TY - JOUR A1 - Rosner, Martin A1 - Vogl, Jochen T1 - New offset Delta11B isotope reference materials for geochemical and environmental boron isotope studies N2 - The isotopic composition of boron is a well established tool in various areas of Science and industries. Boron isotope compositions are typically reported as 6"B values which indicate the isotopic difference of a sample relative to the internationally accepted isotope reference material NIST SRM 951. A significant drawback of all of the available boron isotope reference materials is that non covers a natural boron isotope composition apart from NIST SRM 951. PY - 2011 SN - 1471-8022 VL - 75 IS - 3 SP - 1755 PB - Mineralogical Society of Great Britain and Ireland CY - London AN - OPUS4-32684 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - JOUR A1 - Seewald, J.S. A1 - Reeves, E.P. A1 - Bach, W. A1 - Saccocia, P.J. A1 - Craddock, P.R. A1 - Shanks III, W.C. A1 - Sylva, S.P. A1 - Pichler, T. A1 - Rosner, Martin A1 - Walsh, E. T1 - Submarine venting of magmatic volatiles in the Eastern Manus Basin, Papua New Guinea N2 - The SuSu Knolls and DESMOS hydrothermal fields are located in the back-arc extensional transform zone of the Eastern Manus Basin. In 2006, highly acidic and ΣSO4-rich vent fluids were collected at both sites and analyzed for the chemical and isotopic composition of major and trace species. Fluids exiting the seafloor have measured temperatures from 48 to 215 °C and are milky white in appearance due to precipitation of elemental S0. Vent fluid concentrations of Na, K, and Mg are depleted by as much as 30% relative to seawater, but have the same relative abundance. In contrast, the fluids are highly enriched in dissolved ΣCO2, Cl, SiO2(aq), Fe, and Al relative to seawater. Measured pH (25 °C) ranged from 0.95 to 1.87 and aqueous ΣSO4 ranged from 35 to 135 mmol/kg. The chemical and isotopic composition points to formation via subsurface mixing of seawater with a Na-, K-, Mg-, and Ca-free, volatile-rich magmatic fluid exsolved from subsurface magma bodies during a process analogous to subaerial fumarole discharge. Estimates of the magmatic end-member composition indicate a fluid phase where H2O > SO2 > CO2 ≈ Cl > F. The hydrogen and oxygen isotopic composition of H2O and carbon isotopic composition of ΣCO2 in the vent fluids strongly suggest a contribution of slab-derived H2O and CO2 to melts generated in the mantle beneath the Eastern Manus volcanic zone. Abundant magmatically-derived SO2 undergoes disproportionation during cooling in upflow zones and contributes abundant acidity, SO42-, and S0 to the venting fluids. Interaction of these highly acidic fluids with highly altered mineral assemblages in the upflow zone are responsible for extensive aqueous mobilization of SiO2(aq), Fe, and Al. Temporal variability in the speciation and abundance of aqueous S species between 1995 and 2006 at the DESMOS vent field suggests an increase in the relative abundance of SO2 in the magmatic end-member that has mixed with seawater in the subsurface. Results of this study constrain processes responsible for the formation of hot-spring fluids in magmatically active back-arc environments and the resulting chemical exchange between the lithosphere and water column. PY - 2015 DO - https://doi.org/10.1016/j.gca.2015.04.023 SN - 0016-7037 SN - 1872-9533 VL - 163 SP - 178 EP - 199 PB - Elsevier Science CY - New York, NY AN - OPUS4-33433 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - JOUR A1 - Rosner, Martin A1 - Wiedenbeck, M. A1 - Ludwig, T. T1 - Composition-induced variations in SIMS instrumental mass fractionation during boron isotope ratio measurements of silicate glasses N2 - An analytical artefact is reported here related to differences in instrumental mass fractionation between NIST SRM glasses and natural geological glasses during SIMS boron isotope determinations. The data presented demonstrated an average 3.4‰ difference between the NIST glasses and natural basaltic to rhyolitic glasses mainly in terms of their sputtering-induced fractionation of boron isotopes. As no matrix effect was found among basaltic to rhyolitic glasses, instrumental mass fractionation of most natural glass samples can be corrected by using appropriate glass reference materials. In order to confirm the existence of the compositionally induced variations in boron SIMS instrumental mass bias, the observed offset in SIMS instrumental mass bias has been independently reproduced in two laboratories and the phenomenon has been found to be stable over a period of more than one year. This study highlights the need for a close match between the chemical composition of the reference material and the samples being investigated. Nous montrons l'existence d'un artefact analytique reliéà différents fractionnements de masse instrumentaux, observés sur les verres NIST SRM et des verres naturels durant des mesures des isotopes de bore par SIMS. Les données montrent une différence d'environ 3.4‰ entre les verres NIST et les verres naturels, de composition variant de basaltique à rhyolitique, en termes de fractionnement des isotopes du bore principalement induit par le phénomène de dispersion. Comme aucun effet de matrice n'a été observé entre les verres basaltiques et les verres rhyolitiques, le fractionnement de masse instrumental de la plupart des verres naturels peut être corrigé en utilisant des verres de références appropriés. Dans le but de confirmer l'existence de biais de masse liéà la composition lors de mesure du bore par SIMS, nous avons reproduit indépendamment le décalage observé entre deux laboratoires et ce phénomène s'est révélé stable sur une période de plus d'un an. Cette étude met en lumière le besoin d'ajuster précisément les compositions chimiques des matériaux de référence et des échantillons à analyser. KW - Boron isotopes KW - SIMS KW - Matrix effect KW - Glass reference materials KW - Instrumental mass fractionation KW - Isotope du bore KW - Effet de matrice KW - Matériaux vitreux de référence KW - Fractionnement de masse instrumental PY - 2008 DO - https://doi.org/10.1111/j.1751-908X.2008.00875.x SN - 1639-4488 SN - 1751-908X VL - 32 IS - 1 SP - 27 EP - 38 PB - Blackwell CY - Oxford AN - OPUS4-17783 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - JOUR A1 - Rosner, Martin T1 - Geochemical and instrumental fundamentals for accurate and precise strontium isotope data of food samples: comment on "determination of the strontium isotope ration by ICP-MS ginseng as a tracer of regional origin" (Choi et al., 2008) N2 - The strontium isotope composition of food samples has been successfully used to trace the provenance of both herbal and animal agricultural products. Adequately accurate and precise 87Sr/86Sr ratios, however, are key to unravel environmental and anthropogenic strontium contributions of specific growing areas. In a recently published analytical method in Food Chemistry by Choi et al. (2008) a demonstrably inadequate protocol for the determination of 87Sr/86Sr ratios of ginseng is presented. Based on well established geological and analytical fundamentals the 87Sr/86Sr ratios presented by Choi et al. (2008) are too inaccurate and imprecise to be used to trace the origin of the ginseng. Appropriate wet chemical separation techniques and mass spectrometric instrumentation enables the generation of 87Sr/86Sr data with very low expanded uncertainties (<0.05%, k = 2). Those high quality data allow the identification of even small strontium contributions of source reservoirs or physical and anthropogenic processes if diagnostic isotope compositions are present. KW - Strontium isotopes KW - Food provenance studies KW - TIMS KW - ICP-MS KW - Analytical accuracy KW - Mass spectrometry PY - 2010 DO - https://doi.org/10.1016/j.foodchem.2010.01.019 SN - 0308-8146 VL - 121 IS - 3 SP - 918 EP - 921 PB - Elsevier CY - Amsterdam [u.a.] ; Jena AN - OPUS4-21325 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - JOUR A1 - Vogl, Jochen A1 - Rosner, Martin A1 - Pritzkow, Wolfgang T1 - Development and validation of a single collector SF-ICPMS procedure for the determination of boron isotope ratios in water and food samples N2 - Boron isotope studies on technical materials and geological and environmental samples are one hot topic in nowadays isotope research. Provenance studies of artefacts, food and other products might become another one, as several recent studies demonstrate. Typically boron isotope determinations have been carried out by TIMS. To open up this research field to a broader scientific community we developed two analytical procedures for boron isotope determinations based on single collector SF-ICPMS combined with a sample preparation procedure consisting of dry-ashing and a three step ion chromatographic boron-matrix separation. The developed procedures consist of one low resolution (LR) and one medium resolution (MR) procedure. The repeatability for the δ11B determination in three independently measured aliquots lies between 0.2 and 0.8‰ for the LR procedure and between 0.3 and 1.5‰ for the MR procedure. The expanded uncertainties with a coverage factor of k=2 range between 1.4 and 1.6‰ for the LR procedure and between 2.9 and 3.2‰ for the MR procedure. The accuracy, expressed as average deviation from the reference values, is 0.43‰ for the LR procedure and 0.33‰ for the MR procedure. To test the practicability of the procedures the matrix tolerance has been investigated as well and was found to be up to 2 mg kg-1 of alkaline and alkaline earth elements in the final measurement solution containing 100 µg kg-1 boron. Thus a highly efficient matrix separation for SF-ICPMS boron isotope determinations is required, similar to TIMS. PY - 2011 DO - https://doi.org/10.1039/c0ja00220h SN - 0267-9477 SN - 1364-5544 VL - 26 IS - 4 SP - 861 EP - 869 PB - Royal Society of Chemistry CY - London AN - OPUS4-23419 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - JOUR A1 - Gabitov, R.I. A1 - Schmitt, A.K. A1 - Rosner, Martin A1 - McKeegan, K.D. A1 - Gaetani, G.A. A1 - Cohen, A.L. A1 - Watson, E.B. A1 - Harrison, T.M. T1 - In situ delta7Li, Li/Ca, and Mg/Ca analyses of synthetic aragonites N2 - In situ secondary ion mass spectrometry (SIMS) analyses of δ7Li, Li/Ca, and Mg/Ca were performed on five synthetic aragonite samples precipitated from seawater at 25°C at different rates. The compositions of δ7Li in bulk aragonites and experimental fluids were measured by multicollector inductively coupled plasma–mass spectrometry (MC-ICP-MS). Both techniques yielded similar δ7Li in aragonite when SIMS analyses were corrected to calcium carbonate reference materials. Fractionation factors α7Li/6Li range from 0.9895 to 0.9923, which translates to a fractionation between aragonite and fluid from -10.5‰ to -7.7‰. The within-sample δ7Li range determined by SIMS is up to 27‰, exceeding the difference between bulk δ7Li analyses of different aragonite precipitates. Moreover, the centers of aragonite hemispherical bundles (spherulites) are enriched in Li/Ca and Mg/Ca relative to spherulite fibers by up to factors of 2 and 8, respectively. The Li/Ca and Mg/Ca ratios of spherulite fibers increase with aragonite precipitation rate. These results suggest that precipitation rate is a potentially important consideration when using Li isotopes and elemental ratios in natural carbonates as a proxy for seawater composition and temperature. KW - Lithium KW - Isotope KW - Aragonite KW - Rate KW - SIMS KW - Magnesium PY - 2011 DO - https://doi.org/10.1029/2010GC003322 SN - 1525-2027 VL - 12 IS - 3 (Technical Brief) SP - 1 EP - 16 CY - Washington, DC, USA AN - OPUS4-23312 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - JOUR A1 - Rosner, Martin A1 - Pritzkow, Wolfgang A1 - Vogl, Jochen A1 - Voerkelius, S. T1 - Development and validation of a method to determine the boron isotopic composition of crop plants N2 - We present a comprehensive chemical and mass spectrometric method to determine boron isotopic compositions of plant tissue. The method including dry ashing, a three-step ion chromatographic boron–matrix separation, and 11B/10B isotope ratio determinations using the Cs2BO2+ graphite technique has been validated using certified reference and quality control materials. The developed method is capable to determine δ11B values in plant tissue down to boron concentrations of 1 mg/kg with an expanded uncertainty of ≤1.7‰ (k = 2). The determined δ11B values reveal an enormous isotopic range of boron in plant tissues covering three-quarters of the natural terrestrial occurring variation in the boron isotopic composition. As the local environment and anthropogenic activity mainly control the boron intake of plants, the boron isotopic composition of plants can be used for food provenance studies. KW - Boron isotope variations KW - Delta-scale KW - Stable isotopes KW - Isotope reference materials KW - Provenance KW - Authenticity PY - 2011 DO - https://doi.org/10.1021/ac102836h SN - 0003-2700 SN - 1520-6882 VL - 83 IS - 7 SP - 2562 EP - 2568 PB - American Chemical Society CY - Washington, DC AN - OPUS4-23495 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - JOUR A1 - Vogl, Jochen A1 - Rosner, Martin A1 - Pritzkow, Wolfgang T1 - The need for new isotope reference materials N2 - Isotope reference materials are needed to calibrate and validate analytical procedures used for the determination of isotope amount ratios, procedurally defined isotope ratios or so-called δ values. In contrast to the huge analytical progress in isotope ratio analytics, the production of isotope reference materials has not kept pace with the increasing needs of isotope analysts. Three representative isotope systems are used to explain the technical and non-technical difficulties and drawbacks, on one hand, and to demonstrate what can be achieved at its best, on the other hand. A clear statement is given that new isotope reference materials are needed to obtain traceable and thus comparable data, which is essential for all kinds of isotope research. The range of available isotope reference materials and δ reference materials should be increased and matrix reference materials certified for isotope compositions or δ values, which do not exist yet, should be provided. KW - Isotope reference materials KW - Delta reference materials KW - Synthetic isotope mixtures KW - Mass spectrometry KW - Comparability KW - Traceability KW - Measurement uncertainty PY - 2013 DO - https://doi.org/10.1007/s00216-012-6605-3 SN - 1618-2642 SN - 1618-2650 VL - 405 IS - 9 SP - 2763 EP - 2770 PB - Springer CY - Berlin AN - OPUS4-28169 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - JOUR A1 - Vogl, Jochen A1 - Rosner, Martin T1 - Production and certification of a unique set