540 Chemie und zugeordnete Wissenschaften
Refine
Year of publication
Document Type
- Article (983)
- Doctoral Thesis (597)
- Book (22)
- Contribution to a Periodical (16)
- Preprint (12)
- Conference Proceeding (11)
- Report (9)
- Review (5)
- diplomthesis (3)
- Diploma Thesis (2)
Has Fulltext
- yes (1664)
Is part of the Bibliography
- no (1664)
Keywords
- crystal structure (39)
- Crystal Structure (24)
- Synthesis (15)
- ESR Spectra (14)
- NMR spectroscopy (14)
- RNA (14)
- hydrogen bonding (11)
- IR Spectra (10)
- NMR (10)
- SARS-CoV-2 (9)
Institute
- Biochemie und Chemie (1122)
- Biochemie, Chemie und Pharmazie (247)
- Pharmazie (151)
- Zentrum für Biomolekulare Magnetische Resonanz (BMRZ) (47)
- Biowissenschaften (37)
- Medizin (35)
- Physik (31)
- Präsidium (27)
- Exzellenzcluster Makromolekulare Komplexe (18)
- MPI für Biophysik (15)
Einfache elektrochemische Methode zur Bestimmung von Chlorit in wässrigen und nicht-wässrigen Systemen Stoffe bzw. Verbindungen, welche nachweislich krebserregend oder fruchtbarkeitsschädigend sind, werden seit Jahren, insbesondere durch die WHO, streng reguliert. Zu diesen Stoffen zählt u. a. Chlorit, welches als Abbauprodukt in Desinfektionsmitteln, Poolwassern und im Rahmen von organischen Oxidationsprozessen vorkommt. Im Rahmen des Projektes sollte eine elektrochemische Methode zu Detektion von Chlorit in wässrigen und organischen Proben entwickelt werden, wobei auf eine Glaskohlenstoffelektrode in Kombination mit Li [NTf]2 im Wässrigen und [Bmpyrr][NTf]2/MeOH im Organischen als Elektrolyten zurückgegriffen wurden.
Bei der Methodenentwicklung wurde auf Differentielle-Puls-Voltammetrie zurückgegriffen, da diese im Vergleich zum Cyclovoltammetrie deutlich empfindlicher ist. Die Methodenvalidierung nach ICH-Guidelines konnte erfolgreich durchgeführt werden Dabei konnte im Wässrigen eine Nachweisgrenze von 0.07 mg L-1 (Organisch: 0.20 mg L-1) erhalten werden. Beide lagen deutlich unter den WHO-Grenzwerten von 0.7 mg L-1. Die Selektivität/Interferenz wurde gegenüber den übrigen Chlor-Spezies getestet; für alle Spezies, außer Hypochlorit, konnten für die Wiederfindungsrate von Chlorit Werte nahe 100% erhalten werden. Die entwickelte Methode konnte erfolgreich auf wässrige (Poolproben, Desinfektionsmittel) und organische Proben (aus Pinnick-Synthesen) angewendet werden. Insbesondere durch die Anwendung im Bereich der Pinnick-Oxidation war der Sensor für mögliche In-Line-Analytik geeignet. Bei den organischen Proben konnte zudem die ionische Flüssigkeit zu 92% zurückgewonnen werden, was den Elektrolyten in Hinblick auf Nachhaltigkeit und Wirtschaftlichkeit noch attraktiver macht.
Entwicklung ionenchromatographischer Methoden zur Detektion von Chloroxo-Spezies
Der Bedarf an schnellen, kostengünstigen Analysemethoden, welche den Vorgaben der einzelnen Behörden weltweit entsprechen, ist in den letzten Jahren enorm gestiegen. Im Rahmen des Projektes sollte eine ionenchromatographische Methode (IC) entwickelt werden, welche neben den Chloroxo-Spezies (Chlorid, Hypochlorit, Chlorit, Chlorat und Perchlorat) auch die bekannten Standardionen (Fluorid, Bromid, Nitrat, Phosphat, Sulfat, Iodid) nachweisbar macht. Zunächst gelang es, die Methodenparameter zu optimieren und so die Chloro-Spezies, außer Hypochlorit, von den übrigen Standardanionen innerhalb von 50 Minuten vollständig zu trennen. Die Methode konnte in der weiteren Entwicklung sogar noch um die Detergenzien-Anionen Acetat, Formiat, Oxalat und Tartrat erweitert werden. (ASupp 7, 45 °C, 0.8 mL min-1, 6 mmol L-1 Na2CO3 / 1 mmol L-1 NaHCO3 + 10% Acetonitril). Auch alle notwendigen Validierungsparameter konnten erfolgreich bestimmt werden. Zuletzt war es möglich, erfolgreich unterschiedliche Realproben zu vermessen.
