Dynamics and underlying processes of N2O and NO soil-atmosphere exchange under extreme meteorological boundary conditions

Climate models predict an increasing frequency and intensity of summer drought periods with subsequent heavy rainfall or soil frost and thaw events in mountain regions of Central Europe. These indirect effects of global warming may considerably influence soil microbial processes and in consequence e...
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Autor*in:	Goldberg, Stefanie D. - 1982- [verfasserIn]
Hochschulschrift:	Bayreuth, Univ., Diss., 2009

Format:	E-Book
Sprache:	Englisch

Erschienen:	2009

Schlagwörter:	Stickstoffkreislauf / Bodenanalyse
Formangabe:	Hochschulschrift

Systematik:	WI 5020

Anmerkung:	Enth. außerdem 5 Papers
Umfang:	Online-Ressource (179 S., 5,22 MB)

Links:	Link aufrufen Volltext Volltext Volltext Volltext Volltext

DOI / URN:	urn:nbn:de:bvb:703-opus-5377

Katalog-ID:	594706130

Internformat


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Indexfelder

author_variant	s d g sd sdg
matchkey_str	goldbergstefanied:2009----:yaisnudrynpoessf2adooltopeexhneneeteeee
oclc_num	643146129
hierarchy_sort_str	2009
bklnumber	43.47 43.50
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allfields	urn:nbn:de:bvb:703-opus-5377 urn (DE-627)594706130 (DE-576)9594706139 (DE-599)BVBBV035364937 (OCoLC)643146129 (DE-604)BV035364937 DE-627 ger DE-627 rakwb eng XA-DE 550 DNB 16,13 ssgn WI 5020 BVB rvk (DE-625)rvk/148869: 43.47 bkl 43.50 bkl Goldberg, Stefanie D. 1982- verfasserin (DE-588)137692072 (DE-627)594844282 (DE-576)304845051 aut Dynamics and underlying processes of N2O and NO soil-atmosphere exchange under extreme meteorological boundary conditions vorgelegt von Stefanie D. Goldberg 2009 Online-Ressource (179 S., 5,22 MB) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Enth. außerdem 5 Papers Bayreuth, Univ., Diss., 2009 Climate models predict an increasing frequency and intensity of summer drought periods with subsequent heavy rainfall or soil frost and thaw events in mountain regions of Central Europe. These indirect effects of global warming may considerably influence soil microbial processes and in consequence emissions of climate-relevant trace gases. Regarding the nitrogen cycle, N2O and NO emissions are of concern, since they are involved in climate warming and soils represent a main source for these two gases. In spite of a growing number of studies on this subject, knowledge on effects of climate change on soil N2O and NO emissions is still scarce. This is mainly due to a hitherto poor mechanistic understanding of underlying processes within soil. In this thesis, the impact of extreme meteorological boundary conditions on N2O and NO fluxes in a Norway spruce forest and an acidic fen in the Fichtelgebirge area was investigated. The summer drought period and precipitation were experimentally increased in the forest and the fen over a 2-year span. Soil frost was induced in the forest by removal of the natural snow cover. The experiments were run in three replicates each and non-manipulated plots served as controls. Throughout the experiments, N2O and NO fluxes were recorded in weekly to monthly intervals. In addition, N2O concentrations and isotope signatures in soil air were measured along soil profiles to identify and localise the underlying biogenic production and consumption processes. Prolonged drought continuously reduced the N2O emission from the forest soil and even turned the soil temporarily into a sink for atmospheric N2O. Soil freezing and thawing caused a burst of N2O release contributing 84 % of the annual emission ... 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spelling	urn:nbn:de:bvb:703-opus-5377 urn (DE-627)594706130 (DE-576)9594706139 (DE-599)BVBBV035364937 (OCoLC)643146129 (DE-604)BV035364937 DE-627 ger DE-627 rakwb eng XA-DE 550 DNB 16,13 ssgn WI 5020 BVB rvk (DE-625)rvk/148869: 43.47 bkl 43.50 bkl Goldberg, Stefanie D. 1982- verfasserin (DE-588)137692072 (DE-627)594844282 (DE-576)304845051 aut Dynamics and underlying processes of N2O and NO soil-atmosphere exchange under extreme meteorological boundary conditions vorgelegt von Stefanie D. Goldberg 2009 Online-Ressource (179 S., 5,22 MB) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Enth. außerdem 5 Papers Bayreuth, Univ., Diss., 2009 Climate models predict an increasing frequency and intensity of summer drought periods with subsequent heavy rainfall or soil frost and thaw events in mountain regions of Central Europe. These indirect effects of global warming may considerably influence soil microbial processes and in consequence emissions of climate-relevant trace gases. Regarding the nitrogen cycle, N2O and NO emissions are of concern, since they are involved in climate warming and soils represent a main source for these two gases. In spite