{"title":"地下水流动原理","authors":"Paul A. Bouts","doi":"10.1201/9780203719770-1","DOIUrl":null,"url":null,"abstract":"Hydraulic head is the elevation to which water will naturally rise in a well (a.k.a. “static level). Any well that is not being pumped will do for this, but a well that is created especially for measuring hydraulic head is known as an observation well a monitoring well or a piezometer. For unconfined aquifers the hydraulic head is the same thing as the water table. For confined aquifers it is not.","PeriodicalId":343154,"journal":{"name":"Groundwater and Surface Water Pollution","volume":"77 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2019-01-22","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Principles of Groundwater Flow\",\"authors\":\"Paul A. Bouts\",\"doi\":\"10.1201/9780203719770-1\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Hydraulic head is the elevation to which water will naturally rise in a well (a.k.a. “static level). Any well that is not being pumped will do for this, but a well that is created especially for measuring hydraulic head is known as an observation well a monitoring well or a piezometer. For unconfined aquifers the hydraulic head is the same thing as the water table. For confined aquifers it is not.\",\"PeriodicalId\":343154,\"journal\":{\"name\":\"Groundwater and Surface Water Pollution\",\"volume\":\"77 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2019-01-22\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Groundwater and Surface Water Pollution\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1201/9780203719770-1\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Groundwater and Surface Water Pollution","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1201/9780203719770-1","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Hydraulic head is the elevation to which water will naturally rise in a well (a.k.a. “static level). Any well that is not being pumped will do for this, but a well that is created especially for measuring hydraulic head is known as an observation well a monitoring well or a piezometer. For unconfined aquifers the hydraulic head is the same thing as the water table. For confined aquifers it is not.
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