Comparison of soil organic carbon speciation using C NEXAFS and CPMAS 13C NMR spectroscopy
We compared synchrotron-based C near-edge X-ray absorption fine structure (NEXAFS) and CPMAS 13C nuclear magnetic resonance (NMR) spectroscopy with respect to their precision and accuracy to quantify different organic carbon (OC) species in defined mixtures of soil organic matter source compounds. W...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Prietzel, Jörg [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2018transfer abstract |
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| Umfang: |
13 |
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| Übergeordnetes Werk: |
Enthalten in: SPG-56 from Sweet potato Zhongshu-1 delayed growth of tumor xenografts in nude mice by modulating gut microbiota - Wang, Meimei ELSEVIER, 2018, an international journal for scientific research into the environment and its relationship with man, Amsterdam [u.a.] |
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| Übergeordnetes Werk: |
volume:628 ; year:2018 ; day:1 ; month:07 ; pages:906-918 ; extent:13 |
| Links: |
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| DOI / URN: |
10.1016/j.scitotenv.2018.02.121 |
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ELV042450373 |
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| 245 | 1 | 0 | |a Comparison of soil organic carbon speciation using C NEXAFS and CPMAS 13C NMR spectroscopy |
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| 520 | |a We compared synchrotron-based C near-edge X-ray absorption fine structure (NEXAFS) and CPMAS 13C nuclear magnetic resonance (NMR) spectroscopy with respect to their precision and accuracy to quantify different organic carbon (OC) species in defined mixtures of soil organic matter source compounds. We also used both methods to quantify different OC species in organic surface horizons of a Histic Leptosol as well as in mineral topsoil and subsoil horizons of two soils with different parent material, stage of pedogenesis, and OC content (Cambisol: 15–30 OC mgg−1, Podzol: 0.9–7 OC mgg−1). CPMAS 13C NMR spectroscopy was more accurate and precise (mean recovery of different C functional groups 96–103%) than C NEXAFS spectroscopy (mean recovery 92–113%). For organic surface and topsoil samples, NMR spectroscopy consistently yielded larger O-alkyl C percentages and smaller alkyl C percentages than C NEXAFS spectroscopy. For the Cambisol subsoil samples both methods performed well and showed similar C speciation results. NEXAFS spectroscopy yielded excellent spectra with a high signal-to-noise ratio also for OC-poor Podzol subsoil samples, whereas this was not the case for CPMAS 13C NMR spectroscopy even after sample treatment with HF. Our results confirm the analytical power of CPMAS 13C NMR spectroscopy for a reliable quantitative OC speciation in soils with >10mgOCg−1. Moreover, they highlight the potential of synchrotron-based C NEXAFS spectroscopy as fast, non-invasive method to semi-quantify different C functional groups in soils with low C content (0.9–10mgg−1). | ||
| 520 | |a We compared synchrotron-based C near-edge X-ray absorption fine structure (NEXAFS) and CPMAS 13C nuclear magnetic resonance (NMR) spectroscopy with respect to their precision and accuracy to quantify different organic carbon (OC) species in defined mixtures of soil organic matter source compounds. We also used both methods to quantify different OC species in organic surface horizons of a Histic Leptosol as well as in mineral topsoil and subsoil horizons of two soils with different parent material, stage of pedogenesis, and OC content (Cambisol: 15–30 OC mgg−1, Podzol: 0.9–7 OC mgg−1). CPMAS 13C NMR spectroscopy was more accurate and precise (mean recovery of different C functional groups 96–103%) than C NEXAFS spectroscopy (mean recovery 92–113%). For organic surface and topsoil samples, NMR spectroscopy consistently yielded larger O-alkyl C percentages and smaller alkyl C percentages than C NEXAFS spectroscopy. For the Cambisol subsoil samples both methods performed well and showed similar C speciation results. NEXAFS spectroscopy yielded excellent spectra with a high signal-to-noise ratio also for OC-poor Podzol subsoil samples, whereas this was not the case for CPMAS 13C NMR spectroscopy even after sample treatment with HF. Our results confirm the analytical power of CPMAS 13C NMR spectroscopy for a reliable quantitative OC speciation in soils with >10mgOCg−1. Moreover, they highlight the potential of synchrotron-based C NEXAFS spectroscopy as fast, non-invasive method to semi-quantify different C functional groups in soils with low C content (0.9–10mgg−1). | ||
