Black carbon increases cation exchange capacity in soils
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 potenti...
| Autor principal: | Liang, Biqing |
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| Outros Autores: | Lehmann, Johannes, Solomon, D., Kinyangi, James M., Grossman, Julie M., O'Neill, Brendan E., Skjemstad, Jan O., Thies, Janice E., Luizão, Flávio Jesus, Petersen, James B., Neves, Eduardo Goés |
| Grau: | Artigo |
| Idioma: | English |
| Publicado em: |
Soil Science Society of America Journal
2020
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| Acesso em linha: |
https://repositorio.inpa.gov.br/handle/1/18729 |
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oai:repositorio:1-18729 |
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oai:repositorio:1-18729 Black carbon increases cation exchange capacity in soils Liang, Biqing Lehmann, Johannes Solomon, D. Kinyangi, James M. Grossman, Julie M. O'Neill, Brendan E. Skjemstad, Jan O. Thies, Janice E. Luizão, Flávio Jesus Petersen, James B. Neves, Eduardo Goés Carbon Ion Exchange Microscopic Examination Ph Effects Positive Ions Spectroscopic Analysis Biogeochemical Processes Black Carbon Cation Exchange Capacity (cec) Scanning Transmission X-ray Microscopy (stxm) Soil Surveys Carbon Ion Exchange Microscopic Examination Ph Effects Positive Ions Soil Surveys Spectroscopic Analysis Biogeochemistry Black Carbon Ion Exchange Organic Carbon Oxidation Soil Nutrient Soil Organic Matter Amazon River Brasil South America Bacteria (microorganisms) Fungi 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. © Soil Science Society of America. 2020-06-15T22:02:46Z 2020-06-15T22:02:46Z 2006 Artigo https://repositorio.inpa.gov.br/handle/1/18729 10.2136/sssaj2005.0383 en Volume 70, Número 5, Pags. 1719-1730 Restrito Soil Science Society of America Journal |
| institution |
Instituto Nacional de Pesquisas da Amazônia - Repositório Institucional |
| collection |
INPA-RI |
| language |
English |
| topic |
Carbon Ion Exchange Microscopic Examination Ph Effects Positive Ions Spectroscopic Analysis Biogeochemical Processes Black Carbon Cation Exchange Capacity (cec) Scanning Transmission X-ray Microscopy (stxm) Soil Surveys Carbon Ion Exchange Microscopic Examination Ph Effects Positive Ions Soil Surveys Spectroscopic Analysis Biogeochemistry Black Carbon Ion Exchange Organic Carbon Oxidation Soil Nutrient Soil Organic Matter Amazon River Brasil South America Bacteria (microorganisms) Fungi |
| spellingShingle |
Carbon Ion Exchange Microscopic Examination Ph Effects Positive Ions Spectroscopic Analysis Biogeochemical Processes Black Carbon Cation Exchange Capacity (cec) Scanning Transmission X-ray Microscopy (stxm) Soil Surveys Carbon Ion Exchange Microscopic Examination Ph Effects Positive Ions Soil Surveys Spectroscopic Analysis Biogeochemistry Black Carbon Ion Exchange Organic Carbon Oxidation Soil Nutrient Soil Organic Matter Amazon River Brasil South America Bacteria (microorganisms) Fungi Liang, Biqing Black carbon increases cation exchange capacity in soils |
| topic_facet |
Carbon Ion Exchange Microscopic Examination Ph Effects Positive Ions Spectroscopic Analysis Biogeochemical Processes Black Carbon Cation Exchange Capacity (cec) Scanning Transmission X-ray Microscopy (stxm) Soil Surveys Carbon Ion Exchange Microscopic Examination Ph Effects Positive Ions Soil Surveys Spectroscopic Analysis Biogeochemistry Black Carbon Ion Exchange Organic Carbon Oxidation Soil Nutrient Soil Organic Matter Amazon River Brasil South America Bacteria (microorganisms) Fungi |
| description |
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. © Soil Science Society of America. |
| format |
Artigo |
| author |
Liang, Biqing |
| author2 |
Lehmann, Johannes Solomon, D. Kinyangi, James M. Grossman, Julie M. O'Neill, Brendan E. Skjemstad, Jan O. Thies, Janice E. Luizão, Flávio Jesus Petersen, James B. Neves, Eduardo Goés |
| author2Str |
Lehmann, Johannes Solomon, D. Kinyangi, James M. Grossman, Julie M. O'Neill, Brendan E. Skjemstad, Jan O. Thies, Janice E. Luizão, Flávio Jesus Petersen, James B. Neves, Eduardo Goés |
| title |
Black carbon increases cation exchange capacity in soils |
| title_short |
Black carbon increases cation exchange capacity in soils |
| title_full |
Black carbon increases cation exchange capacity in soils |
| title_fullStr |
Black carbon increases cation exchange capacity in soils |
| title_full_unstemmed |
Black carbon increases cation exchange capacity in soils |
| title_sort |
black carbon increases cation exchange capacity in soils |
| publisher |
Soil Science Society of America Journal |
| publishDate |
2020 |
| url |
https://repositorio.inpa.gov.br/handle/1/18729 |
| _version_ |
1787141494611640320 |
| score |
11.755432 |