Ionic strength dependence of aggregate size and morphology on polymerclay flocculation

被引:29
|
作者
Wilkinson, Nikolas [1 ]
Metaxas, Athena [1 ]
Brichetto, Eric [2 ]
Wickramaratne, Susith [3 ]
Reineke, Theresa M. [3 ]
Dutcher, Cari S. [2 ]
机构
[1] Univ Minnesota, Dept Chem Engn & Mat Sci, 421 Washington Ave SE, Minneapolis, MN 55455 USA
[2] Univ Minnesota, Dept Mech Engn, 111 Church St SE, Minneapolis, MN 55455 USA
[3] Univ Minnesota, Dept Chem, 207 Pleasant St SE, Minneapolis, MN 55455 USA
基金
美国国家科学基金会;
关键词
Flocculation; Anisotropic particles; Smectite clays; Polyelectrolytes; Aqueous colloidal suspensions; POLYELECTROLYTE ADSORPTION; MONTMORILLONITE SUSPENSIONS; SODIUM MONTMORILLONITE; RHEOLOGICAL PROPERTIES; WATER-TREATMENT; PARTICLES; BENTONITE; ELECTROLYTE; PH; SYSTEMS;
D O I
10.1016/j.colsurfa.2017.06.085
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
Polymer-driven flocculation of suspended particles is a critical process for many applications, including composite materials synthesis, paper manufacturing, and water treatment. However, the role of solution physicochemical properties on the polymer-particle assembly dynamics is nontrivial, particularly for non-spherical, polydisperse particulates such as natural clays. In this work, we study the effects of ionic strength and aggregate size and structure on the polymer behavior and flocculation performance with anisotropic bentonite clay particles. Using jar tests, laser diffraction, confocal microscopy, and X-ray diffraction, we demonstrate that for smectite clay particles, the final floc structure is largely informed by ionic-strength driven changes to the initial clay aggregate size and surface structure. With increasing bentonite aggregate size, a transition from a networked to a patched polymer -aggregate floc structure is observed, independent of ionic strength during flocculation. Solutions were studied over four orders of magnitude of NaCl ionic strength. Initial, pre-flocculated bentonite aggregate sizes ranging from 0.015 mu m to 15 mu m were used, produced by tuning the initial solution ionic strength. Bentonite aggregate size and structure were measured with laser and X-ray diffraction, internal floc structure was visualized using confocal microscopy, and macro floc structure (fractal dimension) was measured with optical imaging. These results shed new light on the fundamental complexity of ionic strength dependence and the importance of the aggregate size and structure of the initial dispersion, in determining optimal reagent dosing and structure control for flocculation of anisotropic clays.
引用
收藏
页码:1037 / 1046
页数:10
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