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- W4315692541 abstract "The transport of dissolved chemical mass, or solutes, in groundwater comprises a significant component of many geologic processes. Many forms of metasomatism and diagenesis, for example, are driven by chemical reactions whose components are supplied by flowing groundwater. In addition, accumulations of hydrocarbons and metal-rich ore deposits are greatly controlled by the transport of chemicals by flowing groundwater. Groundwater also plays a role in the formation and dissolution of evaporite deposits. Detailed examples of how groundwater affects metasomatism, diagenesis, evaporites, and the formation of ore and hydrocarbon deposits will be discussed in later chapters. In this chapter we introduce the basic principles of solute transport in groundwater. As the chapter progresses we discuss the governing equations, techniques for solving these equations, variable-density flow and transport, multiconstituent reactive transport, ultrafiltration and, finally, the role of microbes." @default.
- W4315692541 created "2023-01-12" @default.
- W4315692541 date "2006-05-04" @default.
- W4315692541 modified "2023-09-23" @default.
- W4315692541 title "Solute transport" @default.
- W4315692541 doi "https://doi.org/10.1017/9780511807855.004" @default.
- W4315692541 hasPublicationYear "2006" @default.
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