Search results for "AE"

showing 10 items of 28636 documents

CCDC 981913: Experimental Crystal Structure Determination

2014

Related Article: Abdou K. D. Dimé, Charles H. Devillers, Hélène Cattey, Dominique Lucas|2014|Dalton Trans.|43|14554|doi:10.1039/C4DT00221K

(mu-7172737-tetrakis(4-methylphenyl)-1232-diphenyl-525414243454647-octaazaundecacyclo[36.2.1.136.1811.11316.11821.12326.12831.13336.0224.0422]octatetraconta-136(48)7911(47)12141618(45)19212326(44)272931(43)32343638(41)39-docosaenato(4-)-1kappa4N25N41N42N43:2kappa4N5N45N46N47)-di-nickel(ii) chloroform solvateSpace GroupCrystallographyCrystal SystemCrystal StructureCell ParametersExperimental 3D Coordinates
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CCDC 855779: Experimental Crystal Structure Determination

2012

Related Article: K.Salorinne, E.Nauha, M.Nissinen|2012|Chem.Asian J.|7|809|doi:10.1002/asia.201100969

(mu2-281420-Tetraethyl-6121824-tetramethoxy-410:1622-bis(39-dithia-6-oxaundecane-111-dioxy)calix(4)arene)-di-silver(i) bis(hexafluorophosphate) dichloromethane solvateSpace GroupCrystallographyCrystal SystemCrystal StructureCell ParametersExperimental 3D Coordinates
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CCDC 764821: Experimental Crystal Structure Determination

2013

Related Article: Susanta Hazra, Sagarika Bhattacharya, Mukesh Kumar Singh, Luca Carrella, Eva Rentschler, Thomas Weyhermueller, Gopalan Rajaraman, and Sasankasekhar Mohanta|2013|Inorg.Chem.|52|12881|doi:10.1021/ic400345w

(mu2-5511171723-Hexamethyl-371519-tetraazatricyclo[19.3.1.1913]hexacosa-1(25)279(26)101214192123-decaene-2526-diolato)-acetonitrile-aqua-bis(azido)-iron(iii)-nickel(ii) perchlorateSpace GroupCrystallographyCrystal SystemCrystal StructureCell ParametersExperimental 3D Coordinates
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CCDC 1919442: Experimental Crystal Structure Determination

2019

Related Article: Jana Anhäuser, Rakesh Puttreddy, Lukas Glanz, Andreas Schneider, Marianne Engeser, Kari Rissanen, Arne Lützen|2019|Chem.-Eur.J.|25|12294|doi:10.1002/chem.201903164

(rac)-hexakis(mu-NN'-[tricyclo[8.2.2.247]hexadeca-1(12)46101315-hexaene-512-diylbis(41-phenylene)]bis[1-(pyridin-2-yl)methanimine])-tetra-iron(ii) octakis(trifluoromethanesulfonate) unknown solvateSpace GroupCrystallographyCrystal SystemCrystal StructureCell ParametersExperimental 3D Coordinates
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CCDC 998787: Experimental Crystal Structure Determination

2014

Related Article: Roman I. Zubatyuk, Anna A. Sinelshchikova, Yulia Y. Enakieva, Yulia G. Gorbunova, Aslan Y. Tsivadze, Sergey E. Nefedov, Alla Bessmertnykh-Lemeune, Roger Guilard, Oleg V. Shishkin|2014|CrystEngComm|16|10428|doi:10.1039/C4CE01623H

(tetraethyl (1020-diphenylporphyrin-515-diyl)bis(phosphonatato))-platinum(ii)Space GroupCrystallographyCrystal SystemCrystal StructureCell ParametersExperimental 3D Coordinates
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CCDC 1919440: Experimental Crystal Structure Determination

2019

Related Article: Jana Anhäuser, Rakesh Puttreddy, Lukas Glanz, Andreas Schneider, Marianne Engeser, Kari Rissanen, Arne Lützen|2019|Chem.-Eur.J.|25|12294|doi:10.1002/chem.201903164

ΔΔΔ)-hexakis(mu-(RP)-NN'-[tricyclo[8.2.2.247]hexadeca-1(12)46101315-hexaene-512-diylbis(41-phenylene)]bis[1-(pyridin-2-yl)methanimine])-tetra-iron(ii) octakis(trifluoromethanesulfonate) acetonitrile unknown solvateSpace GroupCrystallographyCrystal SystemCrystal StructureCell ParametersExperimental 3D Coordinates
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The influence of decision-making in tree ring-based climate reconstructions.

