TY - JOUR A1 - Reinsch, Martin A1 - Töpfer, Antje A1 - Lehmann, Andreas A1 - Nehls, Irene T1 - Determination of ochratoxin A in wine by liquid chromatography tandem mass spectrometry after combined anion-exchange/reversed-phase clean-up JF - Analytical and bioanalytical chemistry N2 - Ochratoxin A (OTA) is a mycotoxin produced by Aspergillus ochraceus and Penicillium verrucosum. It has been found and analysed in several foods and feeds. Owing to its toxicity and occurrence in food and feed, the European Community has issued directives and some countries have their own regulations for OTA contents in food, feed and beverages. This work describes a method for the determination of OTA in mulled and red wine. It is based on combined anion exchange/reversed-phase clean-up and was analysed by liquid chromatography coupled with tandem mass spectrometry (multiple reaction monitoring). The method was validated with natural contaminated and spiked wine samples with OTA contents from 1.34 to 3.48 g kg–1. Owing to its accuracy, good reproducibility and repeatability, this easy method is a good alternative to liquid chromatography–fluorescence detection methods. KW - Ochratoxin A KW - Wine KW - Tandem mass spectrometry KW - Solid-phase extraction KW - Anion exchange KW - Liquid chromatography PY - 2005 DO - https://doi.org/10.1007/s00216-005-3097-4 SN - 1618-2642 SN - 1618-2650 VL - 381 IS - 8 SP - 1592 EP - 1595 PB - Springer CY - Berlin AN - OPUS4-10306 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - JOUR A1 - Wanner, C. A1 - Poethig, R. A1 - Carrero, S. A1 - Fernandez-Martinez, A. A1 - Jäger, Christian A1 - Furrer, G. T1 - Natural occurrence of nanocrystalline Al-hydroxysulfates: Insights on formation, Al solubility control and As retention JF - Geochimica et Cosmochimica Acta N2 - Nanocrystalline basaluminite [Al4OH10(SO4)(H2O)3–5] and Aggregation of the e-Keggin polyoxocation [Al12(AlO4)(OH)24(H2O)12]7+, referred to as Al13, have both been described to form in acid mine Drainage environments. Although the chemical composition is quite similar, their crystalline varieties significantly differ, demonstrating that various types of Al-hydroxysulfates can form under similar conditions and that their respective formation is not fully understood yet. Here, we report the occurrence of nanocrystalline precipitates that form naturally in a small alpine catchment in Switzerland where an acidic mountainous stream (pH 4) is neutralized successively after mixing with several neutral tributaries. The stepwise neutralization in conjunction with the large amount of precipitates provide an ideal setting for obtaining new insights into (i) the structure of naturally forming Al-hydroxysulfates, (ii) their formation mechanism, (iii) their role in controlling the solubility of Al, and (iv) their ability to lower the mobility of As. Synchrotron-based high-energy X-ray diffraction and subsequent pair distribution function analyses demonstrate that these precipitates are structurally identical to basaluminite samples obtained from acid mine drainage sites. In contrast, only minor amounts of tetrahedrally coordinated Al, as present in Al13, were identified by nuclear magnetic resonance spectroscopy. The precipitates are further characterized by elevated As concentrations up to 600 lg/g, whereas other heavy metals are at background concentrations only. Given the low As concentrations in the stream from which precipitation occurs (<0.03 mg/L), high As concentrations confirm that basaluminite serves as a highly efficient As sink, which is attributed to its high anion-exchange capacity. Chemical analysis of streamwater samples in combination with geochemical modeling show that precipitation occurs instantaneously upon mixing with neutral streams. Moreover, our data reveal that the precipitation of basaluminite exerts a strong solubility control on dissolved Al concentrations as manifested by the quasi-constant basaluminite ion activity product observed during neutralization from pH 5 to pH 5.9. We hypothesize that in our field system, high fluoride and sulfate concentrations on the order of 100 and 1–2 mg/L, KW - Basaluminite KW - Al13 KW - Acid rock drainage KW - Arsenic retention KW - Aluminum KW - Anion exchange PY - 2018 DO - https://doi.org/10.1016/j.gca.2018.06.031 SN - 0016-7037 SN - 1872-9533 VL - 238 SP - 252 EP - 269 PB - Elsevier Ltd. AN - OPUS4-46164 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER -