|
|
|
|||||||||||||||||
| JOURNAL HOME | HELP | CONTACT PUBLISHER | SUBSCRIBE | ARCHIVE | SEARCH | TABLE OF CONTENTS |
SPECIAL SECTION: SAVANNAH RIVER SITE |
a Dep. of Environmental Engineering and Science, Clemson University, L.G. Rich Environmental Research Laboratory, 342 Computer Court, Anderson, SC 29625
b Savannah River National Laboratory, Aiken, SC 29808
Correspondence: * Corresponding author (fredi{at}clemson.edu).
Received for publication 16 March 2006. Improved understanding of flow and radionuclide transport in vadose zone sediments is fundamental to future planning involving radioactive materials. To that end, long-term experiments were conducted at the Savannah River Site (SRS), where a series of lysimeters containing sources of different Pu oxidation states were placed in the shallow subsurface and exposed to the environment for 2 to 11 yr. After the experiments, Pu activity concentrations were measured along vertical cores from the lysimeters. Plutonium distributions were anomalous in naturetransport from oxidized Pu sources was less than expected, and a small fraction of Pu from reduced sources moved more. Studies conducted with these lysimeter sediments indicated that surface-mediated, oxidationreduction (redox) reactions may be responsible for the anomalies. This hypothesis is tested by performing transient Pu transport simulations that include retardation and first-order redox reactions on mineral surfaces within a steady-state flow field. These simulations affirm the consistency of the surface-mediated, redox hypothesis with observed Pu activity profiles below the source. Such profiles are captured well by a steady-state, net downward flow model. The redox model explains how Pu(V/VI) sources release activity that moves downward more slowly than expected, and how Pu(III/IV) sources result in a small fraction of activity that moves downward farther than expected. The calibrated parameter values were robust and well defined throughout all simulations. Approximate retardation factors for Pu(V/VI) were 15, and for Pu(III/IV) were 10,000. For these values, ko averaged 2.4 x 107 h1; kr averaged 7.1 x 104 h1 (standard deviations are 1.6 x 107 h1 and 1.6 x 104 h1 respectively).
Abbreviations: INL, Idaho National Lab Puo, oxidized class of Pu Pur, reduced class of Pu SRS, Savannah River Site.
This article has been cited by other articles:
![]() |
D. I. Demirkanli, F. J. Molz, D. I. Kaplan, and R. A. Fjeld Soil-Root Interactions Controlling Upward Plutonium Transport in Variably Saturated Soils Vadose Zone J., July 7, 2009; 8(3): 574 - 585. [Abstract] [Full Text] [PDF] |
||||
![]() |
D. I. Demirkanli, F. J. Molz, D. I. Kaplan, and R. A. Fjeld A Fully Transient Model for Long-Term Plutonium Transport in the Savannah River Site Vadose Zone: Root Water Uptake Vadose Zone J., August 13, 2008; 7(3): 1099 - 1109. [Abstract] [Full Text] [PDF] |
||||
![]() |
J. C. Seaman, B. B. Looney, and M. K. Harris Research in Support of Remediation Activities at the Savannah River Site Vadose Zone J., May 17, 2007; 6(2): 316 - 326. [Abstract] [Full Text] [PDF] |
||||
| JOURNAL HOME | HELP | CONTACT PUBLISHER | SUBSCRIBE | ARCHIVE | SEARCH | TABLE OF CONTENTS |