Rare Earth Element Distributions and Trends in Natural Waters with a Focus on Groundwater

被引:199
作者
Noack, Clinton W. [1 ,2 ]
Dzombak, David A. [2 ]
Karamalidis, Athanasios K. [1 ,2 ]
机构
[1] Reg Univ Alliance, Natl Energy Technol Lab, Pittsburgh, PA 15236 USA
[2] Carnegie Mellon Univ, Dept Civil & Environm Engn, Pittsburgh, PA 15213 USA
关键词
PLASMA-MASS SPECTROMETRY; YELLOWSTONE-NATIONAL-PARK; RICH AQUITARD SEQUENCE; ACID-MINE DRAINAGE; TERRESTRIAL WATERS; COAL-MINE; GEOCHEMICAL INTERPRETATION; COMPLEXATION BEHAVIOR; AQUEOUS GEOCHEMISTRY; INORGANIC COMPLEXES;
D O I
10.1021/es4053895
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Systematically varying properties and reactivities have led to focused research of the environmental forensic capabilities of rare earth elements (REE). Increasing anthropogenic inputs to natural systems may permanently alter the natural signatures of PEE, motivating characterization of natural REE variability. We compiled and analyzed reported dissolved REE concentration data over a wide range of natural water types (ground-, ocean, river, and lake water) and groundwater chemistries (e.g., fresh, brine, and acidic) with the goal of quantifying the extent of natural REE variability, especially for groundwater systems. Quantitative challenges presented by censored data were addressed with nonparametric distributions and regressions. Reported measurements of REE in natural waters range over nearly 10 orders of magnitude, though the majority of measurements are within 2-4 orders of magnitude, and are highly correlated with one another. Few global correlations exist among dissolved abundance and bulk solution properties in groundwater, indicating the complex nature of source-sink terms and the need for care when comparing results between studies. This collection, homogenization, and analysis of a disparate literature facilitates interstudy comparison and provides insight into the wide range of variables that influence REE geochemistry.
引用
收藏
页码:4317 / 4326
页数:10
相关论文
共 135 条
[1]   Rare earth elements in seawater: Particle association, shale-normalization, and Ce oxidation [J].
Alibo, DS ;
Nozaki, Y .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1999, 63 (3-4) :363-372
[2]  
[Anonymous], ENG COMPUT
[3]  
[Anonymous], 2012, R LANG ENV STAT COMP
[4]  
[Anonymous], P 16 IEEE INT C EM T
[5]   Prediction of Rare Earth Elements in Neutral Alkaline Mine Drainage from Razi Coal Mine, Golestan Province, Northeast Iran, Using General Regression Neural Network [J].
Ardejanii, Faramarz Doulati ;
Rooki, Reza ;
Shokri, Behshad Jodieri ;
Kish, Teimour Eslam ;
Aryafar, Ahmad ;
Tourani, Pourya .
JOURNAL OF ENVIRONMENTAL ENGINEERING, 2013, 139 (06) :896-907
[6]   Distribution of rare earth elements in anionic, cationic and particulate fractions in boreal humus-rich streams affected by acid sulphate soils [J].
Åström, M ;
Corin, N .
WATER RESEARCH, 2003, 37 (02) :273-280
[7]   Anthropogenic origin of positive gadolinium anomalies in river waters [J].
Bau, M ;
Dulski, P .
EARTH AND PLANETARY SCIENCE LETTERS, 1996, 143 (1-4) :245-255
[8]   Yttrium and lanthanides in eastern Mediterranean seawater and their fractionation during redox-cycling [J].
Bau, M ;
Moller, P ;
Dulski, P .
MARINE CHEMISTRY, 1997, 56 (1-2) :123-131
[9]   Produced water in the Western United States: Geographical distribution, occurrence, and composition [J].
Benko, Katie L. ;
Drewes, Joerg E. .
ENVIRONMENTAL ENGINEERING SCIENCE, 2008, 25 (02) :239-246
[10]   CO2 Sequestration in Deep Sedimentary Formations [J].
Benson, Sally M. ;
Cole, David R. .
ELEMENTS, 2008, 4 (05) :325-331