Environmental variability in the reactivity of freshwater dissolved organic carbon to UV-B
Abstract Reductions in the global stratospheric ozone layer arethought to be increasing the amount of ultraviolet B (UV-B) radiationreaching the planet’s surface and may be affecting the chemistry ofdissolved organic carbon (DOC) in surface waters. We studied theabundance of chromophores in DOC coll...
Ausführliche Beschreibung
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
1997 |
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| Umfang: |
9 |
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| Reproduktion: |
Springer Online Journal Archives 1860-2002 |
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| Übergeordnetes Werk: |
in: Biogeochemistry - 1984, 36(1997) vom: Jan., Seite 89-97 |
| Übergeordnetes Werk: |
volume:36 ; year:1997 ; month:01 ; pages:89-97 ; extent:9 |
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NLEJ193206382 |
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| 520 | |a Abstract Reductions in the global stratospheric ozone layer arethought to be increasing the amount of ultraviolet B (UV-B) radiationreaching the planet’s surface and may be affecting the chemistry ofdissolved organic carbon (DOC) in surface waters. We studied theabundance of chromophores in DOC collected in four different aquaticenvironments in southwestern Nova Scotia using 13C nuclearmagnetic resonance (13C NMR) spectroscopy. We showed a clearseasonal pattern in the distribution of structural carbon related tolight-sensitive chromophores. There seemed to be little variation in theUV-B related chemical structure of DOC between lakes and streams, thoughwater from a bog pool showed large differences from the other samples. Thesepatterns of potential UV-B reactivity tend to be dampened however, byvariations in DOC concentrations which also occur seasonally. | ||
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(DE-627)NLEJ193206382 DE-627 ger DE-627 rakwb eng Environmental variability in the reactivity of freshwater dissolved organic carbon to UV-B 1997 9 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract Reductions in the global stratospheric ozone layer arethought to be increasing the amount of ultraviolet B (UV-B) radiationreaching the planet’s surface and may be affecting the chemistry ofdissolved organic carbon (DOC) in surface waters. We studied theabundance of chromophores in DOC collected in four different aquaticenvironments in southwestern Nova Scotia using 13C nuclearmagnetic resonance (13C NMR) spectroscopy. We showed a clearseasonal pattern in the distribution of structural carbon related tolight-sensitive chromophores. There seemed to be little variation in theUV-B related chemical structure of DOC between lakes and streams, thoughwater from a bog pool showed large differences from the other samples. Thesepatterns of potential UV-B reactivity tend to be dampened however, byvariations in DOC concentrations which also occur seasonally. Springer Online Journal Archives 1860-2002 Clair, Thomas A. oth Sayer, Brian G. oth in Biogeochemistry 1984 36(1997) vom: Jan., Seite 89-97 (DE-627)NLEJ188983856 (DE-600)1478541-9 1573-515X nnns volume:36 year:1997 month:01 pages:89-97 extent:9 http://dx.doi.org/10.1023/A:1005735929568 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 36 1997 1 89-97 9 |
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(DE-627)NLEJ193206382 DE-627 ger DE-627 rakwb eng Environmental variability in the reactivity of freshwater dissolved organic carbon to UV-B 1997 9 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract Reductions in the global stratospheric ozone layer arethought to be increasing the amount of ultraviolet B (UV-B) radiationreaching the planet’s surface and may be affecting the chemistry ofdissolved organic carbon (DOC) in surface waters. We studied theabundance of chromophores in DOC collected in four different aquaticenvironments in southwestern Nova Scotia using 13C nuclearmagnetic resonance (13C NMR) spectroscopy. We showed a clearseasonal pattern in the distribution of structural carbon related tolight-sensitive chromophores. There seemed to be little variation in theUV-B related chemical structure of DOC between lakes and streams, thoughwater from a bog pool showed large differences from the other samples. Thesepatterns of potential UV-B reactivity tend to be dampened however, byvariations in DOC concentrations which also occur seasonally. Springer Online Journal Archives 1860-2002 Clair, Thomas A. oth Sayer, Brian G. oth in Biogeochemistry 1984 36(1997) vom: Jan., Seite 89-97 (DE-627)NLEJ188983856 (DE-600)1478541-9 1573-515X nnns volume:36 year:1997 month:01 pages:89-97 extent:9 http://dx.doi.org/10.1023/A:1005735929568 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 36 1997 1 89-97 9 |
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(DE-627)NLEJ193206382 DE-627 ger DE-627 rakwb eng Environmental variability in the reactivity of freshwater dissolved organic carbon to UV-B 1997 9 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract Reductions in the global stratospheric ozone layer arethought to be increasing the amount of ultraviolet B (UV-B) radiationreaching the planet’s surface and may be affecting the chemistry ofdissolved organic carbon (DOC) in surface waters. We studied theabundance of chromophores in DOC collected in four different aquaticenvironments in southwestern Nova Scotia using 13C nuclearmagnetic resonance (13C NMR) spectroscopy. We showed a clearseasonal pattern in the distribution of structural carbon related tolight-sensitive chromophores. There seemed to be little variation in theUV-B related chemical structure of DOC between lakes and streams, thoughwater from a bog pool showed large differences from the other samples. Thesepatterns of potential UV-B reactivity tend to be dampened however, byvariations in DOC concentrations which also occur seasonally. Springer Online Journal Archives 1860-2002 Clair, Thomas A. oth Sayer, Brian G. oth in Biogeochemistry 1984 36(1997) vom: Jan., Seite 89-97 (DE-627)NLEJ188983856 (DE-600)1478541-9 1573-515X nnns volume:36 year:1997 month:01 pages:89-97 extent:9 http://dx.doi.org/10.1023/A:1005735929568 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 36 1997 1 89-97 9 |