| 700 | 1 | |a Müller, Svenja |4 oth | |
| 700 | 1 | |a Kögel-Knabner, Ingrid |4 oth | |
| 700 | 1 | |a Thieme, Jürgen |4 oth | |
| 700 | 1 | |a Jaye, Cherno |4 oth | |
| 700 | 1 | |a Fischer, Daniel |4 oth | |
| 773 | 0 | 8 | |i Enthalten in |n Elsevier Science |a Wang, Meimei ELSEVIER |t SPG-56 from Sweet potato Zhongshu-1 delayed growth of tumor xenografts in nude mice by modulating gut microbiota |d 2018 |d an international journal for scientific research into the environment and its relationship with man |g Amsterdam [u.a.] |w (DE-627)ELV001360035 |
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10.1016/j.scitotenv.2018.02.121 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001197.pica (DE-627)ELV042450373 (ELSEVIER)S0048-9697(18)30511-4 DE-627 ger DE-627 rakwb eng 630 640 610 VZ Prietzel, Jörg verfasserin aut Comparison of soil organic carbon speciation using C NEXAFS and CPMAS 13C NMR spectroscopy 2018transfer abstract 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier We compared synchrotron-based C near-edge X-ray absorption fine structure (NEXAFS) and CPMAS 13C nuclear magnetic resonance (NMR) spectroscopy with respect to their precision and accuracy to quantify different organic carbon (OC) species in defined mixtures of soil organic matter source compounds. We also used both methods to quantify different OC species in organic surface horizons of a Histic Leptosol as well as in mineral topsoil and subsoil horizons of two soils with different parent material, stage of pedogenesis, and OC content (Cambisol: 15–30 OC mgg−1, Podzol: 0.9–7 OC mgg−1). CPMAS 13C NMR spectroscopy was more accurate and precise (mean recovery of different C functional groups 96–103%) than C NEXAFS spectroscopy (mean recovery 92–113%). For organic surface and topsoil samples, NMR spectroscopy consistently yielded larger O-alkyl C percentages and smaller alkyl C percentages than C NEXAFS spectroscopy. For the Cambisol subsoil samples both methods performed well and showed similar C speciation results. NEXAFS spectroscopy yielded excellent spectra with a high signal-to-noise ratio also for OC-poor Podzol subsoil samples, whereas this was not the case for CPMAS 13C NMR spectroscopy even after sample treatment with HF. Our results confirm the analytical power of CPMAS 13C NMR spectroscopy for a reliable quantitative OC speciation in soils with >10mgOCg−1. Moreover, they highlight the potential of synchrotron-based C NEXAFS spectroscopy as fast, non-invasive method to semi-quantify different C functional groups in soils with low C content (0.9–10mgg−1). We compared synchrotron-based C near-edge X-ray absorption fine structure (NEXAFS) and CPMAS 13C nuclear magnetic resonance (NMR) spectroscopy with respect to their precision and accuracy to quantify different organic carbon (OC) species in defined mixtures of soil organic matter source compounds. We also used both methods to quantify different OC species in organic surface horizons of a Histic Leptosol as well as in mineral topsoil and subsoil horizons of two soils with different parent material, stage of pedogenesis, and OC content (Cambisol: 15–30 OC mgg−1, Podzol: 0.9–7 OC mgg−1). CPMAS 13C NMR spectroscopy was more accurate and precise (mean recovery of different C functional groups 96–103%) than C NEXAFS spectroscopy (mean recovery 92–113%). For organic surface and topsoil samples, NMR spectroscopy consistently yielded larger O-alkyl C percentages and smaller alkyl C percentages than C NEXAFS spectroscopy. For the Cambisol subsoil samples both methods performed well and showed similar C speciation results. NEXAFS spectroscopy yielded excellent spectra with a high signal-to-noise ratio also for OC-poor Podzol subsoil samples, whereas this was not the case for CPMAS 13C NMR spectroscopy even after sample treatment with HF. Our results confirm the analytical power of CPMAS 13C NMR spectroscopy for a reliable quantitative OC speciation in soils with >10mgOCg−1. Moreover, they highlight the potential of synchrotron-based C NEXAFS spectroscopy as fast, non-invasive method to semi-quantify different C functional groups in soils with low C content (0.9–10mgg−1). Müller, Svenja oth Kögel-Knabner, Ingrid oth Thieme, Jürgen oth Jaye, Cherno oth Fischer, Daniel oth Enthalten in Elsevier Science Wang, Meimei ELSEVIER SPG-56 from Sweet potato Zhongshu-1 delayed growth of tumor xenografts in nude mice by modulating gut microbiota 2018 an international journal for scientific research into the environment and its relationship with man Amsterdam [u.a.] (DE-627)ELV001360035 volume:628 year:2018 day:1 month:07 pages:906-918 extent:13 https://doi.org/10.1016/j.scitotenv.2018.02.121 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA AR 628 2018 1 0701 906-918 13 |
