scholarly journals A New Paradigm for Long Term Monitoring at the F-Area Seepage Basins, Savannah River Site

2019 ◽  
Author(s):  
Miles E. Denham ◽  
Carol A. Eddy-Dilek ◽  
Haruko M. Wainwright ◽  
Jeffrey Thibault ◽  
Kevin Boerstler
2007 ◽  
Vol 6 (2) ◽  
pp. 344-353 ◽  
Author(s):  
Deniz I. Demirkanli ◽  
Fred J. Molz ◽  
Daniel I. Kaplan ◽  
Robert A. Fjeld ◽  
Steven M. Serkiz

2010 ◽  
Vol 16 (3) ◽  
pp. 224
Author(s):  
Joanne M. Hoare

In their book Effective Ecological Monitoring, David Lindenmayer and Gene Likens set out to demonstrate the importance of long-term ecological monitoring programmes, as well as presenting what they propose to be a new paradigm, ?adaptive monitoring?. In a brief introduction, they set up a framework for discussing ecological monitoring by arguing that monitoring can be categorized into one of three main types, curiosity-driven (passive) monitoring, mandated monitoring or question-driven monitoring, the latter of which they strongly suggest has the most merit. The book is then structured around three main chapters, ?Why monitoring fails?, ?What makes long-term monitoring effective?? and ?The problematic, the effective and the ugly ? some case studies?, and rounded off with a concluding chapter.


2002 ◽  
Vol 713 ◽  
Author(s):  
May Nyman ◽  
James L. Krumhansl ◽  
Carlos Jove-Colon ◽  
Pengchu Zhang ◽  
Tina M. Nenoff ◽  
...  

ABSTRACTIE-911 is a bound form of cystalline silicotitanate (CST) that was extensively tested for removing 137Cs from the Savannah River Site (SRS) tank wastes. In some simulant tests, column plugging incidents were observed, which led to thorough investigations to determine the causes and to develop protocols to avoid future plugging incidents. A related problem was the apparent decrease in Cs scavenging capability in some long-term tests. Our studies revealed that the interaction of IE-911 with the highly basic, high ionic strength, SRS average salt simulant could result in precipitation of; 1) poorly crystalline Nb-oxide, or 2) aluminosilicate zeolitic phases. The source for the Nb-oxide precipitate was determined to be a minor impurity phase that is a byproduct of CST manufacturing. The mechanisms of dissolution and re-precipitation of this phase in column pretreatment solution were investigated, and a protocol to rid IE-911 of this impurity was devised. The source material for the aluminosilicate zeolite precipitate was determined to be predominantly from the waste solution rather than the IE-911. Solubility experiments coupled with a thermodynamic analysis provided a protocol to predict when aluminosilicate precipitation will and will not occur. Finally, it was also established that aluminosilicate precipitation on the surfaces of the IE-911 granules could also account for an apparent decrease in equilibrium Kd and decrease in kinetics of Cs sorption.


2008 ◽  
Vol 7 (3) ◽  
pp. 1099-1109 ◽  
Author(s):  
Deniz I. Demirkanli ◽  
Fred J. Molz ◽  
Daniel I. Kaplan ◽  
Robert A. Fjeld

2009 ◽  
Vol 8 (2) ◽  
pp. 530-530
Author(s):  
Deniz I. Demirkanli ◽  
Fred J. Molz ◽  
Daniel I. Kaplan ◽  
Robert A. Fjeld

2015 ◽  
Vol 49 (3) ◽  
pp. 1286-1293 ◽  
Author(s):  
Christopher R. Armstrong ◽  
Patterson R. Nuessle ◽  
Heather A. Brant ◽  
Gregory Hall ◽  
Justin E. Halverson ◽  
...  

2011 ◽  
Vol 77 (6) ◽  
pp. 2153-2160 ◽  
Author(s):  
Hsiu-Ping Li ◽  
Robin Brinkmeyer ◽  
Whitney L. Jones ◽  
Saijin Zhang ◽  
Chen Xu ◽  
...  

ABSTRACT129I is of major concern because of its mobility in the environment, excessive inventory, toxicity (it accumulates in the thyroid), and long half-life (∼16 million years). The aim of this study was to determine if bacteria from a129I-contaminated oxic aquifer at the F area of the U.S. Department of Energy's Savannah River Site, SC, could accumulate iodide at environmentally relevant concentrations (0.1 μM I−). Iodide accumulation capability was found in 3 out of 136 aerobic bacterial strains isolated from the F area that were closely related toStreptomyces/Kitasatosporaspp.,Bacillus mycoides, andRalstonia/Cupriavidusspp. Two previously described iodide-accumulating marine strains, aFlexibacter aggregansstrain and anArenibacter troitsensisstrain, accumulated 2 to 50% total iodide (0.1 μM), whereas the F-area strains accumulated just 0.2 to 2.0%. Iodide accumulation by FA-30 was stimulated by the addition of H2O2, was not inhibited by chloride ions (27 mM), did not exhibit substrate saturation kinetics with regard to I−concentration (up to 10 μM I−), and increased at pH values of <6. Overall, the data indicate that I−accumulation likely results from electrophilic substitution of cellular organic molecules. This study demonstrates that readily culturable, aerobic bacteria of the F-area aquifer do not accumulate significant amounts of iodide; however, this mechanism may contribute to the long-term fate and transport of129I and to the biogeochemical cycling of iodine over geologic time.


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