In Situ Encapsulating α-MnS into N,S-Codoped Nanotube-Like Carbon as Advanced Anode Material: α → β Phase Transition Promoted Cycling Stability and Superior Li/Na-Storage Performance in Half/Full Cells

2018 ◽  
Vol 30 (21) ◽  
pp. 1706317 ◽  
Author(s):  
Dai-Huo Liu ◽  
Wen-Hao Li ◽  
Yan-Ping Zheng ◽  
Zheng Cui ◽  
Xin Yan ◽  
...  
2019 ◽  
Vol 790 ◽  
pp. 502-508 ◽  
Author(s):  
Michele Catti ◽  
Oscar Fabelo ◽  
Alessandra Filabozzi ◽  
Antonino Pietropaolo ◽  
Alessia Santucci ◽  
...  

2008 ◽  
Vol 39 (12) ◽  
pp. 2815-2819 ◽  
Author(s):  
Daniel R. Kammler ◽  
Mark A. Rodriguez ◽  
Ralph G. Tissot ◽  
Donald W. Brown ◽  
Bjørn Clausen ◽  
...  

2018 ◽  
Vol 5 (4) ◽  
pp. 171932 ◽  
Author(s):  
Kunyapat Thummavichai ◽  
Nannan Wang ◽  
Fang Xu ◽  
Graham Rance ◽  
Yongda Xia ◽  
...  

This study uses two in situ techniques to investigate the geometry and phase change behaviour of bundled ultrathin W 18 O 49 nanowires and WO 3 nanoparticles. The in situ X-ray diffraction (XRD) results have shown that the phase transition of WO 3 nanoparticles occurs in sequence from monoclinic (room temperature) → orthorhombic (350°C) → tetragonal (800°C), akin to bulk WO 3 ; however, W 18 O 49 nanowires remain stable as the monoclinic phase up to 500°C, after which a complete oxidation to WO 3 and transformation to the orthorhombic β-phase at 550°C is observed. The in situ Raman spectroscopy investigations have revealed the Raman peak downshifts as the temperature increases, and have identified the 187.6 cm −1 as the fingerprint band for the phase transition from γ- to β-phase of the WO 3 nanoparticle. Furthermore, WO 3 nanoparticles exhibit the γ- to β-phase conversion at 275°C, which is about 75°C lower than the relaxation temperature of 350°C for the monoclinic γ-W 18 O 49 nanowires. These new fundamental understandings on the phase transition behaviour offer important guidance for the design and development of tungsten oxide-based nanodevices by defining their allowed operating conditions.


2017 ◽  
Vol 425 ◽  
pp. 978-987 ◽  
Author(s):  
Tianbo Yang ◽  
Wanxi Zhang ◽  
Linlin Li ◽  
Bo Jin ◽  
Enmei Jin ◽  
...  

2018 ◽  
Vol 54 (14) ◽  
pp. 1714-1717 ◽  
Author(s):  
Wei Wang ◽  
Lin Liu ◽  
Peng-Fei Wang ◽  
Tong-Tong Zuo ◽  
Ya-Xia Yin ◽  
...  

Due to the space confinement of in situ conversion, the BiOF electrode shows superior magnesium storage performance.


2005 ◽  
Vol 105 ◽  
pp. 55-60 ◽  
Author(s):  
Heinz Günter Brokmeier ◽  
Sang Bong Yi ◽  
No Jin Park ◽  
Jens Homeyer

Due to the high penetration power, the high photon flux and the excellent brilliance high energetic synchrotron radiations are a phantastic tool particular in fast experimentation. Therefore in-situ measurements under applied load or at various temperatures have been carried out to investigate the texture influence on the deformation of magnesium and aluminium. An upgraded loading device with a power up to 20 kN was installed at the hard wiggler beamline BW5. Magnesium samples with different initial textures show the strong influence on this texture on the activation of different glide systems and on the activation of twins. First experiments to study the phase transition in titanium were performed, which demonstrate the strong orientation correlation between the α- and the β-phase.


2019 ◽  
Vol 7 (27) ◽  
pp. 16541-16552 ◽  
Author(s):  
Xuefang Xie ◽  
Yang Hu ◽  
Guozhao Fang ◽  
Xinxin Cao ◽  
Bo Yin ◽  
...  

In situ formed hierarchical FeS nanosheets supported by a TiO2/C fibrous backbone exhibit higher rate capability and cycling stability as anode materials for lithium ion batteries.


2020 ◽  
Vol 12 (18) ◽  
pp. 20874-20881 ◽  
Author(s):  
Longfei Wang ◽  
Zhi Zhang ◽  
Yongfa Cheng ◽  
Yanan Zhang ◽  
Weifeng Liu ◽  
...  

2014 ◽  
Vol 47 (4) ◽  
pp. 1205-1215 ◽  
Author(s):  
David E. Damby ◽  
Edward W. Llewellin ◽  
Claire J. Horwell ◽  
Ben J. Williamson ◽  
Jens Najorka ◽  
...  

Cristobalite is a common mineral in volcanic ash produced from dome-forming eruptions. Assessment of the respiratory hazard posed by volcanic ash requires understanding the nature of the cristobalite it contains. Volcanic cristobalite contains coupled substitutions of Al3+ and Na+ for Si4+; similar co-substitutions in synthetic cristobalite are known to modify the crystal structure, affecting the stability of the α and β forms and the observed transition between them. Here, for the first time, the dynamics and energy changes associated with the α–β phase transition in volcanic cristobalite are investigated using X-ray powder diffraction with simultaneous in situ heating and differential scanning calorimetry. At ambient temperature, volcanic cristobalite exists in the α form and has a larger cell volume than synthetic α-cristobalite; as a result, its diffraction pattern sits between ICDD α- and β-cristobalite library patterns, which could cause ambiguity in phase identification. On heating from ambient temperature, volcanic cristobalite exhibits a lower degree of thermal expansion than synthetic cristobalite, and it also has a lower α–β transition temperature (∼473 K) compared with synthetic cristobalite (upwards of 543 K); these observations are discussed in relation to the presence of Al3+ and Na+ defects. The transition shows a stable and reproducible hysteresis loop with α and β phases coexisting through the transition, suggesting that discrete crystals in the sample have different transition temperatures.


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