Reduction of iron (III) and humic substances plays a major role in anaerobic respiration in an Arctic peat soil

Author:

Lipson David A.,Jha Mony,Raab Theodore K.,Oechel Walter C.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference61 articles.

1. Topdown control of microbial activity and biomass in an Arctic soil ecosystem;Allen;Environ. Microbiol.,2009

2. Total soluble Fe in soil solutions of chemically different soils;Ammari;Geoderma,2006

3. Standardized general method for the determination of iron with 1,10-phenanthroline;Analytical Methods Committee;Analyst,1978

4. Colorimetric determination of oxidizable carbon in acid soil solutions;Bartlett;Soil Sci. Soc. Am. J.,1988

5. Carbon pools and accumulation rates in an age-series of soils in drained thaw-lake basins, Arctic Alaska;Bockheim;Soil Sci. Soc. Am. J.,2004

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