Soil humic-like organic compounds in prescribed fire emissions using nuclear magnetic resonance spectroscopy
Here we present the chemical characterization of the water-soluble organic carbon fraction of atmospheric aerosol collected during a prescribed fire burn in relation to soil organic matter and biomass combustion. Using nuclear magnetic resonance spectroscopy, we observed that humic-like substances i...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Chalbot, M.-C. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2013transfer abstract |
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| Schlagwörter: |
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| Umfang: |
5 |
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| Übergeordnetes Werk: |
Enthalten in: Structural failure performance of the encased functionally graded porous cylinder consolidated by graphene platelet under uniform radial loading - Li, Zhaochao ELSEVIER, 2019, Amsterdam [u.a.] |
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| Übergeordnetes Werk: |
volume:181 ; year:2013 ; pages:167-171 ; extent:5 |
| Links: |
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| DOI / URN: |
10.1016/j.envpol.2013.06.008 |
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| 245 | 1 | 0 | |a Soil humic-like organic compounds in prescribed fire emissions using nuclear magnetic resonance spectroscopy |
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| 520 | |a Here we present the chemical characterization of the water-soluble organic carbon fraction of atmospheric aerosol collected during a prescribed fire burn in relation to soil organic matter and biomass combustion. Using nuclear magnetic resonance spectroscopy, we observed that humic-like substances in fire emissions have been associated with soil organic matter rather than biomass. Using a chemical mass balance model, we estimated that soil organic matter may contribute up to 41% of organic hydrogen and up to 27% of water-soluble organic carbon in fire emissions. Dust particles, when mixed with fresh combustion emissions, substantially enhances the atmospheric oxidative capacity, particle formation and microphysical properties of clouds influencing the climatic responses of atmospheric aeroso. Owing to the large emissions of combustion aerosol during fires, the release of dust particles from soil surfaces that are subjected to intense heating and shear stress has, so far, been lacking. | ||
| 520 | |a Here we present the chemical characterization of the water-soluble organic carbon fraction of atmospheric aerosol collected during a prescribed fire burn in relation to soil organic matter and biomass combustion. Using nuclear magnetic resonance spectroscopy, we observed that humic-like substances in fire emissions have been associated with soil organic matter rather than biomass. Using a chemical mass balance model, we estimated that soil organic matter may contribute up to 41% of organic hydrogen and up to 27% of water-soluble organic carbon in fire emissions. Dust particles, when mixed with fresh combustion emissions, substantially enhances the atmospheric oxidative capacity, particle formation and microphysical properties of clouds influencing the climatic responses of atmospheric aeroso. Owing to the large emissions of combustion aerosol during fires, the release of dust particles from soil surfaces that are subjected to intense heating and shear stress has, so far, been lacking. | ||
| 650 | 7 | |a Organic carbon |2 Elsevier | |
| 650 | 7 | |a Mineral dust |2 Elsevier | |
| 650 | 7 | |a Wildfires |2 Elsevier | |
| 650 | 7 | |a Biomass burning |2 Elsevier | |
| 650 | 7 | |a Aerosol |2 Elsevier | |
| 650 | 7 | |a Nuclear magnetic resonance |2 Elsevier | |
| 700 | 1 | |a Nikolich, G. |4 oth | |
| 700 | 1 | |a Etyemezian, V. |4 oth | |
| 700 | 1 | |a Dubois, D.W. |4 oth | |
| 700 | 1 | |a King, J. |4 oth | |
| 700 | 1 | |a Shafer, D. |4 oth | |
| 700 | 1 | |a Gamboa da Costa, G. |4 oth | |
| 700 | 1 | |a Hinton, J.F. |4 oth | |
| 700 | 1 | |a Kavouras, I.G. |4 oth | |
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10.1016/j.envpol.2013.06.008 doi GBVA2013006000004.pica (DE-627)ELV021761132 (ELSEVIER)S0269-7491(13)00325-4 DE-627 ger DE-627 rakwb eng 333.7 570 690 333.7 DE-600 570 DE-600 690 DE-600 690 VZ 50.31 bkl 56.11 bkl Chalbot, M.