Black Carbon Increases Cation Exchange Capacity in Soils
Top Cited Papers
- 1 September 2006
- journal article
- biogeochemical processes
- Published by Wiley in Soil Science Society of America Journal
- Vol. 70 (5) , 1719-1730
- https://doi.org/10.2136/sssaj2005.0383
Abstract
Black Carbon (BC) may significantly affect nutrient retention and play a key role in a wide range of biogeochemical processes in soils, especially for nutrient cycling. Anthrosols from the Brazilian Amazon (ages between 600 and 8700 yr BP) with high contents of biomass‐derived BC had greater potential cation exchange capacity (CEC measured at pH 7) per unit organic C than adjacent soils with low BC contents. Synchrotron‐based near edge X‐ray absorption fine structure (NEXAFS) spectroscopy coupled with scanning transmission X‐ray microscopy (STXM) techniques explained the source of the higher surface charge of BC compared with non‐BC by mapping cross‐sectional areas of BC particles with diameters of 10 to 50 μm for C forms. The largest cross‐sectional areas consisted of highly aromatic or only slightly oxidized organic C most likely originating from the BC itself with a characteristic peak at 286.1 eV, which could not be found in humic substance extracts, bacteria or fungi. Oxidation significantly increased from the core of BC particles to their surfaces as shown by the ratio of carboxyl‐C/aromatic‐C. Spotted and non‐continuous distribution patterns of highly oxidized C functional groups with distinctly different chemical signatures on BC particle surfaces (peak shift at 286.1 eV to a higher energy of 286.7 eV) indicated that non‐BC may be adsorbed on the surfaces of BC particles creating highly oxidized surface. As a consequence of both oxidation of the BC particles themselves and adsorption of organic matter to BC surfaces, the charge density (potential CEC per unit surface area) was greater in BC‐rich Anthrosols than adjacent soils. Additionally, a high specific surface area was attributable to the presence of BC, which may contribute to the high CEC found in soils that are rich in BC.Keywords
Funding Information
- Division of Environmental Biology of the National Science Foundation (DEB-0425995)
This publication has 50 references indexed in Scilit:
- Near‐edge X‐ray absorption fine structure (NEXAFS) spectroscopy for mapping nano‐scale distribution of organic carbon forms in soil: Application to black carbon particlesGlobal Biogeochemical Cycles, 2005
- Changes in clay-associated organic matter quality in a C depletion sequence as measured by differential thermal analysesPublished by Elsevier ,2005
- Morphological and chemical properties of black carbon in physical soil fractions as revealed by scanning electron microscopy and energy-dispersive X-ray spectroscopyPublished by Elsevier ,2005
- Carbon isotope geochemistry and nanomorphology of soil black carbon: Black chernozemic soils in central Europe originate from ancient biomass burningGlobal Biogeochemical Cycles, 2002
- Pedogenesis and pre-Colombian land use of “Terra Preta Anthrosols” (“Indian black earth”) of Western AmazoniaGeoderma, 2002
- X-Ray Absorption Spectroscopy Investigation of the Activation Process of Raney Nickel CatalystsJournal of Catalysis, 2000
- Estimation of charcoal (char) in soilsCommunications in Soil Science and Plant Analysis, 1999
- Black carbon formation by savanna fires: Measurements and implications for the global carbon cycleJournal of Geophysical Research: Atmospheres, 1996
- Carbon K-shell excitation spectra of linear and branched alkanesJournal of Electron Spectroscopy and Related Phenomena, 1987
- A Mechanically Controlled Variable Rate Leaching DeviceSoil Science Society of America Journal, 1977