Improved analysis methods to study the behavior of potassium ions in the interlayer of montmorillonite

• Main Authors: Danchao Huang, Gang Xie, Pengfei Hu, Sipei Hu, Zhan Zhao, Wai Li, Mingyi Deng, Pingya Luo
• Format: Article
• Language: English
• Published: Elsevier 2020-07-01
• Series: Journal of Materials Research and Technology
• Subjects: Potassium chloride; Montmorillonite; Analysis methods; Interaction mechanism; Shale
• Online Access: http://www.sciencedirect.com/science/article/pii/S2238785420312102

The behavior of potassium chloride (KCl) as a main mud shale inhibitor remains poorly defined in the interlayer of montmorillonite (Mt). In this paper, a new analysis method of transmission electron microscopy-energy dispersive X-ray spectroscopy (TEM-EDS) was established. The distribution of K+ in the interlayer of Mt and the processes surrounding d-spacing shifts in Mt were investigated through X-ray diffraction and TEM-EDS. The experimental results revealed shoulder peaks in the diffraction patterns at KCl concentrations between 11% and 19%. The distribution of K+ varied in the inner and outer layers of Mt with different KCl concentrations. It could be concluded that the distribution of K+ and the changes in d-spacing of Na are determined by two factors: negative charge sites and concentration difference. When the KCl concentration was below 8%, both factors cause the outer layer of Mt to adsorb more K+ than the inner layer, with all layers exhibiting d-spacings within the 1.50 nm state. At an 8% KCl concentration, all negative charge sites were occupied by K+. As the KCl concentration rose above 8%, the outer layer of Mt adsorbed more K+ than the inner layer due to the concentration difference. With a further increase in the KCl concentration, the d-spacing shifted linearly to 1.30 nm from the outer to the inner layer of Mt. All layers of Mt exhibited a d-spacing of 1.30 nm at KCl concentrations of up to 23%. These results demonstrate the benefits and capabilities of the proposed method in investigating the intercalating mechanisms of Mt.