-C. verfasserin aut Soil humic-like organic compounds in prescribed fire emissions using nuclear magnetic resonance spectroscopy 2013transfer abstract 5 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Here we present the chemical characterization of the water-soluble organic carbon fraction of atmospheric aerosol collected during a prescribed fire burn in relation to soil organic matter and biomass combustion. Using nuclear magnetic resonance spectroscopy, we observed that humic-like substances in fire emissions have been associated with soil organic matter rather than biomass. Using a chemical mass balance model, we estimated that soil organic matter may contribute up to 41% of organic hydrogen and up to 27% of water-soluble organic carbon in fire emissions. Dust particles, when mixed with fresh combustion emissions, substantially enhances the atmospheric oxidative capacity, particle formation and microphysical properties of clouds influencing the climatic responses of atmospheric aeroso. Owing to the large emissions of combustion aerosol during fires, the release of dust particles from soil surfaces that are subjected to intense heating and shear stress has, so far, been lacking. Here we present the chemical characterization of the water-soluble organic carbon fraction of atmospheric aerosol collected during a prescribed fire burn in relation to soil organic matter and biomass combustion. Using nuclear magnetic resonance spectroscopy, we observed that humic-like substances in fire emissions have been associated with soil organic matter rather than biomass. Using a chemical mass balance model, we estimated that soil organic matter may contribute up to 41% of organic hydrogen and up to 27% of water-soluble organic carbon in fire emissions. Dust particles, when mixed with fresh combustion emissions, substantially enhances the atmospheric oxidative capacity, particle formation and microphysical properties of clouds influencing the climatic responses of atmospheric aeroso. Owing to the large emissions of combustion aerosol during fires, the release of dust particles from soil surfaces that are subjected to intense heating and shear stress has, so far, been lacking. Organic carbon Elsevier Mineral dust Elsevier Wildfires Elsevier Biomass burning Elsevier Aerosol Elsevier Nuclear magnetic resonance Elsevier Nikolich, G. oth Etyemezian, V. oth Dubois, D.W. oth King, J. oth Shafer, D. oth Gamboa da Costa, G. oth Hinton, J.F. oth Kavouras, I.G. oth Enthalten in Elsevier Science Li, Zhaochao ELSEVIER Structural failure performance of the encased functionally graded porous cylinder consolidated by graphene platelet under uniform radial loading 2019 Amsterdam [u.a.] (DE-627)ELV00327988X volume:181 year:2013 pages:167-171 extent:5 https://doi.org/10.1016/j.envpol.2013.06.008 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 50.31 Technische Mechanik VZ 56.11 Baukonstruktion VZ AR 181 2013 167-171 5 045F 333.7 |
| spelling |
10.1016/j.envpol.2013.06.008 doi GBVA2013006000004.pica (DE-627)ELV021761132 (ELSEVIER)S0269-7491(13)00325-4 DE-627 ger DE-627 rakwb eng 333.7 570 690 333.7 DE-600 570 DE-600 690 DE-600 690 VZ 50.31 bkl 56.11 bkl Chalbot, M.-C. verfasserin aut Soil humic-like organic compounds in prescribed fire emissions using nuclear magnetic resonance spectroscopy 2013transfer abstract 5 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Here we present the chemical characterization of the water-soluble organic carbon fraction of atmospheric aerosol collected during a prescribed fire burn in relation to soil organic matter and biomass combustion. Using nuclear magnetic resonance spectroscopy, we observed that humic-like substances in fire emissions have been associated with soil organic matter rather than biomass. Using a chemical mass balance model, we estimated that soil organic matter may contribute up to 41% of organic hydrogen and up to 27% of water-soluble organic carbon in fire emissions. Dust particles, when mixed with fresh combustion emissions, substantially enhances the atmospheric oxidative capacity, particle formation and microphysical properties of clouds influencing the climatic responses of atmospheric aeroso. Owing to the large emissions of combustion aerosol during fires, the release of dust particles from soil surfaces that are subjected to intense heating and shear stress has, so far, been lacking. Here we present the chemical characterization of the water-soluble organic carbon fraction of atmospheric aerosol collected during a prescribed fire burn in relation to soil organic matter and biomass combustion. Using nuclear magnetic resonance spectroscopy, we observed that humic-like substances in fire emissions have been associated with soil organic matter rather than biomass. Using a chemical mass balance model, we estimated that soil organic matter may contribute up to 41% of organic hydrogen and up to 27% of water-soluble organic carbon in fire emissions. Dust particles, when mixed with fresh combustion emissions, substantially enhances the atmospheric oxidative capacity, particle formation and microphysical properties of clouds influencing the climatic responses of atmospheric aeroso. Owing to the large emissions of combustion aerosol during fires, the release of dust particles from soil surfaces that are subjected to intense heating and shear stress has, so far, been lacking. Organic carbon Elsevier Mineral dust Elsevier Wildfires Elsevier Biomass burning Elsevier Aerosol Elsevier Nuclear magnetic resonance Elsevier Nikolich, G. oth Etyemezian, V. oth Dubois, D.W. oth King, J. oth Shafer, D. oth Gamboa da Costa, G. oth Hinton, J.F. oth Kavouras, I.G. oth Enthalten in Elsevier Science Li, Zhaochao ELSEVIER Structural failure performance of the encased functionally graded porous cylinder consolidated by graphene platelet under uniform radial loading 2019 Amsterdam [u.a.] (DE-627)ELV00327988X volume:181 year:2013 pages:167-171 extent:5 https://doi.org/10.1016/j.envpol.2013.06.008 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 50.31 Technische Mechanik VZ 56.11 Baukonstruktion VZ AR 181 2013 167-171 5 045F 333.7 |
