Thomas Loerting

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Thomas Loerting

Thomas Loerting (born October 29, 1973) is an Austrian chemist and associate professor at the University of Innsbruck. His research focuses on amorphous systems, the physics and chemistry of ice and chemistry at low temperatures. [1]

Contents

Biography

Thomas Loerting was born in Innsbruck where he also graduated from high-school ("Reithmanngymnasium") in 1992. He studied chemistry at the University of Innsbruck and received his Master's degree in 1997. In 1998, over the course of his Ph.D. in Innsbruck, Loerting was a guest lecturer at the Gadjah Mada University in Yogyakarta and the Chulalongkorn University in Bangkok, Thailand. He successfully defended his Ph.D. thesis titled "Kinetics of water mediated proton transfer in the atmosphere" in 2000. In 2001, he joined the team of Nobel laureate Mario Molina at the Massachusetts Institute of Technology. Loerting returned to Innsbruck in 2004 as assistant professor working together with Erwin Mayer. His habilitation "Disordered water at low temperatures" was submitted 2007. In 2008, he was elected as member of the Austrian Academy of Sciences ("Junge Kurie"). Since 2010, he is associate professor at the Institute of Physical Chemistry. [2] As of 2012, he is also speaker of the research platform "Advanced Materials", which counts over 10 research groups. [3] In addition to his academic work, he serves as advisor to the Austrian Luge Federation.

Research

Thomas Loerting research includes more than 180 peer-reviewed international publications with more than 8000 citations, resulting in a h-index of 48 (as of October 2022). His first contributions were in the field of Theoretical and Computational chemistry, contributing to the understanding of hydration of sulfur dioxide and sulfur trioxide as well as the decomposition of chlorine nitrate, relevant to the chemistry of the atmosphere. He soon moved on to experiments where he advanced the field of amorphous ices, ice polymorphs and carbonic acid over the course of his career.

Amorphous ices

Thomas Loerting provided significant contributions for the understanding of polyamorphism in water. This includes the recognition of VHDA as third distinct amorphous state of water [4] as well as extensive studies on structure and dynamics of low- and high-density amorphous ice (LDA and HDA) using dilatometry, spectroscopy, calorimetry and diffraction. One particularly notable finding was that LDA and HDA both exhibit glass-to-liquid transitions at ambient pressure, [5] which provides support for the LLCP scenario in water. [6]

Ice polymorphs

In addition to his achievements in the field of amorphous ices, Thomas Loerting is recognized for his works on crystalline ices, including the recent discovery of ice XIX. Together with his team he provided the first experimental proof that for each hydrogen-disordered ice phase (in this case: ice VI) several hydrogen-ordered counterparts (ices XV and XIX) may exist. [7] [8] [9] [10]

Cryochemistry

Another focus in the body of work of Thomas Loerting is acid-base chemistry under cryo-conditions. By employing the cryo-preparation and rapid quenching technique developed by Hage, Hallbrucker and Mayer, [11] coupled with FTIR-spectroscopy of the solid and the matrix isolated species, Loerting and his co-workers have pioneered formation and isomerisation of carbonic acid and its derivatives. [12] [13] [14] [15] [16] [17] [18] [19]

Awards and fellowships

Thomas Loerting has received numerous awards for his scientific input. Among the most notable are:

Related Research Articles

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Carbon is a chemical element; it has symbol C and atomic number 6. It is nonmetallic and tetravalent—meaning that its atoms are able to form up to four covalent bonds due to its valence shell exhibiting 4 electrons. It belongs to group 14 of the periodic table. Carbon makes up about 0.025 percent of Earth's crust. Three isotopes occur naturally, 12C and 13C being stable, while 14C is a radionuclide, decaying with a half-life of 5,700 years. Carbon is one of the few elements known since antiquity.

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Carbon monoxide is a poisonous, flammable gas that is colorless, odorless, tasteless, and slightly less dense than air. Carbon monoxide consists of one carbon atom and one oxygen atom connected by a triple bond. It is the simplest carbon oxide. In coordination complexes, the carbon monoxide ligand is called carbonyl. It is a key ingredient in many processes in industrial chemistry.

