Surma, Jakub

[["dc.bibliographiccitation.firstpage","401"],["dc.bibliographiccitation.lastpage","428"],["dc.contributor.author","Surma, Jakub"],["dc.contributor.author","Assonov, Sergey"],["dc.contributor.author","Staubwasser, Michael"],["dc.contributor.editor","Bindeman, Ilya"],["dc.contributor.editor","Pack, Andreas"],["dc.date.accessioned","2021-10-01T09:58:16Z"],["dc.date.available","2021-10-01T09:58:16Z"],["dc.date.issued","2021"],["dc.identifier.doi","10.2138/rmg.2021.86.12"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/90028"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-469"],["dc.publisher","Mineralogical Society of America"],["dc.publisher.place","Chantilly, Virginia"],["dc.relation.ispartof","Triple oxygen isotope geochemistry"],["dc.title","Triple Oxygen Isotope Systematics in the Hydrologic Cycle"],["dc.type","book_chapter"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","7403"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Scientific reports"],["dc.bibliographiccitation.volume","9"],["dc.contributor.author","Surma, J."],["dc.contributor.author","Assonov, S."],["dc.contributor.author","Herwartz, D."],["dc.contributor.author","Voigt, C."],["dc.contributor.author","Staubwasser, M."],["dc.date.accessioned","2019-07-24T07:06:39Z"],["dc.date.available","2019-07-24T07:06:39Z"],["dc.date.issued","2019-05-09"],["dc.description.abstract","A correction to this article has been published and is linked from the HTML and PDF versions of this paper. The error has not been fixed in the paper."],["dc.identifier.doi","10.1038/s41598-019-43264-w"],["dc.identifier.pmid","31068607"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/61956"],["dc.language.iso","en"],["dc.relation.eissn","2045-2322"],["dc.relation.issn","2045-2322"],["dc.title","Author Correction: The evolution of 17O-excess in surface water of the arid environment during recharge and evaporation"],["dc.type","journal_article"],["dc.type.internalPublication","no"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.journal","Rapid Communications in Mass Spectrometry : RCM"],["dc.contributor.author","Adnew, Getachew A."],["dc.contributor.author","Hofmann, Magdalena E. G."],["dc.contributor.author","Paul, Dipayan"],["dc.contributor.author","Laskar, Amzad"],["dc.contributor.author","Surma, Jakub"],["dc.contributor.author","Albrecht, Nina"],["dc.contributor.author","Pack, Andreas"],["dc.contributor.author","Schwieters, Johannes"],["dc.contributor.author","Koren, Gerbrand"],["dc.contributor.author","Peters, Wouter"],["dc.contributor.author","Röckmann, Thomas"],["dc.date.accessioned","2019-07-24T06:59:58Z"],["dc.date.available","2019-07-24T06:59:58Z"],["dc.date.issued","2019"],["dc.description.abstract","Determination of δ17 O values directly from CO2 with traditional gas source isotope ratio mass spectrometry is not possible due to isobaric interference of 13 C16 O16 O on 12 C17 O16 O. The methods developed so far use either chemical conversion or isotope equilibration to determine the δ17 O value of CO2 . In addition, δ13 C measurements require correction for the interference from 12 C17 O16 O on 13 C16 O16 O since it is not possible to resolve the two isotopologues."],["dc.identifier.doi","10.1002/rcm.8478"],["dc.identifier.pmid","31063233"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/16564"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/61954"],["dc.language.iso","en"],["dc.notes.intern","Merged from goescholar"],["dc.notes.intern","In goescholar not merged with http://resolver.sub.uni-goettingen.de/purl?gs-1/16764 but duplicate"],["dc.relation.eissn","1097-0231"],["dc.relation.issn","0951-4198"],["dc.relation.issn","1097-0231"],["dc.rights","CC BY 4.0"],["dc.rights.access","openAccess"],["dc.rights.uri","https://creativecommons.org/licenses/by/4.0"],["dc.subject.ddc","550"],["dc.title","Determination of the triple oxygen and carbon isotopic composition of CO2 from atomic ion fragments formed in the ion source of the 253 Ultra High-Resolution Isotope Ratio Mass Spectrometer"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","4972"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Scientific reports"],["dc.bibliographiccitation.volume","8"],["dc.contributor.author","Surma, J."],["dc.contributor.author","Assonov, S."],["dc.contributor.author","Herwartz, D."],["dc.contributor.author","Voigt, C."],["dc.contributor.author","Staubwasser, M."],["dc.date.accessioned","2019-07-24T07:04:37Z"],["dc.date.available","2019-07-24T07:04:37Z"],["dc.date.issued","2018-03-21"],["dc.description.abstract","This study demonstrates the potential of triple O-isotopes to quantify evaporation with recharge on a salt lake from the Atacama Desert, Chile. An evaporative gradient was found in shallow ponds along a subsurface flow-path from a groundwater source. Total dissolved solids (TDS) increased by 177 g/l along with an increase in δ18O by 16.2‰ and in δD by 65‰. 17O-excess decreased by 79 per meg, d-excess by 55‰. Relative humidity (h), evaporation over inflow (E/I), the isotopic composition of vapor ( R V ) and of inflowing water ( R WI ) determine the isotope distribution in 17O-excess over δ18O along a well-defined evaporation curve as the classic Craig-Gordon model predicts. A complementary on-site simple (pan) evaporation experiment over a change in TDS, δ18O, and 17O-excess by 392 g/l, 25.0‰, and -130 per meg, respectively, was used to determine the effects of sluggish brine evaporation and of wind turbulence. These effects translate to uncertainty in E/I rather than h. The local composition of R V relative to R WI pre-determines the general ability to resolve changes in h. The triple O-isotope system is useful for quantitative hydrological balancing of lakes and for paleo-humidity reconstruction, particularly if complemented by D/H analysis."],["dc.identifier.doi","10.1038/s41598-018-23151-6"],["dc.identifier.pmid","29563523"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/61955"],["dc.language.iso","en"],["dc.relation.eissn","2045-2322"],["dc.relation.issn","2045-2322"],["dc.title","The evolution of 17O-excess in surface water of the arid environment during recharge and evaporation"],["dc.type","journal_article"],["dc.type.internalPublication","no"],["dspace.entity.type","Publication"]]