5.7.
Feo composed the serenate Oreste and Polinice for Madrid in 1738, and for the Fathers of the Holy Cross in Prague he wrote the oratorio La distruzione dell'esercito dei Cananei con la morte di Sisara The Destruction of the Canaanite Army and the Death of Sisara, 1739.
In the first stratigraphically lower sample chromites had an average composition(wt.%: Al2O3- 5.0,TiO2- 2.7, FeO- 26.1, MgO- 3.4 with Cr/(Cr+Al)=88.5) corresponding to that of the Swedish fossil meteorites and ordinary chondrites.