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阳离子无序岩盐阴极原位二氧化碳脱气的化学起源

Chemical Origin of in Situ Carbon Dioxide Outgassing from a Cation-Disordered Rock Salt Cathode.

作者信息

Huang Tzu-Yang, Cai Zijian, Crafton Matthew J, Giovine Raynald, Patterson Ashlea, Hau Han-Ming, Rastinejad Justin, Rinkel Bernardine L D, Clément Raphaële J, Ceder Gerbrand, McCloskey Bryan D

机构信息

Department of Chemical and Biomolecular Engineering, University of California-Berkeley, Berkeley, California 94720, United States.

Energy Storage and Distributed Resources Division, Lawrence Berkeley National Laboratory, Berkeley, California 94720, United States.

出版信息

Chem Mater. 2024 Jun 24;36(13):6535-6546. doi: 10.1021/acs.chemmater.4c00756. eCollection 2024 Jul 9.

DOI:10.1021/acs.chemmater.4c00756
PMID:39005535
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC11238339/
Abstract

In situ carbon dioxide (CO) outgassing is a common phenomenon in lithium-ion batteries (LiBs), primarily due to parasitic side reactions at the cathode-electrolyte interface. However, little is known about the chemical origins of the in situ CO released from emerging Li-excess cation-disordered rock salt (DRX) cathodes. In this study, we selectively labeled various carbon sources with C in cathodes containing a representative DRX material, LiMnTiO (LMTO), and performed differential electrochemical mass spectrometry (DEMS) during galvanostatic cycling in a carbonate-based electrolyte. When charging LMTO cathodes, electrolyte solvent (EC) decomposition is the dominant source of the CO outgassing. The amount of EC-originated CO is strongly correlated with the total surface area of carbon black in the electrode, revealing the critical role of electron-conducting carbon additives in the electrolyte degradation mechanisms. In addition, unusual bimodal CO evolution during the first cycle is found to originate from carbon black oxidation. Overall, the underlying chemical origin of in situ CO release during battery cycling is highly voltage- and cycle-dependent. This work further provides insights into improving the stability of DRX cathodes in LiBs and is envisioned to help guide future relevant material design to mitigate parasitic reactions in DRX-based batteries.

摘要

原位二氧化碳(CO)脱气是锂离子电池(LiB)中的常见现象,主要是由于阴极-电解质界面处的寄生副反应。然而,对于新兴的富锂阳离子无序岩盐(DRX)阴极释放的原位CO的化学来源知之甚少。在本研究中,我们在含有代表性DRX材料LiMnTiO(LMTO)的阴极中用¹³C选择性标记了各种碳源,并在基于碳酸盐的电解质中恒电流循环期间进行了差分电化学质谱(DEMS)分析。当对LMTO阴极充电时,电解质溶剂(EC)分解是CO脱气的主要来源。源自EC的CO量与电极中炭黑的总表面积密切相关,揭示了导电碳添加剂在电解质降解机制中的关键作用。此外,发现第一个循环中异常的双峰CO释放源自炭黑氧化。总体而言,电池循环期间原位CO释放的潜在化学来源高度依赖于电压和循环。这项工作进一步为提高LiB中DRX阴极的稳定性提供了见解,并有望帮助指导未来相关的材料设计,以减轻基于DRX的电池中的寄生反应。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/898b/11238339/c0872d169e15/cm4c00756_0008.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/898b/11238339/afbce06e144a/cm4c00756_0001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/898b/11238339/1ee31f2111e3/cm4c00756_0002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/898b/11238339/bc0b37bbd8b2/cm4c00756_0003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/898b/11238339/41f303bdf855/cm4c00756_0004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/898b/11238339/8d59e9e1ee18/cm4c00756_0006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/898b/11238339/91d8d4401a86/cm4c00756_0007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/898b/11238339/c0872d169e15/cm4c00756_0008.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/898b/11238339/afbce06e144a/cm4c00756_0001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/898b/11238339/1ee31f2111e3/cm4c00756_0002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/898b/11238339/bc0b37bbd8b2/cm4c00756_0003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/898b/11238339/41f303bdf855/cm4c00756_0004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/898b/11238339/8d59e9e1ee18/cm4c00756_0006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/898b/11238339/91d8d4401a86/cm4c00756_0007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/898b/11238339/c0872d169e15/cm4c00756_0008.jpg

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