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10.1016/j.scitotenv.2018.02.121 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001197.pica (DE-627)ELV042450373 (ELSEVIER)S0048-9697(18)30511-4 DE-627 ger DE-627 rakwb eng 630 640 610 VZ Prietzel, Jörg verfasserin aut Comparison of soil organic carbon speciation using C NEXAFS and CPMAS 13C NMR spectroscopy 2018transfer abstract 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier We compared synchrotron-based C near-edge X-ray absorption fine structure (NEXAFS) and CPMAS 13C nuclear magnetic resonance (NMR) spectroscopy with respect to their precision and accuracy to quantify different organic carbon (OC) species in defined mixtures of soil organic matter source compounds. We also used both methods to quantify different OC species in organic surface horizons of a Histic Leptosol as well as in mineral topsoil and subsoil horizons of two soils with different parent material, stage of pedogenesis, and OC content (Cambisol: 15–30 OC mgg−1, Podzol: 0.9–7 OC mgg−1). CPMAS 13C NMR spectroscopy was more accurate and precise (mean recovery of different C functional groups 96–103%) than C NEXAFS spectroscopy (mean recovery 92–113%). For organic surface and topsoil samples, NMR spectroscopy consistently yielded larger O-alkyl C percentages and smaller alkyl C percentages than C NEXAFS spectroscopy. For the Cambisol subsoil samples both methods performed well and showed similar C speciation results. NEXAFS spectroscopy yielded excellent spectra with a high signal-to-noise ratio also for OC-poor Podzol subsoil samples, whereas this was not the case for CPMAS 13C NMR spectroscopy even after sample treatment with HF. Our results confirm the analytical power of CPMAS 13C NMR spectroscopy for a reliable quantitative OC speciation in soils with >10mgOCg−1. Moreover, they highlight the potential of synchrotron-based C NEXAFS spectroscopy as fast, non-invasive method to semi-quantify different C functional groups in soils with low C content (0.9–10mgg−1). We compared synchrotron-based C near-edge X-ray absorption fine structure (NEXAFS) and CPMAS 13C nuclear magnetic resonance (NMR) spectroscopy with respect to their precision and accuracy to quantify different organic carbon (OC) species in defined mixtures of soil organic matter source compounds. We also used both methods to quantify different OC species in organic surface horizons of a Histic Leptosol as well as in mineral topsoil and subsoil horizons of two soils with different parent material, stage of pedogenesis, and OC content (Cambisol: 15–30 OC mgg−1, Podzol: 0.9–7 OC mgg−1). CPMAS 13C NMR spectroscopy was more accurate and precise (mean recovery of different C functional groups 96–103%) than C NEXAFS spectroscopy (mean recovery 92–113%). For organic surface and topsoil samples, NMR spectroscopy consistently yielded larger O-alkyl C percentages and smaller alkyl C percentages than C NEXAFS spectroscopy. For the Cambisol subsoil samples both methods performed well and showed similar C speciation results. NEXAFS spectroscopy yielded excellent spectra with a high signal-to-noise ratio also for OC-poor Podzol subsoil samples, whereas this was not the case for CPMAS 13C NMR spectroscopy even after sample treatment with HF. Our results confirm the analytical power of CPMAS 13C NMR spectroscopy for a reliable quantitative OC speciation in soils with >10mgOCg−1. Moreover, they highlight the potential of synchrotron-based C NEXAFS spectroscopy as fast, non-invasive method to semi-quantify different C functional groups in soils with low C content (0.9–10mgg−1). Müller, Svenja oth Kögel-Knabner, Ingrid oth Thieme, Jürgen oth Jaye, Cherno oth Fischer, Daniel oth Enthalten in Elsevier Science Wang, Meimei ELSEVIER SPG-56 from Sweet potato Zhongshu-1 delayed growth of tumor xenografts in nude mice by modulating gut microbiota 2018 an international journal for scientific research into the environment and its relationship with man Amsterdam [u.a.] (DE-627)ELV001360035 volume:628 year:2018 day:1 month:07 pages:906-918 extent:13 https://doi.org/10.1016/j.scitotenv.2018.02.121 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA AR 628 2018 1 0701 906-918 13 |