Da ein Nachweis von Hypochlorit mittels IC nicht möglich war, wurden weitere Anstrengung unternommen, dieses Anion mittels IC-PCR (Nachsäulenderivatisierung) nachzuweisen. Als Detektionsprinzip wurde dabei auf eine Bromat-Nachweis-Methode mittels UV/VIS zurückgegriffen, welche im Rahmen des Projektes angepasst wurde. Da davon ausgegangen werden muss, dass das Hypochlorit mit reaktiven Stellen innerhalb des Säulenmaterials reagiert und somit nicht mehr detektiert werden kann, wurden Passivierungsexperimente an der Vorsäule und Säule für 24 h mit einer Hypochlorit-NaOH-Mischung durchgeführt. Nach 60 Stunden Passivierung konnten erstmals reproduzierbare Ergebnisse bei dem Nachweis von OCl- erhalten werden. Zuletzt konnten erfolgreich fünf unterschiedliche Realproben vermessen und der Hypochlorit-Gehalt mit bisher angewandten Methoden verglichen werden, wobei die erhaltenen Werte in der gleichen Größenordnung lagen.
Entwicklung eines Sensors unter Verwendung der Viologen-Grundstruktur auf metallischen Oberflächen
Früher fanden Viologene und deren Derivate Anwendung im Bereich der Schädlingsbekämpfung und wurden hauptsächlich als Kontaktherbizid verwendet. Mittlerweile hat sich das Anwendungsspektrum der Viologene deutlich verändert, u.a. werden die in organischen Redox-Fluss-Batterien als Elektrolyte eingesetzt. Im Rahmen diesen Projekts wurden mehrere bekannte Viologen-Grundkörper (u. A. Methylviologen (MV)) vollständig elektrochemisch charakterisiert Im Anschluss wurde MV mit unterschiedlichen Ankergruppen (Thiol-, Sulfonat, -Phosphonat-, Carboxylanker) modifiziert und auf metallische Oberfläche (u. A. Gold und Kupfer) abgeschieden mit dem Ziel ein neues Sensor-Motiv für die Analytik zu entwickeln. Der Thiolanker konnte erfolgreich auf Gold, der Carboxylanker erfolgreich auf Kupfer abgeschieden werden. Die anschließenden elektrochemischen Untersuchungen der abgeschiedenen Monolagen ergaben jedoch eine geringe Stabilität der Anker in wässriger und organischer Umgebung, sodass in Zukunft weitere Anstrengungen unternommen werden müssen, die Stabilität des Viologensystems auf der Oberfläche zu verbessern.
