Suman Khushboo, Mittal Mohit, Joshi Yogesh M
Department of Chemical Engineering, Indian Institute of Technology, Kanpur 208016, India.
J Phys Condens Matter. 2020 May 20;32(22):224002. doi: 10.1088/1361-648X/ab724d.
In this work, we investigate the physical origin of ergodicity breaking in an aqueous colloidal dispersion of synthetic hectorite clay, LAPONITE, by performing dissolution and rheological experiments with monovalent salt and tetrasodium pyrophosphate solution. We also study the effect of pH and nature of interface, nitrogen and paraffin oil on the same. Dissolution experiments carried out for dispersions with both the interfaces show similar results. However, for samples with a nitrogen interface, all the effects are observed to get expedited in time compared to a paraffin oil interface. When kept in contact with water, 1.5 wt.% and 2.8 wt.% colloidal dispersion at pH 10 swells at small ages, while it does not swell at large ages. The solution of tetrasodium pyrophosphate, interestingly, dissolves the entire colloidal dispersion sample with pH 10 irrespective of the concentration of clay. Experiments carried out on colloidal dispersions prepared in water having pH 13 demonstrate no effect of water as well as sodium pyrophosphate solution on the same suggesting a possibility of the presence of negative charge on edge at that pH. We believe that all the behaviors observed for samples at pH 10 can be explained by an attractive gel microstructure formed by edge-to-face contact. Furthermore, the absence of swelling in old colloidal dispersion at pH 10 and dissolution of the same by sodium pyrophosphate solution cannot be explained by merely repulsive interactions. This behavior suggests that attractive interactions originating from edge-to-face contact play an important role in causing ergodicity breaking in the colloidal dispersions at pH 10 at all the ages irrespective of the clay concentration. We further substantiate the presence of a fractal network structure formed by interparticle edge-face association using rheological tools and cryo-TEM imaging. We also conduct a comprehensive study of the effect of tetrasodium pyrophosphate on the sol-gel transition of LAPONITE dispersion.
在这项工作中,我们通过用单价盐和焦磷酸四钠溶液进行溶解和流变学实验,研究了合成锂皂石粘土LAPONITE的水相胶体分散体中遍历性破坏的物理起源。我们还研究了pH值和界面性质(氮气和石蜡油)对其的影响。对具有两种界面的分散体进行的溶解实验显示了相似的结果。然而,对于具有氮气界面的样品,与石蜡油界面相比,所有影响在时间上都更快出现。当与水接触时,pH值为10的1.5 wt.%和2.8 wt.%胶体分散体在较小龄期会膨胀,而在较大龄期则不会膨胀。有趣的是,焦磷酸四钠溶液能溶解pH值为10的整个胶体分散体样品,而与粘土浓度无关。在pH值为13的水中制备的胶体分散体上进行的实验表明,水和焦磷酸钠溶液对其均无影响,这表明在该pH值下边缘可能存在负电荷。我们认为,在pH值为10时观察到的样品的所有行为都可以通过由边对面接触形成的吸引性凝胶微观结构来解释。此外,pH值为10的旧胶体分散体中没有膨胀现象以及其被焦磷酸钠溶液溶解,这不能仅仅用排斥相互作用来解释。这种行为表明,源自边对面接触的吸引相互作用在导致pH值为10的所有龄期的胶体分散体中的遍历性破坏中起着重要作用,而与粘土浓度无关。我们进一步使用流变学工具和低温透射电子显微镜成像证实了由颗粒间边-面缔合形成的分形网络结构的存在。我们还全面研究了焦磷酸四钠对LAPONITE分散体溶胶-凝胶转变的影响。