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10.1016/j.scitotenv.2018.02.121 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001197.pica (DE-627)ELV042450373 (ELSEVIER)S0048-9697(18)30511-4 DE-627 ger DE-627 rakwb eng 630 640 610 VZ Prietzel, Jörg verfasserin aut Comparison of soil organic carbon speciation using C NEXAFS and CPMAS 13C NMR spectroscopy 2018transfer abstract 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier We compared synchrotron-based C near-edge X-ray absorption fine structure (NEXAFS) and CPMAS 13C nuclear magnetic resonance (NMR) spectroscopy with respect to their precision and accuracy to quantify different organic carbon (OC) species in defined mixtures of soil organic matter source compounds. We also used both methods to quantify different OC species in organic surface horizons of a Histic Leptosol as well as in mineral topsoil and subsoil horizons of two soils with different parent material, stage of pedogenesis, and OC content (Cambisol: 15–30 OC mgg−1, Podzol: 0.9–7 OC mgg−1). CPMAS 13C NMR spectroscopy was more accurate and precise (mean recovery of different C functional groups 96–103%) than C NEXAFS spectroscopy (mean recovery 92–113%). For organic surface and topsoil samples, NMR spectroscopy consistently yielded larger O-alkyl C percentages and smaller alkyl C percentages than C NEXAFS spectroscopy. For the Cambisol subsoil samples both methods performed well and showed similar C speciation results. NEXAFS spectroscopy yielded excellent spectra with a high signal-to-noise ratio also for OC-poor Podzol subsoil samples, whereas this was not the case for CPMAS 13C NMR spectroscopy even after sample treatment with HF. Our results confirm the analytical power of CPMAS 13C NMR spectroscopy for a reliable quantitative OC speciation in soils with >10mgOCg−1. Moreover, they highlight the potential of synchrotron-based C NEXAFS spectroscopy as fast, non-invasive method to semi-quantify different C functional groups in soils with low C content (0.9–10mgg−1). We compared synchrotron-based C near-edge X-ray absorption fine structure (NEXAFS) and CPMAS 13C nuclear magnetic resonance (NMR) spectroscopy with respect to their precision and accuracy to quantify different organic carbon (OC) species in defined mixtures of soil organic matter source compounds. We also used both methods to quantify different OC species in organic surface horizons of a Histic Leptosol as well as in mineral topsoil and subsoil horizons of two soils with different parent material, stage of pedogenesis, and OC content (Cambisol: 15–30 OC mgg−1, Podzol: 0.9–7 OC mgg−1). CPMAS 13C NMR spectroscopy was more accurate and precise (mean recovery of different C functional groups 96–103%) than C NEXAFS spectroscopy (mean recovery 92–113%). For organic surface and topsoil samples, NMR spectroscopy consistently yielded larger O-alkyl C percentages and smaller alkyl C percentages than C NEXAFS spectroscopy. For the Cambisol subsoil samples both methods performed well and showed similar C speciation results. NEXAFS spectroscopy yielded excellent spectra with a high signal-to-noise ratio also for OC-poor Podzol subsoil samples, whereas this was not the case for CPMAS 13C NMR spectroscopy even after sample treatment with HF. Our results confirm the analytical power of CPMAS 13C NMR spectroscopy for a reliable quantitative OC speciation in soils with >10mgOCg−1. Moreover, they highlight the potential of synchrotron-based C NEXAFS spectroscopy as fast, non-invasive method to semi-quantify different C functional groups in soils with low C content (0.9–10mgg−1). Müller, Svenja oth Kögel-Knabner, Ingrid oth Thieme, Jürgen oth Jaye, Cherno oth Fischer, Daniel oth Enthalten in Elsevier Science Wang, Meimei ELSEVIER SPG-56 from Sweet potato Zhongshu-1 delayed growth of tumor xenografts in nude mice by modulating gut microbiota 2018 an international journal for scientific research into the environment and its relationship with man Amsterdam [u.a.] (DE-627)ELV001360035 volume:628 year:2018 day:1 month:07 pages:906-918 extent:13 https://doi.org/10.1016/j.scitotenv.2018.02.121 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA AR 628 2018 1 0701 906-918 13 |
