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  • 550 - Earth sciences  (6)
  • Lunar and Planetary Science and Exploration  (4)
  • Inorganic Chemistry  (3)
  • 2005-2009  (10)
  • 1990-1994  (3)
  • 1
    Electronic Resource
    Electronic Resource
    Weinheim : Wiley-Blackwell
    Zeitschrift für anorganische Chemie 608 (1992), S. 33-42 
    ISSN: 0044-2313
    Keywords: Diacylphosphines ; Di-cyclohexoylposphine ; Diadamant-1-oylphosphine ; keto-enol tautomerism ; NMR-parameters, thermodynamic data ; X-ray structure determination ; very short O‥H‥O bridge ; Chemistry ; Inorganic Chemistry
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology
    Description / Table of Contents: Acyl- and Alkylidenephosphines. XXXII. Di-cyclohexoyl- and Diadamant-1-oylphosphine - Keto-Enol Tautomerism and StructureLithium dihydrogenphosphide · DME (1) [12] and cyclo-hexoyl or adamant-1-oyl chloride react in a molar ratio of 3:2 to give lithium di-cyclo-hexoylphosphide · DME and the corresponding diadamant-1-oylphosphide.2THF (1) resp. Treatment of these two compounds with 85% tetrafluoroboric acid. diethylether adduct yields di-cyclo-hexoyl- (1b) and diadamant-1-oylphosphine (1c). In nmr spectroscopic studies 1b over a range of 203 to 343 K, a strong temperature dependence of the keto-enol equilibrium is found; thermodynamic data characteristic for the formation of the enol tautomer (ΔH0 = -4.3 kJ. mol-1; ΔS0 = -9.2 J. mol-1. K (-1) are compared of 1,3-diketones.The enol tautomer of diadamant-1-oylphosphine (E-1c) as obtained from a benzene solution in thin colourless plates, crystallizes in the monoclinic space group P21/c {a = 722.2(2); b = 1085.5(4); c = 2434.8(5) pm; ß = 96.43(2)° at -100 ± 3°C; Z = 4}. An X- ray structure analysis (Rw = 0.033) shows bond lengths and angles to be almost identical within the enolic system (P—C 179/180; C—O 130/129; C—C(adamant-1-yl) 152/153 pm; C—P—C 99°; P—C—O 124°/124°; P—C—C 120°/120°; C—C—O 116°/116°. The geometry of the very strong, but probably asymmetric O‥H‥O bridge is discussed (O—H 120/130, O‥O 245 pm).
    Notes: Aus Lithium-dihydrogenphosphid · DME (1) [12] und cyclo-Hexoyl- bzw. Adamant-1-oyl-chlorid im Molverhältnis 3:2 zugängliches Lithium-di-cyclo-hexoylphosphid · DME und -diadamant-1-oylphosphid · 2THF 1) reagieren mit 85proz. Tetrafluoroborsäure · Diethylether-Addukt zu Di-cyclo-hexoyl- 1b) und Diadamant-1-oylphosphan (1 c). Die Lage des Keto-Enol-Gleichgewichts zwischen 203 und 343 K sowie thermodynamische Daten zur Bildung des Enol-Isomers ΔH0= -4,3kJ.Mol-1; ΔS0;=-9,2 J · mol-1 · K-1 () wurden NMR-spektroskopisch an einer 2 M Lösung des bei +20°C flüssigen Di-cyclo-Hexoyl-Derivates 1b in d8-Toluol ermittelt und mit Werten von 1,3-Diketonen verglichen.Das farblose, sich aus Benzol in dünnen Plättchen abscheidende Enol-Tautomer des Diadamant-1-oylphosphans (E-1 c) kristallisiert monoklin in der Raumgruppe P21/c {a = 722,2(2) b = 1085,5(4); c = 2434,8(5) pm; ß = 96,43(2)° bei - 100 ± 3°C; Z = 4}. Nach den Ergebnissen der Röntgenstrukturanalyse (Rw=0,033) weist das Molekül in beiden des Hälften des Enolrings nahezu identische Bindungslängen und -winkel auf P—C 179/180; C—O 130/129; C—C(Adamant-1-yl) 152/153 pm; C—P—C 99°; P—C—O 124°/124°; P—C—C 120°/120°; C—C—O 116°/116°. Die Geometrie der sehr starken, aber vermutlich asymmetrischen O‥H‥O-Brücke wird diskutiert (O—H 120/130; O‥O 245 pm).
