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Titlebook: Environmental Tracers in Subsurface Hydrology; Peter G. Cook,Andrew L. Herczeg Book 2000 Springer Science+Business Media New York 2000 Gro

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发表于 2025-3-21 18:55:07 | 显示全部楼层 |阅读模式
书目名称Environmental Tracers in Subsurface Hydrology
编辑Peter G. Cook,Andrew L. Herczeg
视频video
图书封面Titlebook: Environmental Tracers in Subsurface Hydrology;  Peter G. Cook,Andrew L. Herczeg Book 2000 Springer Science+Business Media New York 2000 Gro
描述.Environmental Tracers in Subsurface Hydrology. synthesizesthe research of specialists into a comprehensive review of theapplication of environmental tracers to the study of soil water andgroundwater flow. The book includes chapters which cover ionictracers, noble gases, chlorofluorocarbons, tritium, chlorine-36,oxygen-18, deuterium, and isotopes of carbon, strontium, sulphur andnitrogen. Applications of the tracers include the estimation ofvertical and horizontal groundwater velocities, groundwater rechargerates, inter-aquifer leakage and mixing processes, chemical processesand palaeohydrology. Practicing hydrologists, soil physicists andhydrology professors and students will find the book to be a valuablesupport in their work.
出版日期Book 2000
关键词Groundwater; environment; hydrology; mixing; spheric; hydrogeology; terrestrial pollution
版次1
doihttps://doi.org/10.1007/978-1-4615-4557-6
isbn_softcover978-1-4613-7057-4
isbn_ebook978-1-4615-4557-6
copyrightSpringer Science+Business Media New York 2000
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发表于 2025-3-21 23:06:12 | 显示全部楼层
https://doi.org/10.1007/978-1-4615-4557-6Groundwater; environment; hydrology; mixing; spheric; hydrogeology; terrestrial pollution
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978-1-4613-7057-4Springer Science+Business Media New York 2000
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Biotechnologies for Water Treatmentogy’by analogy with the dating of solid materials known as geochronology.) Information on soil water and groundwater age enables timescales for a range of subsurface processes to be determined. For example, ‘groundwater stratigraphy’is used increasingly to decipher past recharge rates and conditions
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Xianguang Yang,Long Wen,Baojun Liell as isotopic ratios of the water molecule. The subsurface accepts water at variable rates of movement through the soil, via the unsaturated zone, to the water table. At this stage the groundwater composition undergoes significant modification due to two major processes: an increase in the concent
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