{"title":"不断上升的潮湿","authors":"G. Mason","doi":"10.1016/0007-3628(74)90021-8","DOIUrl":null,"url":null,"abstract":"<div><p>A model is proposed where the rate at which ground-water is raised by capillarity equals the rate of evaporation. An examination of the constants indicates that the most likely cause of the wet-line rising with time is the leaching of the soluble lime from the mortar with a conseqent increase in its permeability</p></div>","PeriodicalId":9442,"journal":{"name":"Building Science","volume":"9 3","pages":"Pages 227-231"},"PeriodicalIF":0.0000,"publicationDate":"1974-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/0007-3628(74)90021-8","citationCount":"0","resultStr":"{\"title\":\"Rising damp\",\"authors\":\"G. Mason\",\"doi\":\"10.1016/0007-3628(74)90021-8\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>A model is proposed where the rate at which ground-water is raised by capillarity equals the rate of evaporation. An examination of the constants indicates that the most likely cause of the wet-line rising with time is the leaching of the soluble lime from the mortar with a conseqent increase in its permeability</p></div>\",\"PeriodicalId\":9442,\"journal\":{\"name\":\"Building Science\",\"volume\":\"9 3\",\"pages\":\"Pages 227-231\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1974-09-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1016/0007-3628(74)90021-8\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Building Science\",\"FirstCategoryId\":\"1087\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/0007362874900218\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Building Science","FirstCategoryId":"1087","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/0007362874900218","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
A model is proposed where the rate at which ground-water is raised by capillarity equals the rate of evaporation. An examination of the constants indicates that the most likely cause of the wet-line rising with time is the leaching of the soluble lime from the mortar with a conseqent increase in its permeability
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