{"title":"高岭土的表面电荷","authors":"T.M. Herrington, A.Q. Clarke, J.C. Watts","doi":"10.1016/0166-6622(92)80200-L","DOIUrl":null,"url":null,"abstract":"<div><p>The variation of surface charge with pH for pure and commercially available kaolinite samples was investigated by ion adsorption and potentiometric titration. The contribution of two distinct sources of charge can be identified. The results help to explain previous work on the ion exchange capacity of kaolinite.</p></div>","PeriodicalId":10488,"journal":{"name":"Colloids and Surfaces","volume":null,"pages":null},"PeriodicalIF":0.0000,"publicationDate":"1992-11-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/0166-6622(92)80200-L","citationCount":"74","resultStr":"{\"title\":\"The surface charge of kaolin\",\"authors\":\"T.M. Herrington, A.Q. Clarke, J.C. Watts\",\"doi\":\"10.1016/0166-6622(92)80200-L\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>The variation of surface charge with pH for pure and commercially available kaolinite samples was investigated by ion adsorption and potentiometric titration. The contribution of two distinct sources of charge can be identified. The results help to explain previous work on the ion exchange capacity of kaolinite.</p></div>\",\"PeriodicalId\":10488,\"journal\":{\"name\":\"Colloids and Surfaces\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1992-11-11\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1016/0166-6622(92)80200-L\",\"citationCount\":\"74\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Colloids and Surfaces\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/016666229280200L\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Colloids and Surfaces","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/016666229280200L","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
The variation of surface charge with pH for pure and commercially available kaolinite samples was investigated by ion adsorption and potentiometric titration. The contribution of two distinct sources of charge can be identified. The results help to explain previous work on the ion exchange capacity of kaolinite.
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