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用不同方法对膨润土胶体进行粒度表征。

Size characterization of bentonite colloids by different methods.

作者信息

Plaschke M, Schäfer T, Bundschuh T, Manh T N, Knopp R, Gockeis H, Kim J I

机构信息

Institut für Nukleare Entsorgung, Forschungszentrum Karlsruhe GmbH, Germany.

出版信息

Anal Chem. 2001 Sep 1;73(17):4338-47. doi: 10.1021/ac010116t.

Abstract

The size and shape of colloids released from a natural bentonite into a low-mineralized groundwater are investigated using various colloid characterization methods. For the applied methods such as atomic force microscopy (AFM), laser-induced breakdown detection (UBD), photon correlation spectroscopy (PCS), and flow field-flow fractionation coupled to ICP-mass spectrometric detection (FFFF-ICPMS), the respective raw size data have to be corrected in order to consider chemical composition and shape of the colloids as well as instrumental artifacts. Noncontact mode AFM of the bentonite colloids shows disklike shapes of stacked smectite platelets with a mean height-to-diameter proportion (aspect ratio) of approximately 1/10. A broad particle number size distribution is determined by image processing with a mean particle diameter of 73 nm. In agreement with AFM, a broad size distribution is also found by PCS and FFFF-ICPMS. Likewise, mean particle sizes found by LIBD (67 +/- 13 nm) and FFFF-ICPMS (maximum in the number size distribution, approximately 70 nm) are in fair agreement with the AFM data. Somewhathigher values are obtained by PCS, where mean particle diameters of the intensity-weighted size distributions of larger than 200 nm are found (depending on the algorithm used for data processing). The influence of the disklike particle shape on the results of the individual methods is discussed. As a conclusion, the application of different colloid characterization methods is a prerequisite to get complementary information about colloid size and shape, which is essential for the understanding of natural colloidal systems.

摘要

利用各种胶体表征方法,研究了天然膨润土释放到低矿化度地下水中的胶体的大小和形状。对于所应用的方法,如原子力显微镜(AFM)、激光诱导击穿检测(UBD)、光子相关光谱(PCS)以及与电感耦合等离子体质谱检测联用的流场-流分级法(FFFF-ICPMS),为了考虑胶体的化学成分、形状以及仪器假象,必须对各自的原始尺寸数据进行校正。膨润土胶体的非接触模式原子力显微镜显示出堆叠蒙脱石片晶的盘状形状,平均高径比约为1/10。通过图像处理确定了宽的颗粒数尺寸分布,平均粒径为73nm。与原子力显微镜结果一致,光子相关光谱和流场-流分级法-电感耦合等离子体质谱也发现了宽的尺寸分布。同样,激光诱导击穿检测(67±13nm)和流场-流分级法-电感耦合等离子体质谱(数量尺寸分布中的最大值,约70nm)得到的平均粒径与原子力显微镜数据相当吻合。光子相关光谱得到的值略高,其中发现强度加权尺寸分布的平均粒径大于200nm(取决于用于数据处理的算法)。讨论了盘状颗粒形状对各方法结果的影响。总之,应用不同的胶体表征方法是获取关于胶体大小和形状的补充信息的前提条件,这对于理解天然胶体系统至关重要。

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