of isotope and delta reference materials for Boron isotope determination in geochemical, environmental and industrial materials N2 - Isotopic reference materials are essential to enable reliable and comparable isotope data. In the case of boron only a very limited number of such materials is available, thus preventing adequate quality control of measurement results and validation of analytical procedures. To address this situation a unique set of two boron isotope reference materials (ERM-AE102a and -AE104a) and three offset δ11B reference materials (ERM-AE120, -AE121 and -AE122) were produced and certified. The present article describes the production and certification procedure in detail. The isotopic composition of all the materials was adjusted by mixing boron parent solutions enriched in 10B or 11B with a boron parent solution having a natural isotopic composition under full gravimetric control. All parent solutions were analysed for their boron concentration as well as their boron isotopic composition by thermal ionisation mass spectrometry (TIMS) using isotope dilution as the calibration technique. For all five reference materials the isotopic composition obtained on the basis of the gravimetric data agreed very well with the isotopic composition obtained from different TIMS techniques. Stability and homogeneity studies that were performed showed no significant influence on the isotopic composition or on the related uncertainties. The three reference materials ERM-AE120, ERM-AE121 and ERM-AE122 are the first reference materials with natural δ11B values not equal to 0‰. The certified δ11B values are -20.2‰ for ERM-AE120, 19.9‰ for ERM-AE121 and 39.7‰ for ERM-AE122, each with an expanded uncertainty (k = 2) of 0.6‰. These materials were produced to cover about three-quarters of the known natural boron isotope variation. The 10B enriched isotope reference materials ERM-AE102a and ERM-AE104a were produced for industrial applications utilising 10B for neutron shielding purposes. The certified 10B isotope abundances are 0.29995 for ERM-AE102a and 0.31488 for ERM-AE104a with expanded uncertainties (k = 2) of 0.00027 and 0.00028, respectively. Together with the formerly certified ERM-AE101 and ERM-AE103 a unique set of four isotope reference materials and three offset δ11B reference materials for boron isotope determination are now available from European Reference Materials. KW - Boron isotope variations KW - Delta-scale KW - Stable isotopes KW - Isotope reference materials KW - Delta reference materials KW - Metrology in chemistry KW - Absolute isotope abundance PY - 2012 DO - https://doi.org/10.1111/j.1751-908X.2011.00136.x SN - 1639-4488 SN - 1751-908X VL - 36 IS - 2 SP - 161 EP - 175 PB - Blackwell CY - Oxford AN - OPUS4-26260 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - JOUR A1 - Rosner, Martin A1 - Vogl, Jochen T1 - Bor: Isotopenverhältnisse und die Herkunft einer Probe N2 - Die Industrie nutzt die Borisotopenanalytik in nukleartechnischen Anwendungen. Umwelt- und Geowissenschaften identifizieren anhand der Borisotopenverhältnisse Kontaminationsquellen und charakterisieren Mischungs- und Fraktionsprozesse. In der Lebensmittelanalytik dient der Parameter dazu, Herkunft und Anbauweise von Obst und Gemüse herauszufinden. Seit kurzem gibt es dafür ein validiertes Verfahren und erste Referenzdaten. KW - Isotopenverhältnisse KW - Herkunft KW - TIMS PY - 2012 SN - 1439-9598 SN - 1521-3854 VL - 60 IS - 2 SP - 147 EP - 149 PB - Wiley-VCH Verl. CY - Weinheim AN - OPUS4-25575 LA - deu AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - JOUR A1 - Shanmugam, Sankaran A1 - Peterlechner, Martin A1 - Iskandar, Mohamad Riza A1 - Saikia, Ujjal A1 - Kulitckii, Vladislav A1 - Lipińska-Chwałek, Marta A1 - Mayer, Joachim A1 - Rösner, Harald A1 - Hickel, Tilmann A1 - Divinski, Sergiy V. A1 - Wilde, Gerhard T1 - Coherent twin-oriented Al3Sc-based precipitates in Al matrix N2 - Al3(Sc,Zr,Ti) nanoparticles with an ideal twin-type orientation relationship to Al host matrix were found in cold-rolled and subsequently annealed Al-based alloy. Atomic-scale investigations using high-resolution scanning transmission electron microscopy identified particles that form prominent coherent (111) twin-type interfaces along their longer facets and semi-coherent twin interfaces on their shorter facets. Ab-initio calculations showed that a coherent Al/Al3Sc twin-like phase boundary corresponds to a local energy minimum. A model is proposed explaining the formation of the twin orientation relationship of an Al3Sc nanoparticle with the Al host matrix. KW - Al-based alloy KW - Precipitation KW - Twin orientation relationship KW - Ab initio calculations KW - Transition electron microscopy PY - 2023 DO - https://doi.org/10.1016/j.scriptamat.2023.115351 SN - 1359-6462 VL - 229 SP - 1 EP - 6 PB - Elsevier BV AN - OPUS4-58789 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER -