Wolf, Inken

[["dc.bibliographiccitation.firstpage","229"],["dc.bibliographiccitation.issue","2"],["dc.bibliographiccitation.journal","Soil Biology and Biochemistry"],["dc.bibliographiccitation.lastpage","239"],["dc.bibliographiccitation.volume","32"],["dc.contributor.author","Wolf, I."],["dc.contributor.author","Russow, R."],["dc.date.accessioned","2018-11-07T10:54:51Z"],["dc.date.available","2018-11-07T10:54:51Z"],["dc.date.issued","2000"],["dc.description.abstract","The use of N-15 tracer provides a suitable technique to investigate the processes of N transformation in soils and the origin of the environmentally relevant gaseous N compounds N2O and NO from nitrification and denitrification. incubation experiments with black earth soil under two different water contents are presented here. Nitrification and denitrification proceeded simultaneously, but the importance of these two microbial processes shifted depending on the water content of the soil. Under water-unsaturated conditions the microbial oxidation of NH4+ to NO3- predominated, but a reduction of NO3- also occurred. The emission of NO exceeded the emission of N2O by a factor of up to 20 at the beginning of the experiments. Under water-saturated conditions denitrification was the dominant process of N transformation in the soil. However, nitrification also occurred to a considerable extent. The emission of N2O was greater than under unsaturated conditions. The formation of NO could hardly be observed. N loss by molecular nitrogen from denitrification could be detected under saturated conditions. The N loss amounted to 60% of NO3- and thereby the cumulative N ratio of N-2 to N2O was 3. Under either unsaturated or saturated conditions NO arose from NO2- or during the microbial oxidation of NH4+ to NO2-. However, N2O mainly formed from denitrification under both conditions. Furthermore, NO could not be observed as a precursor of N2O and the free NO2- could not be detected as a common N pool for the formation of N2O and NO. High emissions of NO could be a problem for the black earth soil in the semi-arid climate in central Germany, if there are large amounts of NH4+ in the soil after fertilisation. (C) 2000 Elsevier Science Ltd. All rights reserved."],["dc.identifier.doi","10.1016/S0038-0717(99)00151-0"],["dc.identifier.isi","000085418700011"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/49658"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Pergamon-elsevier Science Ltd"],["dc.relation.issn","0038-0717"],["dc.title","Different pathways of formation of N2O, N-2 and NO in black earth soil"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","93"],["dc.bibliographiccitation.issue","2"],["dc.bibliographiccitation.journal","Forensische Psychiatrie, Psychologie, Kriminologie"],["dc.bibliographiccitation.lastpage","125"],["dc.bibliographiccitation.volume","12"],["dc.contributor.author","Müller, J. L."],["dc.contributor.author","Saimeh, N."],["dc.contributor.author","Briken, P."],["dc.contributor.author","Eucker, S."],["dc.contributor.author","Hoffmann, K."],["dc.contributor.author","Koller, M."],["dc.contributor.author","Wolf, T."],["dc.contributor.author","Dudeck, M."],["dc.contributor.author","Hartl, C."],["dc.contributor.author","Jakovljevic, A.-K."],["dc.contributor.author","Klein, V."],["dc.contributor.author","Knecht, G."],["dc.contributor.author","Müller-Isberner, R."],["dc.contributor.author","Muysers, J."],["dc.contributor.author","Schiltz, K."],["dc.contributor.author","Seifert, D."],["dc.contributor.author","Simon, A."],["dc.contributor.author","Steinböck, H."],["dc.contributor.author","Stuckmann, W."],["dc.contributor.author","Weissbeck, W."],["dc.contributor.author","Wiesemann, C."],["dc.contributor.author","Zeidler, R."],["dc.date.accessioned","2020-12-10T14:14:19Z"],["dc.date.available","2020-12-10T14:14:19Z"],["dc.date.issued","2017"],["dc.identifier.doi","10.1007/s11757-017-0445-0"],["dc.identifier.eissn","1862-7080"],["dc.identifier.issn","1862-7072"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/71323"],["dc.language.iso","de"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","Standards für die Behandlung im Maßregelvollzug nach §§ 63 und 64 StGB"],["dc.title.alternative","Standards for treatment