My Account: Log In | Join | Renew
Search
Author
Title
Vol.
Issue
Year
1st Page

Abstract

 

This article in JEQ

  1. Vol. 34 No. 6, p. 2208-2216
     
    Received: Jan 26, 2005
    Published: Nov, 2005


    * Corresponding author(s): Fiona.H.Crocker@erdc.usace.army.mil
 View
 Download
 Alerts
 Permissions
 Share

doi:10.2134/jeq2005.0032

Biotic and Abiotic Degradation of CL-20 and RDX in Soils

  1. Fiona H. Crocker *a,
  2. Karen T. Thompsonb,
  3. James E. Szecsodyc and
  4. Herbert L. Fredricksonb
  1. a Analytical Services, Inc., 3532 Manor Dr., Suite 3, Vicksburg, MS 39180
    b U.S. Army Engineer Res. and Dev. Center, CEERD-EP, 3909 Halls Ferry Rd., Vicksburg, MS 39180
    c Pacific Northwest National Lab., P.O. Box 999 K3-61, Richland, WA 99354

Abstract

The caged cyclic nitramine 2,4,6,8,10,12-hexanitro-2,4,6,8,10,12-hexaazaisowurtzitane (CL-20) is a new explosive that has the potential to replace existing military explosives, but little is known about its environmental toxicity, transport, and fate. We quantified and compared the aerobic environmental fate of CL-20 to the widely used cyclic nitramine explosive hexahydro-1,3,5-trinitro-1,3,5-triazine (RDX) in surface and subsurface soil microcosms. Soil-free controls and biologically attenuated soil controls were used to separate abiotic processes from biologically mediated processes. Both abiotic and biological processes significantly degraded CL-20 in all soils examined. Apparent abiotic, first-order degradation rates (k) for CL-20 were not significantly different between soil-free controls (0.018 < k < 0.030 d−1) and biologically attenuated soil controls (0.003 < k < 0.277 d−1). The addition of glucose to biologically active soil microcosms significantly increased CL-20 degradation rates (0.068 < k < 1.22 d−1). Extents of mineralization of 14C–CL-20 to 14CO2 in biologically active soil microcosms were 41.1 to 55.7%, indicating that the CL-20 cage was broken, since all carbons are part of the heterocyclic cage. Under aerobic conditions, abiotic degradation rates of RDX were generally slower (0 < k < 0.032 d−1) than abiotic CL-20 degradation rates. In biologically active soil microcosms amended with glucose aerobic RDX degradation rates varied between 0.010 and 0.474 d−1 Biodegradation was a key factor in determining the environmental fate of RDX, while a combination of biotic and abiotic processes was important with CL-20. Our data suggest that CL-20 should be less recalcitrant than RDX in aerobic soils.

  Please view the pdf by using the Full Text (PDF) link under 'View' to the left.

Copyright © 2005. American Society of Agronomy, Crop Science Society of America, Soil Science SocietyASA, CSSA, SSSA