The Kinetic Peculiarities of the Nanocrystallization of Amorphous Alloys Fe₈₄Nb₂B₁₄, which are Doped by Rare Earth Metals by L. Boichyshyn, M. O. Danyliak, B. Kotur, T. Mika

“…The Avrami constant was found to be 1.86 for Fe</span>₈₄<span>Nb</span>₂<span>B</span>₁₄<span> at 703 K, 1.17 for Fe₈₂Nb₂B₁₄Y₂ at 813 K, 1.36 for Fe</span>₈₂<span>Nb</span>₂<span>B</span>₁₄<span>Gd</span>₂<span> at 808 K, 1.76 for Fe</span>₈₂<span>Nb</span>₂<span>B</span>₁₄<span>Tb</span>₂<span> at 808 K and 1.92 for Fe</span>₈₂<span>Nb</span>₂<span>B</span>₁₄<span>Dy</span>₂<span> at 808 K. Two-dimensional diffusion controlled growth mechanism with decreasing nucleation rate was observed in the alloys. …”
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Authigenic rhabdophane from brown iron ore of the oxidation zone of the Babaryk massive sulfide occurrence (South Urals): scanning electron microscope (SEM) and electron backscatt... by E. V. Belogub, V. V. Shilovskikh, K. A. Novoselov, I. A. Blinov, K. A. Filippova

“…<p>Rhabdophane (Ce<span class="inline-formula">_0.34−0.43</span>Nd<span class="inline-formula">_0.13−0.14</span>Ca<span class="inline-formula">_0.06−0.29</span>La<span class="inline-formula">_0.08−0.11</span>Y<span class="inline-formula">_0.05−0.12</span>Pr<span class="inline-formula">_0.03−0.05</span>Sm<span class="inline-formula">_0.02−0.05</span>Gd<span class="inline-formula">_0.02−0.05</span>Fe<span class="inline-formula">_0−0.04</span>Dy<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M10" display="inline" overflow="scroll" dspmath="mathml"><mrow><msub><mi/><mrow><mn mathvariant="normal">0.00</mn><mo>-</mo><mn mathvariant="normal">0.01</mn></mrow></msub><msub><mo>)</mo><mrow><mn mathvariant="normal">0.97</mn><mo>-</mo><mn mathvariant="normal">1.01</mn></mrow></msub></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="80pt" height="13pt" class="svg-formula" dspmath="mathimg" md5hash="ab54368e4dabe72638a100874cc8de52"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="ejm-33-605-2021-ie00001.svg" width="80pt" height="13pt" src="ejm-33-605-2021-ie00001.png"/></svg:svg></span></span>((P<span class="inline-formula">_0.69−0.96</span>S<span class="inline-formula">_0.04−0.31)_1.00</span>O<span class="inline-formula">₄)</span>⚫H<span class="inline-formula">₂</span>O is found in a Fe<span class="inline-formula">³⁺</span>-oxyhydroxide nodule (brown iron ore) collected from the upper part of the oxidation profile of the Babaryk massive sulfide occurrence (South Urals, Russia) at a 1.6 m depth. …”
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Mckelveyite group minerals – Part 4: Alicewilsonite-(YLa), Na₂Sr₂YLa(CO₃)₆&thinsp; ⋅ &thinsp;3H₂O, a new lanthanum-dominant s... by I. Lykova, R. Rowe, G. Poirier, H. Friis, K. Helwig

“…The empirical formula calculated on the basis of six cations with 3 H<span class="inline-formula">₂</span>O molecules is as follows: Na<span class="inline-formula">_2.10</span>Ca<span class="inline-formula">_0.31</span>Sr<span class="inline-formula">_1.56</span>Ba<span class="inline-formula">_0.10</span>Y<span class="inline-formula">_0.74</span>La<span class="inline-formula">_0.63</span>Pr<span class="inline-formula">_0.07</span> Nd<span class="inline-formula">_0.30</span>Sm<span class="inline-formula">_0.03</span>Eu<span class="inline-formula">_0.01</span>Gd<span class="inline-formula">_0.04</span>Dy<span class="inline-formula">_0.05</span>Ho<span class="inline-formula">_0.01</span>Er<span class="inline-formula">_0.04</span> Yb<span class="inline-formula">_0.01</span>(CO<span class="inline-formula">₃</span>)<span class="inline-formula">_5.92</span>(H<span class="inline-formula">₂</span>O)<span class="inline-formula">₃</span>. …”
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Mckelveyite group minerals – Part 3: Bainbridgeite-(YCe), Na₂Ba₂YCe(CO₃)₆&thinsp; ⋅ &thinsp;3H₂O, a new species from Mont Sai... by I. Lykova, R. Rowe, G. Poirier, H. Friis, K. Helwig

“…The empirical formula of the holotype calculated on the basis of six cations is as follows: Na<span class="inline-formula">_2.11</span>Ca<span class="inline-formula">_0.10</span>Sr<span class="inline-formula">_0.37</span>Ba<span class="inline-formula">_1.60</span>Y<span class="inline-formula">_0.70</span>La<span class="inline-formula">_0.29</span>Ce<span class="inline-formula">_0.49</span>Pr<span class="inline-formula">_0.03</span>Nd<span class="inline-formula">_0.11</span>Sm<span class="inline-formula">_0.01</span>Gd<span class="inline-formula">_0.03</span>Dy<span class="inline-formula">_0.07</span>Ho<span class="inline-formula">_0.02</span>Er<span class="inline-formula">_0.05</span> Yb<span class="inline-formula">_0.02</span>(CO<span class="inline-formula">₃</span>)<span class="inline-formula">_5.86</span>(H<span class="inline-formula">₂</span>O)<span class="inline-formula">_3.00</span>. …”
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Mckelveyite group minerals – Part 2: Alicewilsonite-(YCe), Na₂Sr₂YCe(CO₃)₆&thinsp; ⋅ &thinsp;3H₂O, a new species by I. Lykova, R. Rowe, G. Poirier, H. Friis, K. Helwig

“…The empirical formula of the holotype calculated on the basis of six cations is Na<span class="inline-formula">_2.11</span>Ca<span class="inline-formula">_0.11</span>Sr<span class="inline-formula">_1.83</span>Ba<span class="inline-formula">_0.08</span>Y<span class="inline-formula">_0.67</span>(Ce<span class="inline-formula">_0.51</span>La<span class="inline-formula">_0.32</span>Pr<span class="inline-formula">_0.03</span>Nd<span class="inline-formula">_0.09</span>Sm<span class="inline-formula">_0.02</span>Gd<span class="inline-formula">_0.04</span> Dy<span class="inline-formula">_0.08</span>Ho<span class="inline-formula">_0.02</span>Er<span class="inline-formula">_0.06</span>Yb<span class="inline-formula">_0.03)_Σ1.20</span>(CO<span class="inline-formula">₃)_5.88</span> (H<span class="inline-formula">₂</span>O)<span class="inline-formula">_3.00</span>. …”
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