in forensic commitment according to § 63 and § 64 of the German criminal code. Interdisciplinary task force of the DGPPN"],["dc.title.subtitle","Interdisziplinäre Task-Force der DGPPN"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1"],["dc.bibliographiccitation.issue","S1"],["dc.bibliographiccitation.journal","Der Nervenarzt"],["dc.bibliographiccitation.lastpage","29"],["dc.bibliographiccitation.volume","88"],["dc.contributor.author","Müller, J. L."],["dc.contributor.author","Saimeh, N."],["dc.contributor.author","Briken, P."],["dc.contributor.author","Eucker, S."],["dc.contributor.author","Hoffmann, K."],["dc.contributor.author","Koller, M."],["dc.contributor.author","Wolf, T."],["dc.contributor.author","Dudeck, M."],["dc.contributor.author","Hartl, C."],["dc.contributor.author","Jakovljevic, A.-K."],["dc.contributor.author","Klein, V."],["dc.contributor.author","Knecht, G."],["dc.contributor.author","Müller-Isberner, R."],["dc.contributor.author","Muysers, J."],["dc.contributor.author","Schiltz, K."],["dc.contributor.author","Seifert, D."],["dc.contributor.author","Simon, A."],["dc.contributor.author","Steinböck, H."],["dc.contributor.author","Stuckmann, W."],["dc.contributor.author","Weissbeck, W."],["dc.contributor.author","Wiesemann, C."],["dc.contributor.author","Zeidler, R."],["dc.date.accessioned","2020-12-10T14:08:34Z"],["dc.date.available","2020-12-10T14:08:34Z"],["dc.date.issued","2017"],["dc.identifier.doi","10.1007/s00115-017-0382-3"],["dc.identifier.eissn","1433-0407"],["dc.identifier.issn","0028-2804"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/70487"],["dc.language.iso","de"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","Standards für die Behandlung im Maßregelvollzug nach §§ 63 und 64 StGB"],["dc.title.alternative","Standards for treatment in forensic committment according to § 63 and § 64 of the German criminal code. Interdisciplinary task force of the DGPPN"],["dc.title.subtitle","Interdisziplinäre Task-Force der DGPPN"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1862"],["dc.bibliographiccitation.issue","6"],["dc.bibliographiccitation.journal","Soil Science Society of America Journal"],["dc.bibliographiccitation.lastpage","1868"],["dc.bibliographiccitation.volume","67"],["dc.contributor.author","Wolf, I."],["dc.contributor.author","Brumme, Rainer"],["dc.date.accessioned","2018-11-07T10:35:17Z"],["dc.date.available","2018-11-07T10:35:17Z"],["dc.date.issued","2003"],["dc.description.abstract","A (15)N tracer study was conducted to determine N(2) and N(2)O fluxes and the processes responsible for the formation of N(2)O in two beech (Fagus silvatica L.) forest soils: an acid mineral soil (AM) (pH=3.8) and the overlying acid forest floor (AFF) (pH=3.8) from the Soiling and a less acid mineral soil (LAM) (pH=5.2) from the Gottinger Wald. Ammonium and nitrate of undisturbed soil cores were labeled by injecting (15)N. The evolved gases, N(2)O and N(2), and the ammonium and nitrate concentrations in the soils were measured together with the (15)N abundances over a period of 8 d. Nitrous Oxide was produced in all soils by denitrification. Nitrate was reduced to N(2) at higher soil pH (LAM) and in the AFF. The end product of denitrification at the lower soil pH (AM) was N(2)O The N(2)O and N(2) emission calculated on an areal basis decreased from LAM, AFF, to AM. The N(2)O/(N(2)O+N(2)) ratios decreased from AM (1.0), AFF (0.97), to LAM (0.80) during the initial period indicating that the main product of denitrification was N(2)O. On prolonged incubation the N(2)O/(N(2)O+N(2)) ratios decreased for AFF and LAM to 0.78 and 0.32, respectively, and was attributed to a gradual decrease in nitrate concentration. We estimate the in situ N(2) emissions to he 0.71 and 0.51 kg N ha(-1) yr(-1) for the Gottinger Wald and the Solling, using published annual in situ N(2)O emissions and our N(2)/N(2)O ratios. The in situ N(2)O emissions of the Gottinger Wald and Solling are 0.17 and 3 kg ha(-1) yr(-1) and the N(2) emissions increased the annual denitrification losses to about 0.88 and 3.51 kg ha(-1) yr(-1). The approach for estimating in situ N(2) emissions has to be improved in future studies."],["dc.identifier.isi","000186450500027"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/45059"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Soil Sci Soc Amer"],["dc.relation.issn","0361-5995"],["dc.title","Dinitrogen and nitrous oxide formation in beech forest floor and mineral soils"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","e340"],["dc.bibliographiccitation.issue","6"],["dc.bibliographiccitation.journal","British Journal of Dermatology"],["dc.bibliographiccitation.lastpage","e343"],["dc.bibliographiccitation.volume","177"],["dc.contributor.author","Ralser, D.J."],["dc.contributor.author","Lestringant, G.G."],["dc.contributor.author","Du-Thanh, A."],["dc.contributor.author","Kokordelis, P."],["dc.contributor.author","Fischer, J."],["dc.contributor.author","Basmanav, F.B.Ünalan"],["dc.contributor.author","Wolf, S."],["dc.contributor.author","Thiele, H."],["dc.contributor.author","Altmüller, J."],["dc.contributor.author","Nürnberg, P."],["dc.contributor.author","Oji, V."],["dc.contributor.author","Fritz, G."],["dc.contributor.author","Frank, J."],["dc.contributor.author","Betz, R.C."],["dc.date.accessioned","2020-12-10T18:26:59Z"],["dc.date.available","2020-12-10T18:26:59Z"],["dc.date.issued","2017"],["dc.identifier.doi","10.1111/bjd.16024"],["dc.identifier.issn","0007-0963"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/76216"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","Functional implications of novel ADAM10 mutations in reticulate acropigmentation of Kitamura"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","678"],["dc.bibliographiccitation.issue","6"],["dc.bibliographiccitation.journal","JOURNAL OF PLANT NUTRITION AND SOIL SCIENCE-ZEITSCHRIFT FUR PFLANZENERNAHRUNG UND BODENKUNDE"],["dc.bibliographiccitation.lastpage","684"],["dc.bibliographiccitation.volume","167"],["dc.contributor.author","Ludwig, B."],["dc.contributor.author","Wolf, I."],["dc.contributor.author","Teepe, R."],["dc.date.accessioned","2018-11-07T10:43:31Z"],["dc.date.available","2018-11-07T10:43:31Z"],["dc.date.issued","2004"],["dc.description.abstract","The amounts of N2O released in freeze-thaw events depend on site and freezing conditions and contribute considerably to the annual N2O emissions. However, quantitative information on the N transformation rates in freeze-thaw events is scarce. Our objectives were (1) to quantify gross nitrification in a Luvisol during a freeze-thaw event, (2) to analyze the dynamics of the emissions of N2O and N-2, (3) to quantify the contribution of nitrification and denitrification to the emission of N2O, and (4) to determine whether the length of freezing and of thawing affects the C availability for the denitrification. (NO3-)-N-15 was added to undisturbed soil columns, and the columns were subjected to 7 d of freezing and 5 d of thawing. N2O emissions were determined in 3 h intervals, and the concentrations of (N2O)-N-15 and N-15(2) were determined at different times during thawing. During the 12 d experiment, 5.67 mg NO3--N (kg soil)(-1) was produced, and 2.67 mg NO3--N (kg soil)(-1) was lost. By assuming as a first approximation that production and loss occurred exclusively during thawing, the average nitrate-production rate, denitrification rate, and immobilization rate were 1.13, 0.05, and 0.48 mg NO3--N (kg soil)(-1) d(-1), respectively. Immediately after the beginning of the thawing, denitrification contributed by 83% to the N2O production. The ratios of N-15(2) to (N2O)-N-15 during thawing were narrow and ranged from 1.5 to 0.6. For objective (4), homogenized soil samples were incubated under anaerobic conditions after different periods of freezing and thawing. The different periods did not affect the amounts of N-2 and N2O produced in the incubation experiments. Further, addition of labile substrates gave either increases in the amounts of N2O and N-2 produced or no changes which suggested that changes in nutrient availability due to freezing and thawing are only small."],["dc.identifier.doi","10.1002/jpln.200421462"],["dc.identifier.isi","000225871600003"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/47072"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Wiley-v C H Verlag Gmbh"],["dc.relation.issn","1436-8730"],["dc.title","Contribution of nitrification and denitrification to the emission of N2O in a freeze-thaw event in an agricultural soil"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.issue","4"],["dc.bibliographiccitation.journal","British Journal of Dermatology"],["dc.bibliographiccitation.volume","178"],["dc.contributor.author","Humbatova, A."],["dc.contributor.author","Maroofian, R."],["dc.contributor.author","Romano, M.