The catalytic mechanism, electron transfer coupled to proton pumping, of heme-copper oxidases is not yet fully understood. Microsecond freeze-hyperquenching single turnover experiments were carried out with fully reduced cytochrome aa(3) reacting with O(2) between 83 micros and 6 ms. Trapped intermediates were analyzed by low temperature UV-visible, X-band, and Q-band EPR spectroscopy, enabling determination of the oxidation-reduction kinetics of Cu(A), heme a, heme a(3), and of a recently detected tryptophan radical (Wiertz, F. G. M., Richter, O. M. H., Cherepanov, A. V., MacMillan, F., Ludwig, B., and de Vries, S. (2004) FEBS Lett. 575, 127-130). Cu(B) and heme a(3) were EPR silent during all stages of the reaction. Cu(A) and heme a are in electronic equilibrium acting as a redox pair. The reduction potential of Cu(A) is 4.5 mV lower than that of heme a. Both redox groups are oxidized in two phases with apparent half-lives of 57 micros and 1.2 ms together donating a single electron to the binuclear center in each phase. The formation of the heme a(3) oxoferryl species P(R) (maxima at 430 nm and 606 nm) was completed in approximately 130 micros, similar to the first oxidation phase of Cu(A) and heme a. The intermediate F (absorbance maximum at 571 nm) is formed from P(R) and decays to a hitherto undetected intermediate named F(W)(*). F(W)(*) harbors a tryptophan radical, identified by Q-band EPR spectroscopy as the tryptophan neutral radical of the strictly conserved Trp-272 (Trp-272(*)). The Trp-272(*) populates to 4-5% due to its relatively low rate of formation (t((1/2)) = 1.2 ms) and rapid rate of breakdown (t((1/2)) = 60 micros), which represents electron transfer from Cu(A)/heme a to Trp-272(*). The formation of the Trp-272(*) constitutes the major rate-determining step of the catalytic cycle. Our findings show that Trp-272 is a redox-active residue and is in this respect on an equal par to the metallocenters of the cytochrome c oxidase. Trp-272 is the direct reductant either to the heme a(3) oxoferryl species or to Cu (2+)(B). The potential role of Trp-272 in proton pumping is discussed.
Understanding the physics of strongly correlated electronic systems has been a central issue in condensed matter physics for decades. In transition metal oxides, strong correlations characteristic of narrow d bands are at the origin of remarkable properties such as the opening of Mott gap, enhanced effective mass, and anomalous vibronic coupling, to mention a few. SrVO3 with V4+ in a 3d1 electronic configuration is the simplest example of a 3D correlated metallic electronic system. Here, the authors' focus on the observation of a (roughly) quadratic temperature dependence of the inverse electron mobility of this seemingly simple system, which is an intriguing property shared by other metallic oxides. The systematic analysis of electronic transport in SrVO3 thin films discloses the limitations of the simplest picture of e–e correlations in a Fermi liquid (FL); instead, it is shown show that the quasi-2D topology of the Fermi surface (FS) and a strong electron–phonon coupling, contributing to dress carriers with a phonon cloud, play a pivotal role on the reported electron spectroscopic, optical, thermodynamic, and transport data. The picture that emerges is not restricted to SrVO3 but can be shared with other 3d and 4d metallic oxides.
In the search for novel organic charge transfer salts with variable degrees of charge transfer we have studied the effects of two modifications of the recently synthesized donor–acceptor system [tetramethoxypyrene (TMP)]–[tetracyanoquinodimethane (TCNQ)]. One is of chemical nature by substituting the acceptor TCNQ molecules by F4TCNQ molecules. The second consists in simulating the application of uniaxial pressure along the stacking axis of the system. In order to test the chemical substitution, we have grown single crystals of the TMP–F4TCNQ complex and analyzed its electronic structure via electronic transport measurements, ab initio density functional theory (DFT) calculations and UV/VIS/IR absorption spectroscopy. This system shows an almost ideal geometrical overlap of nearly planar molecules stacked alternately (mixed stack) and this arrangement is echoed by a semiconductor-like transport behavior with an increased conductivity along the stacking direction. This is in contrast to TMP–TCNQ which shows a less pronounced anisotropy and a smaller conductivity response. Our band structure calculations confirm the one-dimensional behavior of TMP–F4TCNQ with pronounced dispersion only along the stacking axis. Infrared measurements illustrating the C[triple bond, length as m-dash]N vibration frequency shift in F4TCNQ suggest however no improvement in the degree of charge transfer in TMP–F4TCNQ with respect to TMP–TCNQ. In both complexes about 0.1e is transferred from TMP to the acceptor. Concerning the pressure effect, our DFT calculations on the designed TMP–TCNQ and TMP–F4TCNQ structures under different pressure conditions show that application of uniaxial pressure along the stacking axis of TMP–TCNQ may be the route to follow in order to obtain a much more pronounced charge transfer.
