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Temperature and Microbial Activity Effects on Trace Element Leaching from Metalliferous Peats

Shabnam Qureshia, Brian K. Richards*,a, Murray B. McBrideb, Philippe Baveyeb and Tammo S. Steenhuisa

a Department of Biological and Environmental Engineering, Riley-Robb Hall, Cornell University, Ithaca, NY 14853
b Department of Crop and Soil Sciences, Bradfield Hall, Cornell University, Ithaca, NY 14853



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Fig. 1. Cumulative respiration (mg carbon mineralized per gram peat solids) for both initial and leached M3 and M7 peat soils. Error bars represent ±1 standard deviation.

 


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Fig. 2. Leachate pH as a function of time and incubation temperature. Dashed lines indicate peat soil pH, dotted lines indicate rainfall pH. For this and similar figures, cumulative time (incubation plus leaching) is plotted on the x axis, with the composited Week 3 + 4 sample plotted midway between the Week 3 and 4 leachings.

 


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Fig. 3. Leachate total S, NO3–N, and dissolved organic carbon (DOC) concentrations as a function of time and incubation temperature.

 


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Fig. 4. Leachate Zn, Ni, and As concentrations as a function of time and incubation temperature for M7 acidic peat.

 


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Fig. 5. Leachate Zn, Ni, and As concentrations as a function of time and incubation temperature for M3 neutral peat.

 


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Fig. 6. First cycle leachate concentrations of total S, dissolved organic carbon (DOC), and Zn as a function of initial cumulative respiration. Correlation coefficients (r2) are from linear regressions.

 


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Fig. 7. Leachate Zn concentrations as a function of leachate pH and dissolved organic carbon (DOC) concentration for (a) M7 acidic peat and (b) M3 neutral peat.

 





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Vadose Zone Journal Journal of Plant Registrations
Journal of Natural Resources
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Soil Science Society of America Journal
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