of a growing number of studies on this subject, knowledge on effects of climate change on soil N2O and NO emissions is still scarce. This is mainly due to a hitherto poor mechanistic understanding of underlying processes within soil. In this thesis, the impact of extreme meteorological boundary conditions on N2O and NO fluxes in a Norway spruce forest and an acidic fen in the Fichtelgebirge area was investigated. The summer drought period and precipitation were experimentally increased in the forest and the fen over a 2-year span. Soil frost was induced in the forest by removal of the natural snow cover. The experiments were run in three replicates each and non-manipulated plots served as controls. Throughout the experiments, N2O and NO fluxes were recorded in weekly to monthly intervals. In addition, N2O concentrations and isotope signatures in soil air were measured along soil profiles to identify and localise the underlying biogenic production and consumption processes. Prolonged drought continuously reduced the N2O emission from the forest soil and even turned the soil temporarily into a sink for atmospheric N2O. Soil freezing and thawing caused a burst of N2O release contributing 84 % of the annual emission ... 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These indirect effects of global warming may considerably influence soil microbial processes and in consequence emissions of climate-relevant trace gases. Regarding the nitrogen cycle, N2O and NO emissions are of concern, since they are involved in climate warming and soils represent a main source for these two gases. In spite of a growing number of studies on this subject, knowledge on effects of climate change on soil N2O and NO emissions is still scarce. This is mainly due to a hitherto poor mechanistic understanding of underlying processes within soil. In this thesis, the impact of extreme meteorological boundary conditions on N2O and NO fluxes in a Norway spruce forest and an acidic fen in the Fichtelgebirge area was investigated. The summer drought period and precipitation were experimentally increased in the forest and the fen over a 2-year span. Soil frost was induced in the forest by removal of the natural snow cover. The experiments were run in three replicates each and non-manipulated plots served as controls. Throughout the experiments, N2O and NO fluxes were recorded in weekly to monthly intervals. In addition, N2O concentrations and isotope signatures in soil air were measured along soil profiles to identify and localise the underlying biogenic production and consumption processes. Prolonged drought continuously reduced the N2O emission from the forest soil and even turned the soil temporarily into a sink for atmospheric N2O. Soil freezing and thawing caused a burst of N2O release contributing 84 % of the annual emission ... 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title_sort	dynamics and underlying processes of n2o and no soil-atmosphere exchange under extreme meteorological boundary conditions
title_auth	Dynamics and underlying processes of N2O and NO soil-atmosphere exchange under extreme meteorological boundary conditions
abstract	Climate models predict an increasing frequency and intensity of summer drought periods with subsequent heavy rainfall or soil frost and thaw events in mountain regions of Central Europe. These indirect effects of global warming may considerably influence soil microbial processes and in consequence emissions of climate-relevant trace gases. Regarding the nitrogen cycle, N2O and NO emissions are of concern, since they are involved in climate warming and soils represent a main source for these two gases. In spite of a growing number of studies on this subject, knowledge on effects of climate change on soil N2O and NO emissions is still scarce. This is mainly due to a hitherto poor mechanistic understanding of underlying processes within soil. In this thesis, the impact of extreme meteorological boundary conditions on N2O and NO fluxes in a Norway spruce forest and an acidic fen in the Fichtelgebirge area was investigated. The summer drought period and precipitation were experimentally increased in the forest and the fen over a 2-year span. Soil frost was induced in the forest by removal of the natural snow cover. The experiments were run in three replicates each and non-manipulated plots served as controls. Throughout the experiments, N2O and NO fluxes were recorded in weekly to monthly intervals. In addition, N2O concentrations and isotope signatures in soil air were measured along soil profiles to identify and localise the underlying biogenic production and consumption processes. Prolonged drought continuously reduced the N2O emission from the forest soil and even turned the soil temporarily into a sink for atmospheric N2O. Soil freezing and thawing caused a burst of N2O release contributing 84 % of the annual emission ... Enth. außerdem 5 Papers