2021

Tree-ring chronologies underpin the majority of annually-resolved reconstructions of Common Era climate. However, they are derived using different datasets and techniques, the ramifications of which have hitherto been little explored. Here, we report the results of a double-blind experiment that yielded 15 Northern Hemisphere summer temperature reconstructions from a common network of regional tree-ring width datasets. Taken together as an ensemble, the Common Era reconstruction mean correlates with instrumental temperatures from 1794–2016 CE at 0.79 (p < 0.001), reveals summer cooling in the years following large volcanic eruptions, and exhibits strong warming since the 1980s. Differing in…

/141/704/106/694010506 paleontology010504 meteorology & atmospheric sciencesScienceGeneral Physics and AstronomyClimate changePalaeoclimate01 natural sciencesArticleGeneral Biochemistry Genetics and Molecular BiologyPaleoclimatologySDG 13 - Climate ActionDendrochronologyddc:550Climate change[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment0105 earth and related environmental sciencesResearch dataddc:333.7-333.913 Climate ActionClimate change; Palaeoclimate; Research dataGEMultidisciplinaryQNorthern HemisphereDASGeneral ChemistryResearch data/706/648/697Geography13. Climate actionClimatology/704/106/413GE Environmental Sciences
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Cave bear occupation in Schwabenreith Cave, Austria, during the early last glacial: constraints from 230 Th/U‐dated speleothems

2019

The cave bear was a prominent member of the Upper Pleistocene fauna in Eurasia. While breakthroughs were recently achieved with respect to its phylogeny using ancient DNA techniques, it is still challenging to date cave bear fossils beyond the radiocarbon age range. Without an accurate and precise chronological framework, however, key questions regarding the palaeoecology cannot be addressed, such as the extent to which large climate swings during the last glacial affected the habitat and possibly even conditioned the final extinction of this mammal. Key to constraining the age of cave bear fossils older than the lower limit of radiocarbon dating is to date interlayered speleothems using 23…

/dk/atira/pure/subjectarea/asjc/1200/1201geographygeography.geographical_feature_categoryEastern AlpsbiologyPalaeontologyPaleontologySpeleothemTh/U datingbiology.organism_classificationArchaeologyArts and Humanities (miscellaneous)Cave/dk/atira/pure/sustainabledevelopmentgoals/climate_actionSDG 13 - Climate ActionEarth and Planetary Sciences (miscellaneous)Cave bearcave bear/dk/atira/pure/subjectarea/asjc/1900/1901/dk/atira/pure/subjectarea/asjc/1900/1911Glacial periodearly last glacialspeleothemGeologyJournal of Quaternary Science
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Energy transfer in LH2 of Rhodospirillum Molischianum, studied by subpicosecond spectroscopy and configuration interaction exciton calculations.

2001

Two color transient absorption measurements were performed on a LH2 complex from Rhodospirillum molischianum by using several excitation wavelengths (790, 800, 810, and 830 nm) and probing in the spectral region from 790 to 870 nm at room temperature. The observed energy transfer time of ∼1.0 ps from B800 to B850 at room temperature is longer than the corresponding rates in Rhodopseudomonas acidophila and Rhodobacter sphaeroides. We observed variations (0.9-1.2 ps) of B800-850 energy transfer times at different B800 excitation wavelengths, the fastest time (0.9 ps) was obtained with 800 nm excitation. At 830 nm excitation the energy transfer to the B850 ring takes place within 0.5 ps. The m…

/dk/atira/pure/sustainabledevelopmentgoals/affordable_and_clean_energybiologyChemistryExcitonConfiguration interactionbiology.organism_classificationSpectral lineSurfaces Coatings and FilmsRhodobacter sphaeroidesUltrafast laser spectroscopyMaterials ChemistrySDG 7 - Affordable and Clean EnergyPhysical and Theoretical ChemistryAtomic physicsAbsorption (electromagnetic radiation)SpectroscopyExcitation
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Asymptotic behavior of global solutions of aerotaxis equations

2019

Abstract We study asymptotic behavior of global solutions of one-dimensional aerotaxis model proposed in Knosalla and Nadzieja (2015) [9] .

010101 applied mathematicsAsymptotic behavior of solutionsApplied Mathematics010102 general mathematicsAerotaxis equationsApplied mathematics0101 mathematics01 natural sciencesAnalysisMathematicsJournal of Mathematical Analysis and Applications
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