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10.1016/j.scitotenv.2018.02.121 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001197.pica (DE-627)ELV042450373 (ELSEVIER)S0048-9697(18)30511-4 DE-627 ger DE-627 rakwb eng 630 640 610 VZ Prietzel, Jörg verfasserin aut Comparison of soil organic carbon speciation using C NEXAFS and CPMAS 13C NMR spectroscopy 2018transfer abstract 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier We compared synchrotron-based C near-edge X-ray absorption fine structure (NEXAFS) and CPMAS 13C nuclear magnetic resonance (NMR) spectroscopy with respect to their precision and accuracy to quantify different organic carbon (OC) species in defined mixtures of soil organic matter source compounds. We also used both methods to quantify different OC species in organic surface horizons of a Histic Leptosol as well as in mineral topsoil and subsoil horizons of two soils with different parent material, stage of pedogenesis, and OC content (Cambisol: 15–30 OC mgg−1, Podzol: 0.9–7 OC mgg−1). CPMAS 13C NMR spectroscopy was more accurate and precise (mean recovery of different C functional groups 96–103%) than C NEXAFS spectroscopy (mean recovery 92–113%). For organic surface and topsoil samples, NMR spectroscopy consistently yielded larger O-alkyl C percentages and smaller alkyl C percentages than C NEXAFS spectroscopy. For the Cambisol subsoil samples both methods performed well and showed similar C speciation results. NEXAFS spectroscopy yielded excellent spectra with a high signal-to-noise ratio also for OC-poor Podzol subsoil samples, whereas this was not the case for CPMAS 13C NMR spectroscopy even after sample treatment with HF. Our results confirm the analytical power of CPMAS 13C NMR spectroscopy for a reliable quantitative OC speciation in soils with >10mgOCg−1. Moreover, they highlight the potential of synchrotron-based C NEXAFS spectroscopy as fast, non-invasive method to semi-quantify different C functional groups in soils with low C content (0.9–10mgg−1). We compared synchrotron-based C near-edge X-ray absorption fine structure (NEXAFS) and CPMAS 13C nuclear magnetic resonance (NMR) spectroscopy with respect to their precision and accuracy to quantify different organic carbon (OC) species in defined mixtures of soil organic matter source compounds. We also used both methods to quantify different OC species in organic surface horizons of a Histic Leptosol as well as in mineral topsoil and subsoil horizons of two soils with different parent material, stage of pedogenesis, and OC content (Cambisol: 15–30 OC mgg−1, Podzol: 0.9–7 OC mgg−1). CPMAS 13C NMR spectroscopy was more accurate and precise (mean recovery of different C functional groups 96–103%) than C NEXAFS spectroscopy (mean recovery 92–113%). For organic surface and topsoil samples, NMR spectroscopy consistently yielded larger O-alkyl C percentages and smaller alkyl C percentages than C NEXAFS spectroscopy. For the Cambisol subsoil samples both methods performed well and showed similar C speciation results. NEXAFS spectroscopy yielded excellent spectra with a high signal-to-noise ratio also for OC-poor Podzol subsoil samples, whereas this was not the case for CPMAS 13C NMR spectroscopy even after sample treatment with HF. Our results confirm the analytical power of CPMAS 13C NMR spectroscopy for a reliable quantitative OC speciation in soils with >10mgOCg−1. Moreover, they highlight the potential of synchrotron-based C NEXAFS spectroscopy as fast, non-invasive method to semi-quantify different C functional groups in soils with low C content (0.9–10mgg−1). Müller, Svenja oth Kögel-Knabner, Ingrid oth Thieme, Jürgen oth Jaye, Cherno oth Fischer, Daniel oth Enthalten in Elsevier Science Wang, Meimei ELSEVIER SPG-56 from Sweet potato Zhongshu-1 delayed growth of tumor xenografts in nude mice by modulating gut microbiota 2018 an international journal for scientific research into the environment and its relationship with man Amsterdam [u.a.] (DE-627)ELV001360035 volume:628 year:2018 day:1 month:07 pages:906-918 extent:13 https://doi.org/10.1016/j.scitotenv.2018.02.121 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA AR 628 2018 1 0701 906-918 13 |
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10.1016/j.scitotenv.2018.02.121 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001197.pica (DE-627)ELV042450373 (ELSEVIER)S0048-9697(18)30511-4 DE-627 ger DE-627 rakwb eng 630 640 610 VZ Prietzel, Jörg verfasserin aut Comparison of soil organic carbon speciation using C NEXAFS and CPMAS 13C NMR spectroscopy 2018transfer abstract 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier We compared synchrotron-based C near-edge X-ray absorption fine structure (NEXAFS) and CPMAS 13C nuclear magnetic resonance (NMR) spectroscopy with respect to their precision and accuracy to quantify different organic carbon (OC) species in defined mixtures of soil organic matter source compounds. We also used both methods to quantify different OC species in organic surface horizons of a Histic Leptosol as well as in mineral topsoil and subsoil horizons of two soils with different parent material, stage of pedogenesis, and OC content (Cambisol: 15–30 OC mgg−1, Podzol: 0.9–7 OC mgg−1). CPMAS 13C NMR spectroscopy was more accurate and precise (mean recovery of different C functional groups 96–103%) than C NEXAFS spectroscopy (mean recovery 92–113%). For organic surface and topsoil samples, NMR spectroscopy consistently yielded larger O-alkyl C percentages and smaller alkyl C percentages than C NEXAFS spectroscopy. For the Cambisol subsoil samples both methods performed well and showed similar C speciation results. NEXAFS spectroscopy yielded excellent spectra with a high signal-to-noise ratio also for OC-poor Podzol subsoil samples, whereas this was not the case for CPMAS 13C NMR spectroscopy even after sample treatment with HF. Our results confirm the analytical power of CPMAS 13C NMR spectroscopy for a reliable quantitative OC speciation in soils with >10mgOCg−1. Moreover, they highlight the potential of synchrotron-based C NEXAFS spectroscopy as fast, non-invasive method to semi-quantify different C functional groups in soils with low C content (0.9–10mgg−1). We compared synchrotron-based C near-edge X-ray absorption fine structure (NEXAFS) and CPMAS 13C nuclear magnetic resonance (NMR) spectroscopy with respect to their precision and accuracy to quantify different organic carbon (OC) species in defined mixtures of soil organic matter source compounds. We also used both methods to quantify different OC species in organic surface horizons of a Histic Leptosol as well as in mineral topsoil and subsoil horizons of two soils with different parent material, stage of pedogenesis, and OC content (Cambisol: 15–30 OC mgg−1, Podzol: 0.9–7 OC mgg−1). CPMAS 13C NMR spectroscopy was more accurate and precise (mean recovery of different C functional groups 96–103%) than C NEXAFS spectroscopy (mean recovery 92–113%). For organic surface and topsoil samples, NMR spectroscopy consistently yielded larger O-alkyl C percentages and smaller alkyl C percentages than C NEXAFS spectroscopy. For the Cambisol subsoil samples both methods performed well and showed similar C speciation results. NEXAFS spectroscopy yielded excellent spectra with a high signal-to-noise ratio also for OC-poor Podzol subsoil samples, whereas this was not the case for CPMAS 13C NMR spectroscopy even after sample treatment with HF. Our results confirm the analytical power of CPMAS 13C NMR spectroscopy for a reliable quantitative OC speciation in soils with >10mgOCg−1. Moreover, they highlight the potential of synchrotron-based C NEXAFS spectroscopy as fast, non-invasive method to semi-quantify different C functional groups in soils with low C content (0.9–10mgg−1). Müller, Svenja oth Kögel-Knabner, Ingrid oth Thieme, Jürgen oth Jaye, Cherno oth Fischer, Daniel oth Enthalten in Elsevier Science Wang, Meimei ELSEVIER SPG-56 from Sweet potato Zhongshu-1 delayed growth of tumor xenografts in nude mice by modulating gut microbiota 2018 an international journal for scientific research into the environment and its relationship with man Amsterdam [u.a.] (DE-627)ELV001360035 volume:628 year:2018 day:1 month:07 pages:906-918 extent:13 https://doi.org/10.1016/j.scitotenv.2018.02.121 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA AR 628 2018 1 0701 906-918 13 |
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comparison of soil organic carbon speciation using c nexafs and cpmas 13c nmr spectroscopy |
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Comparison of soil organic carbon speciation using C NEXAFS and CPMAS 13C NMR spectroscopy |
