U isotopic fractionation - a process characterising groundwater systems

Juhani Suksi; Kari Rasilainen; Nuria Marcos

doi:10.1007/3-540-28367-6_69

U isotopic fractionation - a process characterising groundwater systems

Juhani Suksi, Kari Rasilainen, Nuria Marcos

Research output: Chapter in Book/Report/Conference proceeding › Conference article in proceedings › Scientific › peer-review

Abstract

The activity of ²³⁴U relative to ²³⁸U (AR) in groundwaters is controlled by isotope fractionation in water-rock interface. The fractionation is controlled by redox-conditions and rock-groundwater contact time. The measured ARs form thus an important source of information and offer an effective tool to characterise groundwater systems along with other hydrochemical data. The purpose of this paper is to elucidate the link between ARs and groundwater conditions. The paper considers the formation of AR in groundwaters and examines measured data from several study sites in the Fennoscandian Shield.

Original language	English
Title of host publication	Uranium in the Environment
Subtitle of host publication	Mining Impact and Consequences
Editors	Broder Merkel, Andrea Häsche-Berger
Publisher	Springer
Pages	683-690
ISBN (Electronic)	978-3-540-28367-6
ISBN (Print)	978-3-540-28363-8
DOIs	https://doi.org/10.1007/3-540-28367-6_69
Publication status	Published - 2005
MoE publication type	A4 Article in a conference publication
Event	Uranium Mining and Hydrogeology Congress - Freiberg, Germany Duration: 11 Sep 2005 → 16 Sep 2005

Conference

Conference	Uranium Mining and Hydrogeology Congress
Country	Germany
City	Freiberg
Period	11/09/05 → 16/09/05

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Suksi, J., Rasilainen, K., & Marcos, N. (2005). U isotopic fractionation - a process characterising groundwater systems. In B. Merkel, & A. Häsche-Berger (Eds.), Uranium in the Environment: Mining Impact and Consequences (pp. 683-690). Springer. https://doi.org/10.1007/3-540-28367-6_69

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title = "U isotopic fractionation - a process characterising groundwater systems",

abstract = "The activity of 234U relative to 238U (AR) in groundwaters is controlled by isotope fractionation in water-rock interface. The fractionation is controlled by redox-conditions and rock-groundwater contact time. The measured ARs form thus an important source of information and offer an effective tool to characterise groundwater systems along with other hydrochemical data. The purpose of this paper is to elucidate the link between ARs and groundwater conditions. The paper considers the formation of AR in groundwaters and examines measured data from several study sites in the Fennoscandian Shield.",

author = "Juhani Suksi and Kari Rasilainen and Nuria Marcos",

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language = "English",

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editor = "Broder Merkel and Andrea H{\"a}sche-Berger",

booktitle = "Uranium in the Environment",

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address = "Germany",

note = "Uranium Mining and Hydrogeology Congress ; Conference date: 11-09-2005 Through 16-09-2005",

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U isotopic fractionation - a process characterising groundwater systems. / Suksi, Juhani; Rasilainen, Kari; Marcos, Nuria.

Uranium in the Environment: Mining Impact and Consequences. ed. / Broder Merkel; Andrea Häsche-Berger. Springer, 2005. p. 683-690.

Research output: Chapter in Book/Report/Conference proceeding › Conference article in proceedings › Scientific › peer-review

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AU - Rasilainen, Kari

AU - Marcos, Nuria

PY - 2005

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N2 - The activity of 234U relative to 238U (AR) in groundwaters is controlled by isotope fractionation in water-rock interface. The fractionation is controlled by redox-conditions and rock-groundwater contact time. The measured ARs form thus an important source of information and offer an effective tool to characterise groundwater systems along with other hydrochemical data. The purpose of this paper is to elucidate the link between ARs and groundwater conditions. The paper considers the formation of AR in groundwaters and examines measured data from several study sites in the Fennoscandian Shield.

AB - The activity of 234U relative to 238U (AR) in groundwaters is controlled by isotope fractionation in water-rock interface. The fractionation is controlled by redox-conditions and rock-groundwater contact time. The measured ARs form thus an important source of information and offer an effective tool to characterise groundwater systems along with other hydrochemical data. The purpose of this paper is to elucidate the link between ARs and groundwater conditions. The paper considers the formation of AR in groundwaters and examines measured data from several study sites in the Fennoscandian Shield.

U2 - 10.1007/3-540-28367-6_69

DO - 10.1007/3-540-28367-6_69

M3 - Conference article in proceedings

SN - 978-3-540-28363-8

SP - 683

EP - 690

BT - Uranium in the Environment

A2 - Merkel, Broder

A2 - Häsche-Berger, Andrea

PB - Springer

T2 - Uranium Mining and Hydrogeology Congress

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10.1007/3-540-28367-6_69