{"title":"Intercalation of lecithin into bentonite: pH dependence and intercalation mechanism","authors":"Qiang Li , Romain Berraud-Pache , Christelle Souprayen , Maguy Jaber","doi":"10.1016/j.clay.2023.107079","DOIUrl":null,"url":null,"abstract":"<div><p>A series of organoclays<span><span> were synthesized by modifying bentonite with lecithin under two pH reaction solutions, one acid and one basic. The products prepared using various surfactant concentrations (0.2–5.0CEC) were characterized by multiple experimental techniques. The conformational arrangement of the loaded surfactant, as well as the fluctuation in lecithin molecular properties and </span>interlayer<span> cation content in the organoclay were evaluated. According to the experimental results, the conformation of lecithin in the organoclay interlayer space<span> undergoes a transition from flat-lying layer to a tilted paraffin-type-bilayer. This phenomenon happens for both pH but, interestingly, follows two different mechanisms. It can be observed that the cations content decreased during the addition of lecithin at pH = 1.0, suggesting that the surfactant intercalated into the interlayer space through cation exchange. On the contrary at pH = 9.0, the zwitterionic nature of lecithin allowed its intercalation in the interlayer space via ion-dipole interactions with the cations. Compared with the organoclay prepared at pH = 1.0, the organoclay prepared at pH = 9.0 also exhibited weaker hydrophobicity, clearly reflecting the difference in the interlayer conformation.</span></span></span></p></div>","PeriodicalId":245,"journal":{"name":"Applied Clay Science","volume":"244 ","pages":"Article 107079"},"PeriodicalIF":5.3000,"publicationDate":"2023-08-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Applied Clay Science","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0169131723002661","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"CHEMISTRY, PHYSICAL","Score":null,"Total":0}
引用次数: 0
Abstract
A series of organoclays were synthesized by modifying bentonite with lecithin under two pH reaction solutions, one acid and one basic. The products prepared using various surfactant concentrations (0.2–5.0CEC) were characterized by multiple experimental techniques. The conformational arrangement of the loaded surfactant, as well as the fluctuation in lecithin molecular properties and interlayer cation content in the organoclay were evaluated. According to the experimental results, the conformation of lecithin in the organoclay interlayer space undergoes a transition from flat-lying layer to a tilted paraffin-type-bilayer. This phenomenon happens for both pH but, interestingly, follows two different mechanisms. It can be observed that the cations content decreased during the addition of lecithin at pH = 1.0, suggesting that the surfactant intercalated into the interlayer space through cation exchange. On the contrary at pH = 9.0, the zwitterionic nature of lecithin allowed its intercalation in the interlayer space via ion-dipole interactions with the cations. Compared with the organoclay prepared at pH = 1.0, the organoclay prepared at pH = 9.0 also exhibited weaker hydrophobicity, clearly reflecting the difference in the interlayer conformation.
期刊介绍:
Applied Clay Science aims to be an international journal attracting high quality scientific papers on clays and clay minerals, including research papers, reviews, and technical notes. The journal covers typical subjects of Fundamental and Applied Clay Science such as:
• Synthesis and purification
• Structural, crystallographic and mineralogical properties of clays and clay minerals
• Thermal properties of clays and clay minerals
• Physico-chemical properties including i) surface and interface properties; ii) thermodynamic properties; iii) mechanical properties
• Interaction with water, with polar and apolar molecules
• Colloidal properties and rheology
• Adsorption, Intercalation, Ionic exchange
• Genesis and deposits of clay minerals
• Geology and geochemistry of clays
• Modification of clays and clay minerals properties by thermal and physical treatments
• Modification by chemical treatments with organic and inorganic molecules(organoclays, pillared clays)
• Modification by biological microorganisms. etc...