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(DE-627)NLEJ193206382 DE-627 ger DE-627 rakwb eng Environmental variability in the reactivity of freshwater dissolved organic carbon to UV-B 1997 9 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract Reductions in the global stratospheric ozone layer arethought to be increasing the amount of ultraviolet B (UV-B) radiationreaching the planet’s surface and may be affecting the chemistry ofdissolved organic carbon (DOC) in surface waters. We studied theabundance of chromophores in DOC collected in four different aquaticenvironments in southwestern Nova Scotia using 13C nuclearmagnetic resonance (13C NMR) spectroscopy. We showed a clearseasonal pattern in the distribution of structural carbon related tolight-sensitive chromophores. There seemed to be little variation in theUV-B related chemical structure of DOC between lakes and streams, thoughwater from a bog pool showed large differences from the other samples. Thesepatterns of potential UV-B reactivity tend to be dampened however, byvariations in DOC concentrations which also occur seasonally. Springer Online Journal Archives 1860-2002 Clair, Thomas A. oth Sayer, Brian G. oth in Biogeochemistry 1984 36(1997) vom: Jan., Seite 89-97 (DE-627)NLEJ188983856 (DE-600)1478541-9 1573-515X nnns volume:36 year:1997 month:01 pages:89-97 extent:9 http://dx.doi.org/10.1023/A:1005735929568 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 36 1997 1 89-97 9 |
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(DE-627)NLEJ193206382 DE-627 ger DE-627 rakwb eng Environmental variability in the reactivity of freshwater dissolved organic carbon to UV-B 1997 9 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract Reductions in the global stratospheric ozone layer arethought to be increasing the amount of ultraviolet B (UV-B) radiationreaching the planet’s surface and may be affecting the chemistry ofdissolved organic carbon (DOC) in surface waters. We studied theabundance of chromophores in DOC collected in four different aquaticenvironments in southwestern Nova Scotia using 13C nuclearmagnetic resonance (13C NMR) spectroscopy. We showed a clearseasonal pattern in the distribution of structural carbon related tolight-sensitive chromophores. There seemed to be little variation in theUV-B related chemical structure of DOC between lakes and streams, thoughwater from a bog pool showed large differences from the other samples. Thesepatterns of potential UV-B reactivity tend to be dampened however, byvariations in DOC concentrations which also occur seasonally. Springer Online Journal Archives 1860-2002 Clair, Thomas A. oth Sayer, Brian G. oth in Biogeochemistry 1984 36(1997) vom: Jan., Seite 89-97 (DE-627)NLEJ188983856 (DE-600)1478541-9 1573-515X nnns volume:36 year:1997 month:01 pages:89-97 extent:9 http://dx.doi.org/10.1023/A:1005735929568 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 36 1997 1 89-97 9 |
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environmental variability in the reactivity of freshwater dissolved organic carbon to uv-b |
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Environmental variability in the reactivity of freshwater dissolved organic carbon to UV-B |
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Abstract Reductions in the global stratospheric ozone layer arethought to be increasing the amount of ultraviolet B (UV-B) radiationreaching the planet’s surface and may be affecting the chemistry ofdissolved organic carbon (DOC) in surface waters. We studied theabundance of chromophores in DOC collected in four different aquaticenvironments in southwestern Nova Scotia using 13C nuclearmagnetic resonance (13C NMR) spectroscopy. We showed a clearseasonal pattern in the distribution of structural carbon related tolight-sensitive chromophores. There seemed to be little variation in theUV-B related chemical structure of DOC between lakes and streams, thoughwater from a bog pool showed large differences from the other samples. Thesepatterns of potential UV-B reactivity tend to be dampened however, byvariations in DOC concentrations which also occur seasonally. |
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Abstract Reductions in the global stratospheric ozone layer arethought to be increasing the amount of ultraviolet B (UV-B) radiationreaching the planet’s surface and may be affecting the chemistry ofdissolved organic carbon (DOC) in surface waters. We studied theabundance of chromophores in DOC collected in four different aquaticenvironments in southwestern Nova Scotia using 13C nuclearmagnetic resonance (13C NMR) spectroscopy. We showed a clearseasonal pattern in the distribution of structural carbon related tolight-sensitive chromophores. There seemed to be little variation in theUV-B related chemical structure of DOC between lakes and streams, thoughwater from a bog pool showed large differences from the other samples. Thesepatterns of potential UV-B reactivity tend to be dampened however, byvariations in DOC concentrations which also occur seasonally. |
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Abstract Reductions in the global stratospheric ozone layer arethought to be increasing the amount of ultraviolet B (UV-B) radiationreaching the planet’s surface and may be affecting the chemistry ofdissolved organic carbon (DOC) in surface waters. We studied theabundance of chromophores in DOC collected in four different aquaticenvironments in southwestern Nova Scotia using 13C nuclearmagnetic resonance (13C NMR) spectroscopy. We showed a clearseasonal pattern in the distribution of structural carbon related tolight-sensitive chromophores. There seemed to be little variation in theUV-B related chemical structure of DOC between lakes and streams, thoughwater from a bog pool showed large differences from the other samples. Thesepatterns of potential UV-B reactivity tend to be dampened however, byvariations in DOC concentrations which also occur seasonally. |
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