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10.1016/j.envpol.2013.06.008 doi GBVA2013006000004.pica (DE-627)ELV021761132 (ELSEVIER)S0269-7491(13)00325-4 DE-627 ger DE-627 rakwb eng 333.7 570 690 333.7 DE-600 570 DE-600 690 DE-600 690 VZ 50.31 bkl 56.11 bkl Chalbot, M.-C. verfasserin aut Soil humic-like organic compounds in prescribed fire emissions using nuclear magnetic resonance spectroscopy 2013transfer abstract 5 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Here we present the chemical characterization of the water-soluble organic carbon fraction of atmospheric aerosol collected during a prescribed fire burn in relation to soil organic matter and biomass combustion. Using nuclear magnetic resonance spectroscopy, we observed that humic-like substances in fire emissions have been associated with soil organic matter rather than biomass. Using a chemical mass balance model, we estimated that soil organic matter may contribute up to 41% of organic hydrogen and up to 27% of water-soluble organic carbon in fire emissions. Dust particles, when mixed with fresh combustion emissions, substantially enhances the atmospheric oxidative capacity, particle formation and microphysical properties of clouds influencing the climatic responses of atmospheric aeroso. Owing to the large emissions of combustion aerosol during fires, the release of dust particles from soil surfaces that are subjected to intense heating and shear stress has, so far, been lacking. Here we present the chemical characterization of the water-soluble organic carbon fraction of atmospheric aerosol collected during a prescribed fire burn in relation to soil organic matter and biomass combustion. Using nuclear magnetic resonance spectroscopy, we observed that humic-like substances in fire emissions have been associated with soil organic matter rather than biomass. Using a chemical mass balance model, we estimated that soil organic matter may contribute up to 41% of organic hydrogen and up to 27% of water-soluble organic carbon in fire emissions. Dust particles, when mixed with fresh combustion emissions, substantially enhances the atmospheric oxidative capacity, particle formation and microphysical properties of clouds influencing the climatic responses of atmospheric aeroso. Owing to the large emissions of combustion aerosol during fires, the release of dust particles from soil surfaces that are subjected to intense heating and shear stress has, so far, been lacking. Organic carbon Elsevier Mineral dust Elsevier Wildfires Elsevier Biomass burning Elsevier Aerosol Elsevier Nuclear magnetic resonance Elsevier Nikolich, G. oth Etyemezian, V. oth Dubois, D.W. oth King, J. oth Shafer, D. oth Gamboa da Costa, G. oth Hinton, J.F. oth Kavouras, I.G. oth Enthalten in Elsevier Science Li, Zhaochao ELSEVIER Structural failure performance of the encased functionally graded porous cylinder consolidated by graphene platelet under uniform radial loading 2019 Amsterdam [u.a.] (DE-627)ELV00327988X volume:181 year:2013 pages:167-171 extent:5 https://doi.org/10.1016/j.envpol.2013.06.008 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 50.31 Technische Mechanik VZ 56.11 Baukonstruktion VZ AR 181 2013 167-171 5 045F 333.7 |
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10.1016/j.envpol.2013.06.008 doi GBVA2013006000004.pica (DE-627)ELV021761132 (ELSEVIER)S0269-7491(13)00325-4 DE-627 ger DE-627 rakwb eng 333.7 570 690 333.7 DE-600 570 DE-600 690 DE-600 690 VZ 50.31 bkl 56.11 bkl Chalbot, M.