Decay-series disequilibrium study of in-situ, long-term radionuclide transport in water-rock systems

Shangde Luo; K. U. Teh-Lung; Robert Roback; Micheal Murrell; Travis L. Mcling

Decay-series disequilibrium study of in-situ, long-term radionuclide transport in water-rock systems

Shangde Luo, K. U. Teh-Lung, Robert Roback, Micheal Murrell, Travis L. Mcling

Department of Earth Sciences

Research output: Contribution to journal › Conference article › peer-review

Abstract

Uranium and thorium-series disequilibrium in nature permits the determination of many in-situ physico-chemical, geologic and hydrologic variables that control the long-term migration of radionuclides in geologic systems. It also provides site-specific, natural analog information valuable to the assessment of geologic disposal of nuclear wastes. In this study, a model that relates the decay-series radioisotope distributions among solution, sorbed and solid phases in water-rock systems to processes of water transport, sorption-desorption, dissolution-precipitation, radioactive ingrowth-decay, and α recoil is discussed and applied to a basaltic aquifer at the Idaho National Engineering and Environmental Laboratory (INEEL), Idaho.

Original language	English
Pages (from-to)	217-224
Number of pages	8
Journal	Materials Research Society Symposium - Proceedings
Volume	608
Publication status	Published - 2000 Dec 1
Event	Scientific Basis for Nuclear Waste Management XXIII - Boston, MA, USA Duration: 1999 Nov 29 → 1999 Dec 2

All Science Journal Classification (ASJC) codes

Materials Science(all)
Condensed Matter Physics
Mechanics of Materials
Mechanical Engineering

Fingerprint Dive into the research topics of 'Decay-series disequilibrium study of in-situ, long-term radionuclide transport in water-rock systems'. Together they form a unique fingerprint.

Cite this

@article{bf738d357f9a46348152a2b021cb4f96,

title = "Decay-series disequilibrium study of in-situ, long-term radionuclide transport in water-rock systems",

abstract = "Uranium and thorium-series disequilibrium in nature permits the determination of many in-situ physico-chemical, geologic and hydrologic variables that control the long-term migration of radionuclides in geologic systems. It also provides site-specific, natural analog information valuable to the assessment of geologic disposal of nuclear wastes. In this study, a model that relates the decay-series radioisotope distributions among solution, sorbed and solid phases in water-rock systems to processes of water transport, sorption-desorption, dissolution-precipitation, radioactive ingrowth-decay, and α recoil is discussed and applied to a basaltic aquifer at the Idaho National Engineering and Environmental Laboratory (INEEL), Idaho.",

author = "Shangde Luo and Teh-Lung, {K. U.} and Robert Roback and Micheal Murrell and Mcling, {Travis L.}",

year = "2000",

month = dec,

day = "1",

language = "English",

volume = "608",

pages = "217--224",

journal = "Materials Research Society Symposium - Proceedings",

issn = "0272-9172",

publisher = "Materials Research Society",

note = "Scientific Basis for Nuclear Waste Management XXIII ; Conference date: 29-11-1999 Through 02-12-1999",

}

TY - JOUR

T1 - Decay-series disequilibrium study of in-situ, long-term radionuclide transport in water-rock systems

AU - Luo, Shangde

AU - Teh-Lung, K. U.

AU - Roback, Robert

AU - Murrell, Micheal

AU - Mcling, Travis L.

PY - 2000/12/1

Y1 - 2000/12/1

N2 - Uranium and thorium-series disequilibrium in nature permits the determination of many in-situ physico-chemical, geologic and hydrologic variables that control the long-term migration of radionuclides in geologic systems. It also provides site-specific, natural analog information valuable to the assessment of geologic disposal of nuclear wastes. In this study, a model that relates the decay-series radioisotope distributions among solution, sorbed and solid phases in water-rock systems to processes of water transport, sorption-desorption, dissolution-precipitation, radioactive ingrowth-decay, and α recoil is discussed and applied to a basaltic aquifer at the Idaho National Engineering and Environmental Laboratory (INEEL), Idaho.

AB - Uranium and thorium-series disequilibrium in nature permits the determination of many in-situ physico-chemical, geologic and hydrologic variables that control the long-term migration of radionuclides in geologic systems. It also provides site-specific, natural analog information valuable to the assessment of geologic disposal of nuclear wastes. In this study, a model that relates the decay-series radioisotope distributions among solution, sorbed and solid phases in water-rock systems to processes of water transport, sorption-desorption, dissolution-precipitation, radioactive ingrowth-decay, and α recoil is discussed and applied to a basaltic aquifer at the Idaho National Engineering and Environmental Laboratory (INEEL), Idaho.

UR - http://www.scopus.com/inward/record.url?scp=0034516818&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=0034516818&partnerID=8YFLogxK

M3 - Conference article

AN - SCOPUS:0034516818

VL - 608

SP - 217

EP - 224

JO - Materials Research Society Symposium - Proceedings

JF - Materials Research Society Symposium - Proceedings

SN - 0272-9172

T2 - Scientific Basis for Nuclear Waste Management XXIII

Y2 - 29 November 1999 through 2 December 1999

ER -