Refining the site conceptual model at a former uranium mill site in Riverton, Wyoming, USA

被引:30
作者
Dam, William L. [1 ]
Campbell, Sam [2 ]
Johnson, Raymond H. [2 ]
Looney, Brian B. [3 ]
Denham, Miles E. [3 ]
Eddy-Dilek, Carol A. [3 ]
Babits, Steven J. [4 ]
机构
[1] US DOE, Off Legacy Management, Grand Junction, CO 81503 USA
[2] Stoller Newport News Nucl Inc, Grand Junction, CO 81503 USA
[3] US DOE, Savannah River Natl Lab, Off Environm Management, Ctr Sustainable Groundwater & Soil Solut, Aiken, SC 29808 USA
[4] Shoshone & Arapaho Tribes, Lander, WY 82520 USA
关键词
Conceptual site models; Uranium; Unsaturated zone; Groundwater contamination; River flooding; Evaporite mineral deposits; GROUNDWATER CONTAMINATION; TAILINGS PILE; MIXING MODEL;
D O I
10.1007/s12665-015-4706-y
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Milling activities at a former uranium mill site near Riverton, Wyoming, USA, contaminated the shallow groundwater beneath and downgradient of the site. Although the mill operated for < 6 years (1958-1963), its impact remains an environmental liability. Groundwater modeling predicted that natural flushing would achieve compliance with applicable groundwater protection standards by the year 2098. A decade of groundwater monitoring indicated that contaminant concentrations were declining steadily, which confirmed the conceptual site model (CSM). However, local flooding in 2010 mobilized contaminants that migrated downgradient from the Riverton site and resulted in a dramatic increase in groundwater contaminant concentrations. This observation indicated that the original CSM was inadequate to explain site conditions and needed to be refined. In response to the new observations after the flood, a collaborative investigation to better understand site conditions and processes commenced. This investigation included installing 103 boreholes to collect soil and groundwater samples, sampling and analysis of evaporite minerals along the bank of the Little Wind River, an analysis of evapotranspiration in the shallow aquifer, and sampling naturally organic-rich sediments near groundwater discharge areas. The enhanced characterization revealed that the existing CSM did not account for high uranium concentrations in groundwater remaining on the former mill site and groundwater plume stagnation near the Little Wind River. Observations from the flood and subsequent investigations indicate that additional characterization is still needed to continue refining the CSM and determine the viability of the natural flushing compliance strategy. Additional sampling, analysis, and testing of soil and groundwater are necessary to investigate secondary contaminant sources, mobilization of contaminants during floods, geochemical processes, contaminant plume stagnation, distribution of evaporite minerals and organic-rich sediments, and mechanisms and rates of contaminant transfer from soil to groundwater. Future data collection will be used to continually revise the CSM and evaluate the compliance strategy at the site.
引用
收藏
页码:7255 / 7265
页数:11
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