-C. verfasserin aut Soil humic-like organic compounds in prescribed fire emissions using nuclear magnetic resonance spectroscopy 2013transfer abstract 5 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Here we present the chemical characterization of the water-soluble organic carbon fraction of atmospheric aerosol collected during a prescribed fire burn in relation to soil organic matter and biomass combustion. Using nuclear magnetic resonance spectroscopy, we observed that humic-like substances in fire emissions have been associated with soil organic matter rather than biomass. Using a chemical mass balance model, we estimated that soil organic matter may contribute up to 41% of organic hydrogen and up to 27% of water-soluble organic carbon in fire emissions. Dust particles, when mixed with fresh combustion emissions, substantially enhances the atmospheric oxidative capacity, particle formation and microphysical properties of clouds influencing the climatic responses of atmospheric aeroso. Owing to the large emissions of combustion aerosol during fires, the release of dust particles from soil surfaces that are subjected to intense heating and shear stress has, so far, been lacking. Here we present the chemical characterization of the water-soluble organic carbon fraction of atmospheric aerosol collected during a prescribed fire burn in relation to soil organic matter and biomass combustion. Using nuclear magnetic resonance spectroscopy, we observed that humic-like substances in fire emissions have been associated with soil organic matter rather than biomass. Using a chemical mass balance model, we estimated that soil organic matter may contribute up to 41% of organic hydrogen and up to 27% of water-soluble organic carbon in fire emissions. Dust particles, when mixed with fresh combustion emissions, substantially enhances the atmospheric oxidative capacity, particle formation and microphysical properties of clouds influencing the climatic responses of atmospheric aeroso. Owing to the large emissions of combustion aerosol during fires, the release of dust particles from soil surfaces that are subjected to intense heating and shear stress has, so far, been lacking. Organic carbon Elsevier Mineral dust Elsevier Wildfires Elsevier Biomass burning Elsevier Aerosol Elsevier Nuclear magnetic resonance Elsevier Nikolich, G. oth Etyemezian, V. oth Dubois, D.W. oth King, J. oth Shafer, D. oth Gamboa da Costa, G. oth Hinton, J.F. oth Kavouras, I.G. oth Enthalten in Elsevier Science Li, Zhaochao ELSEVIER Structural failure performance of the encased functionally graded porous cylinder consolidated by graphene platelet under uniform radial loading 2019 Amsterdam [u.a.] (DE-627)ELV00327988X volume:181 year:2013 pages:167-171 extent:5 https://doi.org/10.1016/j.envpol.2013.06.008 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 50.31 Technische Mechanik VZ 56.11 Baukonstruktion VZ AR 181 2013 167-171 5 045F 333.7 |
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10.1016/j.envpol.2013.06.008 doi GBVA2013006000004.pica (DE-627)ELV021761132 (ELSEVIER)S0269-7491(13)00325-4 DE-627 ger DE-627 rakwb eng 333.7 570 690 333.7 DE-600 570 DE-600 690 DE-600 690 VZ 50.31 bkl 56.11 bkl Chalbot, M.-C. verfasserin aut Soil humic-like organic compounds in prescribed fire emissions using nuclear magnetic resonance spectroscopy 2013transfer abstract 5 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Here we present the chemical characterization of the water-soluble organic carbon fraction of atmospheric aerosol collected during a prescribed fire burn in relation to soil organic matter and biomass combustion. Using nuclear magnetic resonance spectroscopy, we observed that humic-like substances in fire emissions have been associated with soil organic matter rather than biomass. Using a chemical mass balance model, we estimated that soil organic matter may contribute up to 41% of organic hydrogen and up to 27% of water-soluble organic carbon in fire emissions. Dust particles, when mixed with fresh combustion emissions, substantially enhances the atmospheric oxidative capacity, particle formation and microphysical properties of clouds influencing the climatic responses of atmospheric aeroso. Owing to the large emissions of combustion aerosol during fires, the release of dust particles from soil surfaces that are subjected to intense heating and shear stress has, so far, been lacking. Here we present the chemical characterization of the water-soluble organic carbon fraction of atmospheric aerosol collected during a prescribed fire burn in relation to soil organic matter and biomass combustion. Using nuclear magnetic resonance spectroscopy, we observed that humic-like substances in fire emissions have been associated with soil organic matter rather than biomass. Using a chemical mass balance model, we estimated that soil organic matter may contribute up to 41% of organic hydrogen and up to 27% of water-soluble organic carbon in fire emissions. Dust particles, when mixed with fresh combustion emissions, substantially enhances the atmospheric oxidative capacity, particle formation and microphysical properties of clouds influencing the climatic responses of atmospheric aeroso. Owing to the large emissions of combustion aerosol during fires, the release of dust particles from soil surfaces that are subjected to intense heating and shear stress has, so far, been lacking. Organic carbon Elsevier Mineral dust Elsevier Wildfires Elsevier Biomass burning Elsevier Aerosol Elsevier Nuclear magnetic resonance Elsevier Nikolich, G. oth Etyemezian, V. oth Dubois, D.W. oth King, J. oth Shafer, D. oth Gamboa da Costa, G. oth Hinton, J.F. oth Kavouras, I.G. oth Enthalten in Elsevier Science Li, Zhaochao ELSEVIER Structural failure performance of the encased functionally graded porous cylinder consolidated by graphene platelet under uniform radial loading 2019 Amsterdam [u.a.] (DE-627)ELV00327988X volume:181 year:2013 pages:167-171 extent:5 https://doi.org/10.1016/j.envpol.2013.06.008 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 50.31 Technische Mechanik VZ 56.11 Baukonstruktion VZ AR 181 2013 167-171 5 045F 333.7 |