abstractGer	Climate models predict an increasing frequency and intensity of summer drought periods with subsequent heavy rainfall or soil frost and thaw events in mountain regions of Central Europe. These indirect effects of global warming may considerably influence soil microbial processes and in consequence emissions of climate-relevant trace gases. Regarding the nitrogen cycle, N2O and NO emissions are of concern, since they are involved in climate warming and soils represent a main source for these two gases. In spite of a growing number of studies on this subject, knowledge on effects of climate change on soil N2O and NO emissions is still scarce. This is mainly due to a hitherto poor mechanistic understanding of underlying processes within soil. In this thesis, the impact of extreme meteorological boundary conditions on N2O and NO fluxes in a Norway spruce forest and an acidic fen in the Fichtelgebirge area was investigated. The summer drought period and precipitation were experimentally increased in the forest and the fen over a 2-year span. Soil frost was induced in the forest by removal of the natural snow cover. The experiments were run in three replicates each and non-manipulated plots served as controls. Throughout the experiments, N2O and NO fluxes were recorded in weekly to monthly intervals. In addition, N2O concentrations and isotope signatures in soil air were measured along soil profiles to identify and localise the underlying biogenic production and consumption processes. Prolonged drought continuously reduced the N2O emission from the forest soil and even turned the soil temporarily into a sink for atmospheric N2O. Soil freezing and thawing caused a burst of N2O release contributing 84 % of the annual emission ... Enth. außerdem 5 Papers
abstract_unstemmed	Climate models predict an increasing frequency and intensity of summer drought periods with subsequent heavy rainfall or soil frost and thaw events in mountain regions of Central Europe. These indirect effects of global warming may considerably influence soil microbial processes and in consequence emissions of climate-relevant trace gases. Regarding the nitrogen cycle, N2O and NO emissions are of concern, since they are involved in climate warming and soils represent a main source for these two gases. In spite of a growing number of studies on this subject, knowledge on effects of climate change on soil N2O and NO emissions is still scarce. This is mainly due to a hitherto poor mechanistic understanding of underlying processes within soil. In this thesis, the impact of extreme meteorological boundary conditions on N2O and NO fluxes in a Norway spruce forest and an acidic fen in the Fichtelgebirge area was investigated. The summer drought period and precipitation were experimentally increased in the forest and the fen over a 2-year span. Soil frost was induced in the forest by removal of the natural snow cover. The experiments were run in three replicates each and non-manipulated plots served as controls. Throughout the experiments, N2O and NO fluxes were recorded in weekly to monthly intervals. In addition, N2O concentrations and isotope signatures in soil air were measured along soil profiles to identify and localise the underlying biogenic production and consumption processes. Prolonged drought continuously reduced the N2O emission from the forest soil and even turned the soil temporarily into a sink for atmospheric N2O. Soil freezing and thawing caused a burst of N2O release contributing 84 % of the annual emission ... Enth. außerdem 5 Papers
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title_short	Dynamics and underlying processes of N2O and NO soil-atmosphere exchange under extreme meteorological boundary conditions
url	https://edocs.tib.eu/files/e01dd10/594706130.pdf http://opus.ub.uni-bayreuth.de/volltexte/2009/537 http://opus.ub.uni-bayreuth.de/volltexte/2009/537/pdf/DissGoldberg.pdf http://d-nb.info/99332410X/34 http://nbn-resolving.de/urn:nbn:de:bvb:703-opus-5377
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GND_txt_mv	Goldberg, Stefanie Goldberg, Stefanie D. Hochschulschrift Stickstoffdynamik Stickstoff / Kreislauf Stickstoffkreislauf Bodenanalytik Bodenuntersuchung Boden / Analyse Bodenanalyse
GND_txtF_mv	Goldberg, Stefanie Goldberg, Stefanie D. Hochschulschrift Stickstoffdynamik Stickstoff / Kreislauf Stickstoffkreislauf Bodenanalytik Bodenuntersuchung Boden / Analyse Bodenanalyse
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up_date	2024-07-04T07:20:25.575Z
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Dynamics and underlying processes of N2O and NO soil-atmosphere exchange under extreme meteorological boundary conditions

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