Baalousha M, Lead J R
School of Geography, Earth and Environmental Sciences, University of Birmingham, Edgbaston, Birmingham B15 2TT, United Kingdom.
Environ Sci Technol. 2007 Feb 15;41(4):1111-7. doi: 10.1021/es061766n.
Flow-field flow fractionation (FIFFF) coupled to a UV detector and to atomic force microscopy (AFM) has been used, for the first time, to characterize ultrafine natural colloids (<5 nm) from selected freshwaters. FIFFF-UV measures a "weight diffusion coefficient distribution" and the corresponding "weight hydrodynamic diameter distribution" was calculated by applying FIFFF theory and the Stokes-Einstein equation. In addition, FIFFF has been used to prepare fractions of very narrow size range for AFM analysis. AFM measures number distribution of particle height (related to radius), and these were calculated. Both raw and transformed data show good agreement between the techniques, with conversion of the UV data to a number-weighted distribution giving better agreement and reduced errors. The small differences between the corrected data from UV analysis and the raw AFM data are either due to the fundamental differences in the analytical techniques, that is, measurement of hydrodynamic properties (FIFFF) or properties after sorption to a solid phase (AFM), or are due to the assumptions of the Stokes-Einstein equation not being met, that is, the fine natural colloids are not spherical or permeable. The methodology offers a means of quantifying fine colloid nonsphericity and permeability.
流场流分级法(FIFFF)与紫外检测器和原子力显微镜(AFM)联用,首次用于表征从特定淡水中提取的超细天然胶体(<5纳米)。FIFFF-UV测量“重量扩散系数分布”,并通过应用FIFFF理论和斯托克斯-爱因斯坦方程计算相应的“重量流体动力学直径分布”。此外,FIFFF已用于制备尺寸范围非常窄的级分用于AFM分析。AFM测量颗粒高度(与半径相关)的数量分布,并对其进行计算。原始数据和转换后的数据在两种技术之间显示出良好的一致性,将紫外数据转换为数量加权分布可实现更好的一致性并减少误差。紫外分析校正数据与原始AFM数据之间的微小差异,要么是由于分析技术的根本差异,即流体动力学性质(FIFFF)的测量或吸附到固相后的性质(AFM)的测量,要么是由于未满足斯托克斯-爱因斯坦方程的假设,即细天然胶体不是球形或不可渗透的。该方法提供了一种量化细胶体非球形度和渗透率的手段。