Polydispersity Effect and Coagulation Structures on the Surface Tension of Isotherms for Bentonite Suspensions

R. Dadashev, Z. I. Dadasheva, Z. Z. Alarkhanova, Kh.S. Talkhigova, R. Dzhambulatov, S. Alikhadzhiev, Z. Khasbulatova
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Abstract

The paper presents the results of an experimental study considering the dependence of the surface tension of bentonite aqueous suspensions on the concentration of the solid phase and the time of the surface formation. To conduct experimental studies, a new technique has been developed, which allows leveling the influence of the sedimentation factor on the magnitude of the surface tension. A distinctive feature of the proposed technique is that these methods of measuring surface tension are used for the first time. In this method the process of sedimentation is multidirectional relative to the surface. The results obtained allowed us to determine that the resulting coagulation structures have a significant influence on the nature of changes in the surface tension of bentonite aqueous suspensions. It was established that the polydispersity of the solid phase and water molecules in the dispersion medium play a key role in the formation of spatial structures and, as a consequence, in the formation of a minimum on the surface tension isotherms of bentonite suspensions.
膨润土悬浮液等温线表面张力的多分散性效应和混凝结构
本文给出了考虑膨润土水悬浮液表面张力与固相浓度和表面形成时间关系的实验研究结果。为了进行实验研究,研究人员开发了一种新技术,可以平衡沉积因素对表面张力大小的影响。该技术的一个显著特点是,这些测量表面张力的方法是第一次使用。在这种方法中,沉积过程相对于表面是多向的。得到的结果使我们能够确定所产生的混凝结构对膨润土水悬浮液表面张力变化的性质有重大影响。结果表明,分散介质中固相和水分子的多分散性在空间结构的形成中起着关键作用,因此,在膨润土悬浮液表面张力等温线的最小值的形成中起着关键作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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