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RDX Loss in a Surface Soil under Saturated and Well Drained Conditions

D. B. Ringelberg*, C. M. Reynolds, M. E. Walsh and T. F. Jenkins

U.S. Army ERDC-CRREL, 72 Lyme Rd., Hanover, NH 03755



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Fig. 1. Plot of ln (C/C0) vs. time (h) for RDX in Fort Greely surface soil under (A) unsaturated and (B) saturated conditions. Acetonitrile was added to a final concentration (volume basis) of 0 µL L-1 (0%), 1000 µL L-1 (0.1%), and 10 000 µL L-1 (1%).

 


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Fig. 2. RDX concentrations (mg L-1) in (A) unsaturated and (B) saturated Ft. Greely surface soils. Soils were incubated at room temperature (28°C) in the dark for 5 wk. Control soils were autoclaved (120°C for 20 min) three consecutive times before incubation. Acetonitrile was added to a final concentration (volume basis) of 0 µL L-1 (0%), 1000 µL L-1 (0.1%), and 10 000 µL L-1 (1%).

 


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Fig. 3. The MNX, DNX, and TNX concentrations (mg L-1) in saturated Ft. Greely surface soils. Soils were incubated at room temperature (28°C) in the dark for 5 wk. Control (Ctrl) soils were autoclaved (120°C for 20 min) three consecutive times before incubation. Acetonitrile was added to a final concentration (volume basis) of 0 µL L-1 (0%), 1000 µL L-1 (0.1%), and 10 000 µL L-1 (1%).

 





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