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We compared synchrotron-based C near-edge X-ray absorption fine structure (NEXAFS) and CPMAS 13C nuclear magnetic resonance (NMR) spectroscopy with respect to their precision and accuracy to quantify different organic carbon (OC) species in defined mixtures of soil organic matter source compounds. We also used both methods to quantify different OC species in organic surface horizons of a Histic Leptosol as well as in mineral topsoil and subsoil horizons of two soils with different parent material, stage of pedogenesis, and OC content (Cambisol: 15–30 OC mgg−1, Podzol: 0.9–7 OC mgg−1). CPMAS 13C NMR spectroscopy was more accurate and precise (mean recovery of different C functional groups 96–103%) than C NEXAFS spectroscopy (mean recovery 92–113%). For organic surface and topsoil samples, NMR spectroscopy consistently yielded larger O-alkyl C percentages and smaller alkyl C percentages than C NEXAFS spectroscopy. For the Cambisol subsoil samples both methods performed well and showed similar C speciation results. NEXAFS spectroscopy yielded excellent spectra with a high signal-to-noise ratio also for OC-poor Podzol subsoil samples, whereas this was not the case for CPMAS 13C NMR spectroscopy even after sample treatment with HF. Our results confirm the analytical power of CPMAS 13C NMR spectroscopy for a reliable quantitative OC speciation in soils with >10mgOCg−1. Moreover, they highlight the potential of synchrotron-based C NEXAFS spectroscopy as fast, non-invasive method to semi-quantify different C functional groups in soils with low C content (0.9–10mgg−1). |
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We compared synchrotron-based C near-edge X-ray absorption fine structure (NEXAFS) and CPMAS 13C nuclear magnetic resonance (NMR) spectroscopy with respect to their precision and accuracy to quantify different organic carbon (OC) species in defined mixtures of soil organic matter source compounds. We also used both methods to quantify different OC species in organic surface horizons of a Histic Leptosol as well as in mineral topsoil and subsoil horizons of two soils with different parent material, stage of pedogenesis, and OC content (Cambisol: 15–30 OC mgg−1, Podzol: 0.9–7 OC mgg−1). CPMAS 13C NMR spectroscopy was more accurate and precise (mean recovery of different C functional groups 96–103%) than C NEXAFS spectroscopy (mean recovery 92–113%). For organic surface and topsoil samples, NMR spectroscopy consistently yielded larger O-alkyl C percentages and smaller alkyl C percentages than C NEXAFS spectroscopy. For the Cambisol subsoil samples both methods performed well and showed similar C speciation results. NEXAFS spectroscopy yielded excellent spectra with a high signal-to-noise ratio also for OC-poor Podzol subsoil samples, whereas this was not the case for CPMAS 13C NMR spectroscopy even after sample treatment with HF. Our results confirm the analytical power of CPMAS 13C NMR spectroscopy for a reliable quantitative OC speciation in soils with >10mgOCg−1. Moreover, they highlight the potential of synchrotron-based C NEXAFS spectroscopy as fast, non-invasive method to semi-quantify different C functional groups in soils with low C content (0.9–10mgg−1). |
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We compared synchrotron-based C near-edge X-ray absorption fine structure (NEXAFS) and CPMAS 13C nuclear magnetic resonance (NMR) spectroscopy with respect to their precision and accuracy to quantify different organic carbon (OC) species in defined mixtures of soil organic matter source compounds. We also used both methods to quantify different OC species in organic surface horizons of a Histic Leptosol as well as in mineral topsoil and subsoil horizons of two soils with different parent material, stage of pedogenesis, and OC content (Cambisol: 15–30 OC mgg−1, Podzol: 0.9–7 OC mgg−1). CPMAS 13C NMR spectroscopy was more accurate and precise (mean recovery of different C functional groups 96–103%) than C NEXAFS spectroscopy (mean recovery 92–113%). For organic surface and topsoil samples, NMR spectroscopy consistently yielded larger O-alkyl C percentages and smaller alkyl C percentages than C NEXAFS spectroscopy. For the Cambisol subsoil samples both methods performed well and showed similar C speciation results. NEXAFS spectroscopy yielded excellent spectra with a high signal-to-noise ratio also for OC-poor Podzol subsoil samples, whereas this was not the case for CPMAS 13C NMR spectroscopy even after sample treatment with HF. Our results confirm the analytical power of CPMAS 13C NMR spectroscopy for a reliable quantitative OC speciation in soils with >10mgOCg−1. Moreover, they highlight the potential of synchrotron-based C NEXAFS spectroscopy as fast, non-invasive method to semi-quantify different C functional groups in soils with low C content (0.9–10mgg−1). |
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