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Enthalten in Structural failure performance of the encased functionally graded porous cylinder consolidated by graphene platelet under uniform radial loading Amsterdam [u.a.] volume:181 year:2013 pages:167-171 extent:5 |
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Enthalten in Structural failure performance of the encased functionally graded porous cylinder consolidated by graphene platelet under uniform radial loading Amsterdam [u.a.] volume:181 year:2013 pages:167-171 extent:5 |
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Structural failure performance of the encased functionally graded porous cylinder consolidated by graphene platelet under uniform radial loading |
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soil humic-like organic compounds in prescribed fire emissions using nuclear magnetic resonance spectroscopy |
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Soil humic-like organic compounds in prescribed fire emissions using nuclear magnetic resonance spectroscopy |
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Here we present the chemical characterization of the water-soluble organic carbon fraction of atmospheric aerosol collected during a prescribed fire burn in relation to soil organic matter and biomass combustion. Using nuclear magnetic resonance spectroscopy, we observed that humic-like substances in fire emissions have been associated with soil organic matter rather than biomass. Using a chemical mass balance model, we estimated that soil organic matter may contribute up to 41% of organic hydrogen and up to 27% of water-soluble organic carbon in fire emissions. Dust particles, when mixed with fresh combustion emissions, substantially enhances the atmospheric oxidative capacity, particle formation and microphysical properties of clouds influencing the climatic responses of atmospheric aeroso. Owing to the large emissions of combustion aerosol during fires, the release of dust particles from soil surfaces that are subjected to intense heating and shear stress has, so far, been lacking. |
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Here we present the chemical characterization of the water-soluble organic carbon fraction of atmospheric aerosol collected during a prescribed fire burn in relation to soil organic matter and biomass combustion. Using nuclear magnetic resonance spectroscopy, we observed that humic-like substances in fire emissions have been associated with soil organic matter rather than biomass. Using a chemical mass balance model, we estimated that soil organic matter may contribute up to 41% of organic hydrogen and up to 27% of water-soluble organic carbon in fire emissions. Dust particles, when mixed with fresh combustion emissions, substantially enhances the atmospheric oxidative capacity, particle formation and microphysical properties of clouds influencing the climatic responses of atmospheric aeroso. Owing to the large emissions of combustion aerosol during fires, the release of dust particles from soil surfaces that are subjected to intense heating and shear stress has, so far, been lacking. |
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Here we present the chemical characterization of the water-soluble organic carbon fraction of atmospheric aerosol collected during a prescribed fire burn in relation to soil organic matter and biomass combustion. Using nuclear magnetic resonance spectroscopy, we observed that humic-like substances in fire emissions have been associated with soil organic matter rather than biomass. Using a chemical mass balance model, we estimated that soil organic matter may contribute up to 41% of organic hydrogen and up to 27% of water-soluble organic carbon in fire emissions. Dust particles, when mixed with fresh combustion emissions, substantially enhances the atmospheric oxidative capacity, particle formation and microphysical properties of clouds influencing the climatic responses of atmospheric aeroso. Owing to the large emissions of combustion aerosol during fires, the release of dust particles from soil surfaces that are subjected to intense heating and shear stress has, so far, been lacking. |
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