Although iron-based catalysts are regarded as a promising alternative to precious metal catalysts, their precise electronic structures during catalysis still pose challenges for computational descriptions. A particularly urgent question is the influence of the environment on the electronic structure, and how to describe this properly with computational methods. Here, we study an iron porphyrin chloride complex adsorbed on a graphene sheet using density functional theory calculations to detail how much the electronic structure is influenced by the presence of a graphene layer. Our results indicate that weak interactions due to van der Waals forces dominate between the porphyrin complex and graphene, and only a small amount of charge is transferred between the two entities. Furthermore, the interplay of the ligand field environment, strong p − d hybridization, and correlation effects within the complex are strongly involved in determining the spin state of the iron ion. By bridging molecular chemistry and solid state physics, this study provides first steps towards a joint analysis of the properties of iron-based catalysts from first principles.
Stratospheric inorganic chlorine (Cly) is predominantly released from long-lived chlorinated source gases and, to a small extent, very short-lived chlorinated substances. Cly includes the reservoir species (HCl and ClONO2) and active chlorine species (i.e., ClOx). The active chlorine species drive catalytic cycles that deplete ozone in the polar winter stratosphere. This work presents calculations of inorganic chlorine (Cly) derived from chlorinated source gas measurements on board the High Altitude and Long Range Research Aircraft (HALO) during the Southern Hemisphere Transport, Dynamic and Chemistry (SouthTRAC) campaign in austral late winter and early spring 2019. Results are compared to Cly in the Northern Hemisphere derived from measurements of the POLSTRACC-GW-LCYCLE-SALSA (PGS) campaign in the Arctic winter of 2015/2016. A scaled correlation was used for PGS data, since not all source gases were measured. Using the SouthTRAC data, Cly from a scaled correlation was compared to directly determined Cly and agreed well. An air mass classification based on in situ N2O measurements allocates the measurements to the vortex, the vortex boundary region, and midlatitudes. Although the Antarctic vortex was weakened in 2019 compared to previous years, Cly reached 1687±19 ppt at 385 K; therefore, up to around 50 % of total chlorine was found in inorganic form inside the Antarctic vortex, whereas only 15 % of total chlorine was found in inorganic form in the southern midlatitudes. In contrast, only 40 % of total chlorine was found in inorganic form in the Arctic vortex during PGS, and roughly 20 % was found in inorganic form in the northern midlatitudes. Differences inside the two vortices reach as much as 540 ppt, with more Cly in the Antarctic vortex in 2019 than in the Arctic vortex in 2016 (at comparable distance to the local tropopause). To our knowledge, this is the first comparison of inorganic chlorine within the Antarctic and Arctic polar vortices. Based on the results of these two campaigns, the differences in Cly inside the two vortices are substantial and larger than the inter-annual variations previously reported for the Antarctic.
Biogenic organic precursors play an important role in atmospheric new particle formation (NPF). One of the major precursor species is α-pinene, which upon oxidation can form a suite of products covering a wide range of volatilities. Highly oxygenated organic molecules (HOMs) comprise a fraction of the oxidation products formed. While it is known that HOMs contribute to secondary organic aerosol (SOA) formation, including NPF, they have not been well studied in newly formed particles due to their very low mass concentrations. Here we present gas- and particle-phase chemical composition data from experimental studies of α-pinene oxidation, including in the presence of isoprene, at temperatures (−50 and −30 ∘C) and relative humidities (20 % and 60 %) relevant in the upper free troposphere. The measurements took place at the CERN Cosmics Leaving Outdoor Droplets (CLOUD) chamber. The particle chemical composition was analyzed by a thermal desorption differential mobility analyzer (TD-DMA) coupled to a nitrate chemical ionization–atmospheric pressure interface–time-of-flight (CI-APi-TOF) mass spectrometer. CI-APi-TOF was used for particle- and gas-phase measurements, applying the same ionization and detection scheme. Our measurements revealed the presence of C8−10 monomers and C18−20 dimers as the major compounds in the particles (diameter up to ∼ 100 nm). Particularly, for the system with isoprene added, C5 (C5H10O5−7) and C15 compounds (C15H24O5−10) were detected. This observation is consistent with the previously observed formation of such compounds in the gas phase. However, although the C5 and C15 compounds do not easily nucleate, our measurements indicate that they can still contribute to the particle growth at free tropospheric conditions. For the experiments reported here, most likely isoprene oxidation products enhance the growth of particles larger than 15 nm. Additionally, we report on the nucleation rates measured at 1.7 nm (J1.7 nm) and compared with previous studies, we found lower J1.7 nm values, very likely due to the higher α-pinene and ozone mixing ratios used in the present study.