‐T."],["dc.contributor.author","Tafazzoli, A."],["dc.contributor.author","Behnam, M."],["dc.contributor.author","Dilaver, N."],["dc.contributor.author","Nouri, N."],["dc.contributor.author","Salehi, M."],["dc.contributor.author","Wolf, S."],["dc.contributor.author","Frank, J."],["dc.contributor.author","Kokordelis, P."],["dc.contributor.author","Betz, R.C."],["dc.date.accessioned","2020-12-10T18:26:59Z"],["dc.date.available","2020-12-10T18:26:59Z"],["dc.date.issued","2018"],["dc.identifier.doi","10.1111/bjd.16276"],["dc.identifier.eissn","1365-2133"],["dc.identifier.issn","0007-0963"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/76217"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","An insertion mutation in HOXC 13 underlies pure hair and nail ectodermal dysplasia with lacrimal duct obstruction"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1356"],["dc.bibliographiccitation.issue","15"],["dc.bibliographiccitation.journal","Rapid Communications in Mass Spectrometry"],["dc.bibliographiccitation.lastpage","1360"],["dc.bibliographiccitation.volume","14"],["dc.contributor.author","Yamulki, S."],["dc.contributor.author","Wolf, I."],["dc.contributor.author","Bol, R."],["dc.contributor.author","Grant, B."],["dc.contributor.author","Brumme, Rainer"],["dc.contributor.author","Veldkamp, Edzo"],["dc.contributor.author","Jarvis, S. C."],["dc.date.accessioned","2017-09-07T11:43:33Z"],["dc.date.available","2017-09-07T11:43:33Z"],["dc.date.issued","2002"],["dc.identifier.doi","10.1002/1097-0231(20000815)14:15<1356"],["dc.identifier.gro","3150176"],["dc.identifier.pmid","10920355"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/6912"],["dc.language.iso","en"],["dc.notes.status","zu prüfen"],["dc.relation.issn","0951-4198"],["dc.title","Effects of dung and urine amendments on the isotopic content of N2O released from grasslands"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dc.type.peerReviewed","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.artnumber","PII S0038-0717(02)00001-9"],["dc.bibliographiccitation.firstpage","741"],["dc.bibliographiccitation.issue","5"],["dc.bibliographiccitation.journal","Soil Biology and Biochemistry"],["dc.bibliographiccitation.lastpage","744"],["dc.bibliographiccitation.volume","34"],["dc.contributor.author","Wolf, I."],["dc.contributor.author","Brumme, Rainer"],["dc.date.accessioned","2018-11-07T10:30:27Z"],["dc.date.available","2018-11-07T10:30:27Z"],["dc.date.issued","2002"],["dc.description.abstract","A N-15 tracer field experiment was carried out in an acid soil of a beech forest gap at the Solling area in Germany to determine the different formation processes of N2O. This site has been classified as a seasonal N2O emission type forest. Small amounts of highly enriched N-15 tracer were supplied separately as labelled NH4+ and NO3- seven times from May to October 1998. The N-15 compounds were injected with syringes into the upper 10 cm of the soil. The N2O emission showed a seasonal pattern with low emission in spring, high emission in summer, and low emission in autumn and followed the soil temperature. N2O was evolved only from the N-15-labelled NO3- pool in summer under field moist conditions, indicating that its formation was due to denitrification. In spring, early summer and autumn trapped NO or heterotrophic nitrification may also have been involved in N2O emission. (C) 2002 Elsevier Science Ltd. All rights reserved."],["dc.identifier.doi","10.1016/S0038-0717(02)00001-9"],["dc.identifier.isi","000175658800023"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/43873"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Pergamon-elsevier Science Ltd"],["dc.relation.issn","0038-0717"],["dc.title","Contribution of nitrification and denitrification sources for seasonal N2O emissions in an acid German forest soil"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]