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Kovács, Kristóf
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Kovács, Kristóf
Official Name
Kovács, Kristóf
Alternative Name
Kovács, K.
Kovacs, Kristof
Kovacs, K.
Kóvacs, Kristóf
Kóvacs, K.
Main Affiliation
Now showing 1 - 5 of 5
2006Journal Article [["dc.bibliographiccitation.firstpage","321"],["dc.bibliographiccitation.issue","3"],["dc.bibliographiccitation.journal","Journal of Neurology, Neurosurgery & Psychiatry"],["dc.bibliographiccitation.lastpage","323"],["dc.bibliographiccitation.volume","78"],["dc.contributor.author","Kovacs, T"],["dc.contributor.author","Beck, J A"],["dc.contributor.author","Papp, M I"],["dc.contributor.author","Lantos, P L"],["dc.contributor.author","Aranyi, Z"],["dc.contributor.author","Szirmai, I G"],["dc.contributor.author","Farsang, M"],["dc.contributor.author","Stuke, A"],["dc.contributor.author","Csillik, A"],["dc.contributor.author","Collinge, J"],["dc.date.accessioned","2022-10-06T13:25:48Z"],["dc.date.available","2022-10-06T13:25:48Z"],["dc.date.issued","2006"],["dc.identifier.doi","10.1136/jnnp.2006.104372"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/114917"],["dc.language.iso","en"],["dc.notes.intern","DOI-Import GROB-602"],["dc.relation.issn","0022-3050"],["dc.relation.orgunit","Deutsches Primatenzentrum"],["dc.title","Familial prion disease in a Hungarian family with a novel 144-base pair insertion in the prion protein gene"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dspace.entity.type","Publication"]]Details DOI2016Journal Article [["dc.bibliographiccitation.firstpage","91"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Regional Environmental Change"],["dc.bibliographiccitation.lastpage","103"],["dc.bibliographiccitation.volume","18"],["dc.contributor.author","Lamparter, Gabriele"],["dc.contributor.author","Nobrega, Rodolfo Luiz Bezerra"],["dc.contributor.author","Kovacs, Kristof"],["dc.contributor.author","Amorim, Ricardo Santos"],["dc.contributor.author","Gerold, Gerhard"],["dc.date.accessioned","2020-12-10T14:11:11Z"],["dc.date.available","2020-12-10T14:11:11Z"],["dc.date.issued","2016"],["dc.identifier.doi","10.1007/s10113-016-1015-2"],["dc.identifier.eissn","1436-378X"],["dc.identifier.issn","1436-3798"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/70992"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","Modelling hydrological impacts of agricultural expansion in two macro-catchments in Southern Amazonia, Brazil"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]Details DOI2017Journal Article [["dc.bibliographiccitation.artnumber","e0179414"],["dc.bibliographiccitation.issue","6"],["dc.bibliographiccitation.journal","PLoS ONE"],["dc.bibliographiccitation.volume","12"],["dc.contributor.author","Nobrega, Rodolfo L. B."],["dc.contributor.author","Guzha, Alphonce C."],["dc.contributor.author","Torres, Gilmar N."],["dc.contributor.author","Kovacs, Kristof"],["dc.contributor.author","Lamparter, Gabriele"],["dc.contributor.author","Amorim, Ricardo S. S."],["dc.contributor.author","Couto, Eduardo"],["dc.contributor.author","Gerold, Gerhard"],["dc.date.accessioned","2018-11-07T10:22:43Z"],["dc.date.available","2018-11-07T10:22:43Z"],["dc.date.issued","2017"],["dc.description.abstract","Understanding the impacts of land-use change on landscape-hydrological dynamics is one of the main challenges in the Northern Brazilian Cerrado biome, where the Amazon agricultural frontier is located. Motivated by the gap in literature assessing these impacts, we characterized the soil hydro-physical properties and quantified surface water fluxes from catchments under contrasting land-use in this region. We used data from field measurements in two headwater micro-catchments with similar physical characteristics and different land use, i.e. cerrado sensu stricto vegetation and pasture for extensive cattle ranching. We determined hydraulic and physical properties of the soils, applied ground-based remote sensing techniques to estimate evapotranspiration, and monitored streamflow from October 2012 to September 2014. Our results show significant differences in soil hydro-physical properties between the catchments, with greater bulk density and smaller total porosity in the pasture catchment. We found that evapotranspiration is smaller in the pasture ( 639 +/- 31% mm yr(-1)) than in the cerrado catchment ( 1,004 +/- 24% mm yr(-1)), and that streamflow from the pasture catchment is greater with runoff coefficients of 0.40 for the pasture and 0.27 for the cerrado catchment. Overall, our results confirm that conversion of cerrado vegetation to pasture causes soil hydro-physical properties deterioration, reduction in evapotranspiration reduction, and increased streamflow."],["dc.description.sponsorship","Open-Access-Publikationsfonds 2017"],["dc.identifier.doi","10.1371/journal.pone.0179414"],["dc.identifier.isi","000403274700035"],["dc.identifier.pmid","28609462"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/14556"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/42326"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","PUB_WoS_Import"],["dc.publisher","Public Library Science"],["dc.relation.issn","1932-6203"],["dc.relation.orgunit","Fakultät für Geowissenschaften und Geographie"],["dc.rights","CC BY 4.0"],["dc.rights.uri","https://creativecommons.org/licenses/by/4.0/"],["dc.title","Effects of conversion of native cerrado vegetation to pasture on soil hydro-physical properties, evapotranspiration and streamflow on the Amazonian agricultural frontier"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]Details DOI PMID PMC WOS2015Journal Article [["dc.bibliographiccitation.firstpage","508"],["dc.bibliographiccitation.issue","4"],["dc.bibliographiccitation.journal","Hydrological Processes"],["dc.bibliographiccitation.lastpage","521"],["dc.bibliographiccitation.volume","29"],["dc.contributor.author","Guzha, Alphonce C."],["dc.contributor.author","Nobrega, Rodolfo L. B."],["dc.contributor.author","Kovacs, Kristof"],["dc.contributor.author","Rebola-Lichtenberg, Jessica"],["dc.contributor.author","Amorim, Ricardo S. S."],["dc.contributor.author","Gerold, Gerhard"],["dc.date.accessioned","2018-11-07T10:00:55Z"],["dc.date.available","2018-11-07T10:00:55Z"],["dc.date.issued","2015"],["dc.description.abstract","On the basis of interactions between landscape characteristics and precipitation inputs, watersheds respond differently to different climatic inputs. The objective of this study was to quantitatively characterize controls on runoff generation from two first order micro-catchments in the Amazonia region. The study investigated the variation of hydrological signatures at micro-catchment scale and related these to landscape and land cover differences and weather descriptors that control the observed responses. One catchment is a pasture cleared of all natural vegetation in the early 1980s, and the second catchment is a primary tropical forest with minor signs of disturbance. Water levels and meteorological variables were continuously monitored during the study period (December 2012-May 2013). Water level measurements were converted to discharge, evapotranspiration was quantified using Penman-Monteith equation and catchment pedohydrological properties were also determined. During the study period, mean total rainfall was 1200mm, and direct runoff ratios were 0.29 and 0.12 for the pasture and forest catchments, respectively. Base flow index was relatively high in the forest catchment (0.76) compared with pasture catchment (0.63). Results from this study showed that the pasture catchment had a 35% higher mean stream flow. Analysis of selected individual rainstorm events also showed peak discharges, which were attained much faster in the pasture catchment compared with the forest catchment. At both sites, rainfall-runoff responses were highly dependent on surface and subsurface flow generation. Overland flow was observed in the pasture site during intense rainfall events. The pasture catchment exhibited higher event water contribution than the forest catchment. Findings from this research suggest that shallow lateral pathways play a significant role in controlling runoff generation processes in the forest catchment, whereas infiltration excess runoff generation processes dominate in the pasture catchment. The findings in this study suggest that the conversion of forest to pasture may lead to important changes in runoff generation processes and water storage in these head water catchments. Copyright (c) 2014 John Wiley & Sons, Ltd."],["dc.identifier.doi","10.1002/hyp.10161"],["dc.identifier.isi","000347848900003"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/37909"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Wiley-blackwell"],["dc.relation.issn","1099-1085"],["dc.relation.issn","0885-6087"],["dc.title","Characterizing rainfall-runoff signatures from micro-catchments with contrasting land cover characteristics in southern Amazonia"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]Details DOI WOS2017Journal Article Research Paper [["dc.bibliographiccitation.artnumber","e0182188"],["dc.bibliographiccitation.issue","7"],["dc.bibliographiccitation.journal","PloS one"],["dc.bibliographiccitation.volume","12"],["dc.contributor.author","Zeppenfeld, Thorsten"],["dc.contributor.author","Balkenhol, Niko"],["dc.contributor.author","Kovács, Kristóf"],["dc.contributor.author","Carminati, Andrea"],["dc.date.accessioned","2019-07-09T11:43:30Z"],["dc.date.available","2019-07-09T11:43:30Z"],["dc.date.issued","2017"],["dc.description.abstract","The ability to acquire water from the soil is a major driver in interspecific plant competition and it depends on several root functional traits. One of these traits is the excretion of gel-like compounds (mucilage) that modify physical soil properties. Mucilage secreted by roots becomes hydrophobic upon drying, impedes the rewetting of the soil close to the root, the so called rhizosphere, and reduces water availability to plants. The function of rhizosphere hydrophobicity is not easily understandable when looking at a single plant, but it may constitute a competitive advantage at the ecosystem level. We hypothesize that by making the top soil hydrophobic, deep-rooted plants avoid competititon with shallow-rooted plants. To test this hypothesis we used an individual-based model to simulate water uptake and growth of two virtual plant species, one deep-rooted plant capable of making the soil hydrophobic and a shallow-rooted plant. We ran scenarios with different precipitation regimes ranging from dry to wet (350, 700, and 1400 mm total annual precipitation) and from high to low precipitation frequencies (1, 7, and 14 days). Plant species abundance and biomass were chosen as indicators for competitiveness of plant species. At constant precipitation frequency mucilage hydrophobicity lead to a benefit in biomass and abundance of the tap-rooted population. Under wet conditions this effect diminished and tap-rooted plants were less productive. Without this trait both species coexisted. The effect of root exudation trait remained constant under different precipitation frequencies. This study shows that mucilage secretion is a competitive trait for the acquisition of water. This advantage is achieved by the modification of the soil hydraulic properties and specifically by inducing water repellency in soil regions which are shared with other species."],["dc.identifier.doi","10.1371/journal.pone.0182188"],["dc.identifier.pmid","28753673"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/14545"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/58896"],["dc.language.iso","en"],["dc.notes.intern","Merged from goescholar"],["dc.relation.issn","1932-6203"],["dc.relation.orgunit","Abteilung Wildtierwissenschaften"],["dc.rights","CC BY 4.0"],["dc.rights.uri","https://creativecommons.org/licenses/by/4.0/"],["dc.subject.ddc","550"],["dc.title","Rhizosphere hydrophobicity: A positive trait in the competition for water."],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]Details DOI PMID PMC