Maria Bilichenko, Marcella Iannuzzi, Gabriele Tocci
{"title":"二维材料水界面上憎水剂的滑动不透明度和快速渗透传输 \"的更正","authors":"Maria Bilichenko, Marcella Iannuzzi, Gabriele Tocci","doi":"10.1021/acsnano.4c14736","DOIUrl":null,"url":null,"abstract":"In the discussion of the results presented in Figure 4c of the originally published article, an error was introduced in describing the range of the diffusio-osmotic coefficient. Specifically, the following sentence incorrectly states the range as −450 μm<sup>2</sup>/s to +450 μm<sup>2</sup>/s, whereas the correct range is −4900 μm<sup>2</sup>/s to +5300 μm<sup>2</sup>/s, as shown in Figure 4c: “Notably, graphene-coated systems exhibit the largest variation in diffusio-osmotic mobility, ranging from approximately −450 μm<sup>2</sup>/s for bilayer graphene with <i>r</i> = 2.25 Å to around 450 μm<sup>2</sup>/s for single-layer graphene with <i>r</i> = 1.5 Å”. For all systems except those where graphene is in direct contact with water (i.e., the top two-dimensional material) <i>D</i><sub>DO</sub> falls in a range between −1000 μm<sup>2</sup>/s and +1000 μm<sup>2</sup>/s. For systems where graphene is the top material instead, <i>D</i><sub>DO</sub> can reach values approximately between −5000 μm<sup>2</sup>/s and +5000 μm<sup>2</sup>/s, depending on the size of the hydrophobic solute, further stressing the influence of the large slip-length of graphene on <i>D</i><sub>DO</sub>, as opposed to systems where hBN or MoS<sub>2</sub> are the top materials. In the original article, we discuss our numerical results in the broader context of diffusio-osmotic transport experiments on other systems, in particular on silica which can be considered a model system for studies of diffusio-osmosis. For example, the range of values of <i>D</i><sub>DO</sub> reported in ref (1) (<i>D</i><sub>DO</sub> = −230 μm<sup>2</sup>/s) and ref (2) (<i>D</i><sub>DO</sub> = 200–800 μm<sup>2</sup>/s) is narrower than those on graphene-covered surfaces that we have investigated, highlighting the impact of slippage on diffusio-osmotic transport on graphene as opposed to a nonslipping surface such as silica. The conclusion of the manuscript regarding the influence of hydrophobes’ size and of the slip length on diffusio-osmotic transport is not altered by this correction, in fact we recognize that the slip-induced amplification of D<sub>DO</sub> is more pronounced than what we have discussed previously. We apologize for the error and any confusion it may have caused. This article references 2 other publications. This article has not yet been cited by other publications.","PeriodicalId":21,"journal":{"name":"ACS Nano","volume":"183 1","pages":""},"PeriodicalIF":15.8000,"publicationDate":"2024-11-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Correction to “Slip Opacity and Fast Osmotic Transport of Hydrophobes at Aqueous Interfaces with Two-Dimensional Materials”\",\"authors\":\"Maria Bilichenko, Marcella Iannuzzi, Gabriele Tocci\",\"doi\":\"10.1021/acsnano.4c14736\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"In the discussion of the results presented in Figure 4c of the originally published article, an error was introduced in describing the range of the diffusio-osmotic coefficient. Specifically, the following sentence incorrectly states the range as −450 μm<sup>2</sup>/s to +450 μm<sup>2</sup>/s, whereas the correct range is −4900 μm<sup>2</sup>/s to +5300 μm<sup>2</sup>/s, as shown in Figure 4c: “Notably, graphene-coated systems exhibit the largest variation in diffusio-osmotic mobility, ranging from approximately −450 μm<sup>2</sup>/s for bilayer graphene with <i>r</i> = 2.25 Å to around 450 μm<sup>2</sup>/s for single-layer graphene with <i>r</i> = 1.5 Å”. For all systems except those where graphene is in direct contact with water (i.e., the top two-dimensional material) <i>D</i><sub>DO</sub> falls in a range between −1000 μm<sup>2</sup>/s and +1000 μm<sup>2</sup>/s. For systems where graphene is the top material instead, <i>D</i><sub>DO</sub> can reach values approximately between −5000 μm<sup>2</sup>/s and +5000 μm<sup>2</sup>/s, depending on the size of the hydrophobic solute, further stressing the influence of the large slip-length of graphene on <i>D</i><sub>DO</sub>, as opposed to systems where hBN or MoS<sub>2</sub> are the top materials. In the original article, we discuss our numerical results in the broader context of diffusio-osmotic transport experiments on other systems, in particular on silica which can be considered a model system for studies of diffusio-osmosis. For