<span class="mw-page-title-main">Hydrogen bond</span> Intermolecular attraction between a hydrogen-donor pair and an acceptor

In chemistry, a hydrogen bond is primarily an electrostatic force of attraction between a hydrogen (H) atom which is covalently bonded to a more electronegative "donor" atom or group (Dn), and another electronegative atom bearing a lone pair of electrons—the hydrogen bond acceptor (Ac). Such an interacting system is generally denoted Dn−H···Ac, where the solid line denotes a polar covalent bond, and the dotted or dashed line indicates the hydrogen bond. The most frequent donor and acceptor atoms are the period 2 elements nitrogen (N), oxygen (O), and fluorine (F).

<span class="mw-page-title-main">Carbonic acid</span> Chemical compound

Carbonic acid is a chemical compound with the chemical formula H2CO3. The molecule rapidly converts to water and carbon dioxide in the presence of water. However, in the absence of water, it is quite stable at room temperature. The interconversion of carbon dioxide and carbonic acid is related to the breathing cycle of animals and the acidification of natural waters.

<span class="mw-page-title-main">Clathrate hydrate</span> Crystalline solid containing molecules caged in a lattice of frozen water

Clathrate hydrates, or gas hydrates, clathrates, or hydrates, are crystalline water-based solids physically resembling ice, in which small non-polar molecules or polar molecules with large hydrophobic moieties are trapped inside "cages" of hydrogen bonded, frozen water molecules. In other words, clathrate hydrates are clathrate compounds in which the host molecule is water and the guest molecule is typically a gas or liquid. Without the support of the trapped molecules, the lattice structure of hydrate clathrates would collapse into conventional ice crystal structure or liquid water. Most low molecular weight gases, including O2, H2, N2, CO2, CH4, H2S, Ar, Kr, Xe, and Cl2 as well as some higher hydrocarbons and freons, will form hydrates at suitable temperatures and pressures. Clathrate hydrates are not officially chemical compounds, as the enclathrated guest molecules are never bonded to the lattice. The formation and decomposition of clathrate hydrates are first order phase transitions, not chemical reactions. Their detailed formation and decomposition mechanisms on a molecular level are still not well understood. Clathrate hydrates were first documented in 1810 by Sir Humphry Davy who found that water was a primary component of what was earlier thought to be solidified chlorine.

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<span class="mw-page-title-main">Polyamorphism</span> Ability of a substance to exist in more than one distinct amorphous state

Polyamorphism is the ability of a substance to exist in several different amorphous modifications. It is analogous to the polymorphism of crystalline materials. Many amorphous substances can exist with different amorphous characteristics. However, polyamorphism requires two distinct amorphous states with a clear, discontinuous (first-order) phase transition between them. When such a transition occurs between two stable liquid states, a polyamorphic transition may also be referred to as a liquid–liquid phase transition.

<span class="mw-page-title-main">Grotthuss mechanism</span> Protons hopping across hydrogen bonds between hydronium ions and water molecules

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<span class="mw-page-title-main">Carbon trioxide</span> Chemical compound

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3
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<span class="mw-page-title-main">Ascalaph Designer</span>