Critical spin liquid versus valence-bond glass in a triangular-lattice organic antiferromagnet
(2019)
In the quest for materials with unconventional quantum phases, the organic triangular-lattice antiferromagnet κ-(ET)2Cu2(CN)3 has been extensively discussed as a quantum spin liquid (QSL) candidate. The description of its low temperature properties has become, however, a particularly challenging task. Recently, an intriguing quantum critical behaviour was suggested from low-temperature magnetic torque experiments. Here we highlight significant deviations of the experimental observations from a quantum critical scenario by performing a microscopic analysis of all anisotropic contributions, including Dzyaloshinskii–Moriya and multi-spin scalar chiral interactions. Instead, we show that disorder-induced spin defects provide a comprehensive explanation of the low-temperature properties. These spins are attributed to valence bond defects that emerge spontaneously as the QSL enters a valence-bond glass phase at low temperature. This theoretical treatment is applicable to a general class of frustrated magnetic systems and has important implications for the interpretation of magnetic torque, nuclear magnetic resonance, thermal transport and thermodynamic experiments.
The interaction of trimethyl(methylcyclopentadienyl)platinum(IV) ((C5H4CH3)Pt(CH3)3) molecules on fully and partially hydroxylated SiO2 surfaces, as well as the dynamics of this interaction were investigated using density functional theory (DFT) and finite temperature DFT-based molecular dynamics simulations. Fully and partially hydroxylated surfaces represent substrates before and after electron beam treatment and this study examines the role of electron beam pretreatment on the substrates in the initial stages of precursor dissociation and formation of Pt deposits. Our simulations show that on fully hydroxylated surfaces or untreated surfaces, the precursor molecules remain inactivated while we observe fragmentation of (C5H4CH3)Pt(CH3)3 on partially hydroxylated surfaces. The behavior of precursor molecules on the partially hydroxylated surfaces has been found to depend on the initial orientation of the molecule and the distribution of surface active sites. Based on the observations from the simulations and available experiments, we discuss possible dissociation channels of the precursor.
Stratospheric inorganic chlorine (Cly) is predominantly released from long-lived chlorinated source gases and, to a small extent, very short-lived chlorinated substances. Cly includes the reservoir species (HCl and ClONO2) and active chlorine species (i.e., ClOx). The active chlorine species drive catalytic cycles that deplete ozone in the polar winter stratosphere. This work presents calculations of inorganic chlorine (Cly) derived from chlorinated source gas measurements on board the High Altitude and Long Range Research Aircraft (HALO) during the Southern Hemisphere Transport, Dynamic and Chemistry (SouthTRAC) campaign in austral late winter and early spring 2019. Results are compared to Cly in the Northern Hemisphere derived from measurements of the POLSTRACC-GW-LCYCLE-SALSA (PGS) campaign in the Arctic winter of 2015/2016. A scaled correlation was used for PGS data, since not all source gases were measured. Using the SouthTRAC data, Cly from a scaled correlation was compared to directly determined Cly and agreed well. An air mass classification based on in situ N2O measurements allocates the measurements to the vortex, the vortex boundary region, and midlatitudes. Although the Antarctic vortex was weakened in 2019 compared to previous years, Cly reached 1687±19 ppt at 385 K; therefore, up to around 50 % of total chlorine was found in inorganic form inside the Antarctic vortex, whereas only 15 % of total chlorine was found in inorganic form in the southern midlatitudes. In contrast, only 40 % of total chlorine was found in inorganic form in the Arctic vortex during PGS, and roughly 20 % was found in inorganic form in the northern midlatitudes. Differences inside the two vortices reach as much as 540 ppt, with more Cly in the Antarctic vortex in 2019 than in the Arctic vortex in 2016 (at comparable distance to the local tropopause). To our knowledge, this is the first comparison of inorganic chlorine within the Antarctic and Arctic polar vortices. Based on the results of these two campaigns, the differences in Cly inside the two vortices are substantial and larger than the inter-annual variations previously reported for the Antarctic.