example, the range of values of <i>D</i><sub>DO</sub> reported in ref (1) (<i>D</i><sub>DO</sub> = −230 μm<sup>2</sup>/s) and ref (2) (<i>D</i><sub>DO</sub> = 200–800 μm<sup>2</sup>/s) is narrower than those on graphene-covered surfaces that we have investigated, highlighting the impact of slippage on diffusio-osmotic transport on graphene as opposed to a nonslipping surface such as silica. The conclusion of the manuscript regarding the influence of hydrophobes’ size and of the slip length on diffusio-osmotic transport is not altered by this correction, in fact we recognize that the slip-induced amplification of D<sub>DO</sub> is more pronounced than what we have discussed previously. We apologize for the error and any confusion it may have caused. This article references 2 other publications. This article has not yet been cited by other publications.\",\"PeriodicalId\":21,\"journal\":{\"name\":\"ACS Nano\",\"volume\":\"183 1\",\"pages\":\"\"},\"PeriodicalIF\":15.8000,\"publicationDate\":\"2024-11-24\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"ACS Nano\",\"FirstCategoryId\":\"88\",\"ListUrlMain\":\"https://doi.org/10.1021/acsnano.4c14736\",\"RegionNum\":1,\"RegionCategory\":\"材料科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"CHEMISTRY, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"ACS Nano","FirstCategoryId":"88","ListUrlMain":"https://doi.org/10.1021/acsnano.4c14736","RegionNum":1,"RegionCategory":"材料科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"CHEMISTRY, MULTIDISCIPLINARY","Score":null,"Total":0}
Correction to “Slip Opacity and Fast Osmotic Transport of Hydrophobes at Aqueous Interfaces with Two-Dimensional Materials”
In the discussion of the results presented in Figure 4c of the originally published article, an error was introduced in describing the range of the diffusio-osmotic coefficient. Specifically, the following sentence incorrectly states the range as −450 μm2/s to +450 μm2/s, whereas the correct range is −4900 μm2/s to +5300 μm2/s, as shown in Figure 4c: “Notably, graphene-coated systems exhibit the largest variation in diffusio-osmotic mobility, ranging from approximately −450 μm2/s for bilayer graphene with r = 2.25 Å to around 450 μm2/s for single-layer graphene with r = 1.5 Å”. For all systems except those where graphene is in direct contact with water (i.e., the top two-dimensional material) DDO falls in a range between −1000 μm2/s and +1000 μm2/s. For systems where graphene is the top material instead, DDO can reach values approximately between −5000 μm2/s and +5000 μm2/s, depending on the size of the hydrophobic solute, further stressing the influence of the large slip-length of graphene on DDO, as opposed to systems where hBN or MoS2 are the top materials. In the original article, we discuss our numerical results in the broader context of diffusio-osmotic transport experiments on other systems, in particular on silica which can be considered a model system for studies of diffusio-osmosis. For example, the range of values of DDO reported in ref (1) (DDO = −230 μm2/s) and ref (2) (DDO = 200–800 μm2/s) is narrower than those on graphene-covered surfaces that we have investigated, highlighting the impact of slippage on diffusio-osmotic transport on graphene as opposed to a nonslipping surface such as silica. The conclusion of the manuscript regarding the influence of hydrophobes’ size and of the slip length on diffusio-osmotic transport is not altered by this correction, in fact we recognize that the slip-induced amplification of DDO is more pronounced than what we have discussed previously. We apologize for the error and any confusion it may have caused. This article references 2 other publications. This article has not yet been cited by other publications.
期刊介绍:
ACS Nano, published monthly, serves as an international forum for comprehensive articles on nanoscience and nanotechnology research at the intersections of chemistry, biology, materials science, physics, and engineering. The journal fosters communication among scientists in these communities, facilitating collaboration, new research opportunities, and advancements through discoveries. ACS Nano covers synthesis, assembly, characterization, theory, and simulation of nanostructures, nanobiotechnology, nanofabrication, methods and tools for nanoscience and nanotechnology, and self- and directed-assembly. Alongside original research articles, it offers thorough reviews, perspectives on cutting-edge research, and discussions envisioning the future of nanoscience and nanotechnology.