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References

  1. Thomas Loerting Personal Homepage: Research Overview , retrieved on October 24, 2022
  2. Thomas Loerting Personal Homepage: Biography , retrieved on October 24, 2022
  3. University of Innsbruck: Advanced Materials , retrieved on October 24, 2022
  4. Loerting, T.; Salzmann, C.; Kohl, I.; Mayer, E.; Hallbrucker, A. (2001). "A second distinct structural "state" of high-density amorphous ice at 77 K and 1 bar". Phys. Chem. Chem. Phys. 3 (24): 5355–5357. Bibcode:2001PCCP....3.5355L. doi:10.1039/B108676F.
  5. Amann-Winkel, K.; Böhmer, R.; Fujara, F.; Gainaru, C.; Geil, B.; Loerting, T. (2016). "Colloquium: Water's controversial glass transitions". Rev. Mod. Phys. 88 (1): 011002. Bibcode:2016RvMP...88a1002A. doi:10.1103/RevModPhys.88.011002.
  6. Giovambattista, N.; Loerting, T.; Lukanov, B. R..; Starr, F. W. (2012). "Interplay of the Glass Transition and the Liquid-Liquid Phase Transition in Water". Sci. Rep. 2: 390. Bibcode:2012NatSR...2E.390G. doi:10.1038/srep00390. PMC   3340608 . PMID   22550566.
  7. Gasser, T. M.; Thoeny, A. V.; Plaga, L. J.; Köster, K. W.; Etter, M.; Böhmer, R.; Loerting, T. (2018). "Experiments indicating a second hydrogen ordered phase of ice VI". Chem. Sci. 9 (18): 4224–4234. doi:10.1039/C8SC00135A. PMC   5942039 . PMID   29780552.
  8. Thoeny, A. V.; Gasser, T. M.; Loerting, T. (2019). "Distinguishing ice β-XV from deep glassy ice VI: Raman spectroscopy". Phys. Chem. Chem. Phys. 21 (28): 15452–15462. Bibcode:2019PCCP...2115452T. doi: 10.1039/C9CP02147G . PMID   31257365. S2CID   195764029.
  9. Gasser, T. M.; Thoeny, A. V.; Greussing, V.; Loerting, T. (2021). "Calorimetric Investigation of Hydrogen-Atom Sublattice Transitions in the Ice VI/XV/XIX Trio". J. Phys. Chem. B. 125 (42): 11777–11783. doi:10.1021/acs.jpcb.1c07508. PMC   8558864 . PMID   34647740.
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  12. Tautermann, C. S.; Voegele, A. F.; Loerting, T.; Kohl, I.; Hallbrucker, A.; Mayer, E.; Liedl, K. R. (2002). "Towards the Experimental Decomposition Rate of Carbonic Acid (H2CO3) in Aqueous Solution". Chem. Eur. J. 8 (1): 66–73. doi:10.1002/1521-3765(20020104)8:1<66::AID-CHEM66>3.0.CO;2-F. PMID   11822465.
  13. Winkel, K; Hage, W; Loerting, T; Price, S. L.; Mayer, E. (2007). "Carbonic Acid: From Polyamorphism to Polymorphism". J. Am. Chem. Soc. 129 (45): 13863–13871. doi:10.1021/ja073594f. PMID   17944463.
  14. Kohl, I.; Winkel, K.; Bauer, M.; Liedl, K. R.; Loerting, T.; Mayer, E. (2009). "Raman Spectroscopic Study of the Phase Transition of Amorphous to Crystalline β-Carbonic Acid". Angew. Chem. Int. Ed. 48 (15): 2690–2694. doi:10.1002/anie.200805300. PMID   19212997.
  15. Bernard, J.; Seidl, M.; Kohl, I.; Liedl, K. R.; Mayer, E.; Gálvez, Ó.; Grothe, H.; Loerting, T. (2011). "Spectroscopic Observation of Matrix-Isolated Carbonic Acid Trapped from the Gas Phase". Angew. Chem. Int. Ed. 50 (8): 1939–1943. doi:10.1002/anie.201004729. PMID   21328675.
  16. Bernard, J.; Seidl, M.; Mayer, E; Loerting, T. (2012). "Formation and Stability of Bulk Carbonic Acid (H2CO3) by Protonation of Tropospheric Calcite". ChemPhysChem. 13 (13): 3087–3091. doi:10.1002/cphc.201200422. PMC   3482932 . PMID   22707186.
  17. Bernard, J.; Huber, R. G.; Liedl, K. R.; Grothe, H.; Loerting, T. (2013). "Matrix Isolation Studies of Carbonic Acid—The Vapor Phase above the β-Polymorph". J. Am. Chem. Soc. 135 (20): 7732–7737. doi:10.1021/ja4020925. PMC   3663070 . PMID   23631554.
  18. Bernard, J.; Köck, E.-M..; Huber, R. G.; Liedl, K. R.; Call, L.; Schlögl, R.; Grothe, H.; Loerting, T. (2017). "Carbonic acid monoethyl ester as a pure solid and its conformational isomerism in the gas-phase". RSC Adv. 7 (36): 22222–22233. Bibcode:2017RSCAd...722222B. doi:10.1039/C7RA02792C. PMC   5450006 . PMID   28603608.
  19. Köck, E.-M.; Bernard, J.; Podewitz, M.; Dinu, D. F.; Huber, R. G.; Liedl, K. R.; Grothe, H.; Bertel, E.; Schlögl, R.; Loerting, T. (2020). "Alpha‐Carbonic Acid Revisited: Carbonic Acid Monomethyl Ester as a Solid and its Conformational Isomerism in the Gas Phase". Chem. Eur. J. 26 (1): 285–305. doi:10.1002/chem.201904142. PMC   6972543 . PMID   31593601.
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