4.8 Article

Thermal stability in the blended lithium manganese oxide - Lithium nickel cobalt manganese oxide cathode materials: An in situ time-resolved X-Ray diffraction and mass spectroscopy study

期刊

JOURNAL OF POWER SOURCES
卷 277, 期 -, 页码 193-197

出版社

ELSEVIER
DOI: 10.1016/j.jpowsour.2014.12.015

关键词

Lithium-ion batteries; Structural evolution; Thermal stability; Phase transformation; Gas evolution

资金

  1. U.S. Department of Energy
  2. Assistant Secretary for Energy Efficiency and Renewable Energy, Office of Vehicle Technologies [DE-AC02-98CH10886]
  3. U.S. Department of Energy, Office of Science, Office of Basic Energy Sciences [DE-AC02-98CH10886]
  4. Hong Kong University of Science and Technology
  5. Energy Efficiency & Resources of the Korea Institute of Energy Technology Evaluation and Planning grant - Korea government Ministry of Trade, Industry Energy [20142020103090]
  6. Korea Evaluation Institute of Industrial Technology (KEIT) [20142020103090] Funding Source: Korea Institute of Science & Technology Information (KISTI), National Science & Technology Information Service (NTIS)

向作者/读者索取更多资源

Thermal stabilities of a series of blended LiMn2O4 (LMO) LiNi(1/3)Coi(1/3)Mn(1/3)O(2) (NCM) cathode materials with different weight ratios were studied by in situ time-resolved X-ray diffraction (XRD) combined with mass spectroscopy in the temperature range of 25 degrees C-580 degrees C under helium atmosphere. Upon heating, the electrochemically delithiated LMO changed into Mn3O4 phase at around 250 degrees C. Formation of MnO with rock-salt structure started at 520 degrees C. This observation is in contrast to the previous report for chemically delithiated LMO in air, in which a process of lambda-MnO2 transforming to beta-MnO2 was observed. Oxygen peak was not observed in all cases, presumably as a result of either consumption by the carbon or detection limit. CO2 profile correlates well with the phase transition and indirectly suggests the oxygen release of the cathode. Introducing NCM into LMO has two effects: first, it makes the high temperature rock-salt phase formation more complicated with more peaks in CO2 profile due to different MO (M = Ni, Mn, Co) phases; secondly, the onset temperature of CO2 release is lowered, implying lowered oxygen release temperature. Upon heating, XRD patterns indicate the NCM part reacts first, followed by the LMO part. This confirms the better thermal stability of LMO over NCM. (C) 2014 Elsevier B.V. All rights reserved.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.8
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据