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自终止镍电沉积及析氢过程中氢氧化镍形成的超微电极研究

Ultramicroelectrode Studies of Self-Terminated Nickel Electrodeposition and Nickel Hydroxide Formation upon Water Reduction.

作者信息

Ritzert Nicole L, Moffat Thomas P

机构信息

Material Measurement Laboratory, National Institute of Standards and Technology, 100 Bureau Drive, Gaithersburg, MD 20899, USA.

出版信息

J Phys Chem C Nanomater Interfaces. 2016 Dec 8;120(48):27478-27489. doi: 10.1021/acs.jpcc.6b10006. Epub 2016 Nov 14.

DOI:10.1021/acs.jpcc.6b10006
PMID:28217241
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC5312800/
Abstract

The interaction between electrodeposition of Ni and electrolyte breakdown, namely the hydrogen evolution reaction (HER) HO and HO reduction, was investigated under well-defined mass transport conditions using ultramicroelectrodes (UME's) coupled with optical imaging, generation/collection scanning electrochemical microscopy (G/C-SECM), and preliminary microscale pH measurements. For 5 mmol/L NiCl + 0.1 mol/L NaCl, pH 3.0, electrolytes, the voltammetric current at modest overpotentials, , between -0.6 V and -1.4 V vs. Ag/AgCl, was distributed between metal deposition and HO reduction, with both reactions reaching mass transport limited current values. At more negative potentials, an unusual sharp current spike appeared upon the onset of HO reduction that was accompanied by a transient increase in H production. The peak potential of the current spike was a function of both [Ni(HO)] concentration and pH. The sharp rise in current was ascribed to the onset of autocatalytic HO reduction, where electrochemically generated OH species induce heterogeneous nucleation of Ni(OH) islands, the perimeter of which is reportedly active for HO reduction. As the layer coalesces, further metal deposition is quenched while HO reduction continues albeit at a decreased rate as fewer of the most reactive sites, , Ni/Ni(OH) island edges, are available. At potentials below -1.5 V vs. Ag/AgCl, HO reduction is accelerated, leading to homogeneous precipitation of bulk Ni(OH)·HO within the nearly hemispherical diffusion layer of the UME.

摘要

在明确的传质条件下,使用超微电极(UME)结合光学成像、产生/收集扫描电化学显微镜(G/C-SECM)以及初步的微尺度pH测量,研究了镍的电沉积与电解质分解之间的相互作用,即析氢反应(HER)、H₂O和H₂O₂还原。对于5 mmol/L NiCl₂ + 0.1 mol/L NaCl、pH 3.0的电解质,在相对于Ag/AgCl为-0.6 V至-1.4 V的适度过电位η下,伏安电流分布在金属沉积和H₂O₂还原之间,两个反应均达到传质限制电流值。在更负的电位下,H₂O₂还原开始时出现异常尖锐的电流尖峰,同时H₂产生瞬时增加。电流尖峰的峰值电位是[Ni(H₂O)₆]²⁺浓度和pH的函数。电流的急剧上升归因于自催化H₂O₂还原的开始,其中电化学产生的OH物种诱导Ni(OH)₂岛的异相成核,据报道其周边对H₂O₂还原具有活性。随着层的合并,进一步的金属沉积被淬灭,而H₂O₂还原继续进行,尽管速率降低,因为活性最高的位点(即Ni/Ni(OH)₂岛边缘)减少。在相对于Ag/AgCl低于-1.5 V的电位下,H₂O₂还原加速,导致在UME的近半球形扩散层内形成大量Ni(OH)₂·H₂O的均匀沉淀。