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  • 2
    ISSN: 0044-2313
    Keywords: Lithium bis(2,2-dimethylpropionl)arsenide · DME ; tetrakis(2,2-dimethylpropionyl)diarsine ; X-ray structure determination ; Chemistry ; Inorganic Chemistry
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology
    Description / Table of Contents: Acyl- and Alkylidenearsines VII Synthesis and Structure of Tetrakis(2,2-dimethylpropionyl)diarsineLithium dihydrogenarsenide and 2,2-dimethylpropionyl chloride in a molar ratio of 3:2 react at -40 to -50°C in tetrahydrofuran or 1,2-dimethoxyethane to give the corresponding etherate of lithium bis(2,2-dimethylpropionyl)arsenide (2a). Treatment of these solutions with stoichiometric amounts of 85% tetrafluoroboric acid · diethylether adduct yields yelloworange tetrakis(2,2-dimethylpropionyl)diarsine (5) in 64 or 62% yield resp., but not the expected bis (2,2-dimethylpropionyl)arsine (4a). The very air-sensitive compound crystallizes in the monoclinic space group P21/n {-100 ± 3° C; a = 1224.6(3); b = 1419.7(3); c = 1333.1(3) pm; β = 96.22(2)°; Z = 4}. According to the X-ray structure analysis (Rw = 0.036) the molecule shows synclinal conformation; the two diacylarsyl-subunits are twisted against one another by an angle of 86°. As in another acylarsine [1] the As—C distances (203 to 205 pm) were found to be significantly longer then the standard value of 196 pm. Further characteristic bond lengths and angles are: As- 242; C—O 120 to 121 pm; As—As—C 88 to 107°; As—C—O 118 to 122°
    Notes: Wird das jeweilige, aus Lithiumdihydrogenarsenid und 2,2-Dimethylpropionylchlorid im Molverhältnis 3:2 bei -40 bis -50°C in TetrahydrofuranTetrahydrofuran (THF); 1,2-Dimethoxyethan (DME); Bis( 1,2-dimethylamino)ethan (TMEDA); Tetramethylsilan (TMS). oder 1,2-Dimethoxyethan gebildete, aber nicht isolierte Etherat des Lithium-bis(2,2-dimethypropionyl)arsenids (2a) mit 85proz. Tetrafluorborsäure · Diethylether-Addukt weiter umgesetzt, so erhält man nach der üblichen Aufarbeitung des Ansatzes nicht Bis(2,2-dimethylpropionyl)arsan (4a), sondern mit 64- bzw. 62proz.Ausbeute Tetrakis(2,2-dimethylpropionyl)diarsan (5). Die äußerst oxydationsempfindliche gelborange Verbindung kristallisiert monoklin in der Raumgruppe P21/n {-100 ± 3° C; a = 1224,6(3); b = 1419,7(3); c = 1333,1(3)pm; β = 96,22(2)°; Z = 4}. Nach den Ergebnissen der Röntgenstrukturanalyse (Rw = 0,036) weist das Molekül mit zwei um 86° gegeneinander verdrehten Hälften die synclinale Konformation auf; die As—C-Abstände liegen mit 203 bis 205 pm wie in einem anderen Acylarsan [1] deutlich über dem Standard von 196 pm. Weitere Charakteristische Bindungslängen und -winkel sind: As—As242; C—O 120 bis 121 pm; As—As—C 88 bis 107°; As—C—O 118 bis 122°.
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  • 3
    ISSN: 0044-2313
    Keywords: Dicopper trihydroxide nitrite ; crystal structure ; i.r., Raman spectra ; Chemistry ; Inorganic Chemistry
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology
    Description / Table of Contents: Lattice Vibration Spectra. LXXVI. On Basic Copper Salts  -  Crystal Structure, IR and Raman Spectra of Cu2(OH)3NO2Single-crystal X-ray as well as IR and Raman data of Cu2(OH)3NO2 are presented and discussed with respect to an order-disorder (OD) phase transition and the strength of hydrogen bonds. Cu2(OH)3NO2 crystallizes pseudosymmetrically in the monoclinic space group P21/m (Z = 2, a = 562.22(4), b = 605.94(5), c = 663.55(4) pm and β = 95.415(5)°) forming a layered structure of edge-connected, elongated CuO6 octahedra (final R value 2.5% for 1047 symmetry averaged reflections with I ≥ 2.5 μ1). The NO2- ions are on a split position with dynamic disordering at ambient temperature. On temperature lowering the disorder is frozen out with a symmetry decrease to space group P21. The disorder of the NO2- ions causes four different arrangements of OH(2)- with different strengths of the H…O hydrogen bonds present OD stretching modes in the spectra of isotopically dilute samples 2628, 2535, 2435, and 2343 cm-1 at 90 K. The OH(1)- ions form weak H…N H-bonds to the lone-pair of the nitrogen atoms of the NO2- ions (vOD 2563 cm-1).
    Notes: Die Kristallstruktur sowie die IR- und Raman-Spektren von Cu2(OH)3NO2 werden mitgeteilt und im Hinblick auf eine Ordnungs-Unordnungs(OD)-Phasenumwandlung sowie die Stärke der vorhandenen Wasserstoffbrücken diskutiert. Das basische Nitrit kristallisiert pseudosymmetrisch in der monoklinen Raumgruppe P21/m (Z = 2, R = 2,5%, 1047 symmetriegemittelte Reflexe mit 1 〉 2,5 μ1). Cu2(OH)3NO2 bildet eine Schichtenstruktur kantenverknüpfter, gestreckter CuO6-Oktaeder. Die Nitritionen befinden sich auf einer Splitlage mit dynamischer Fehlordnung bei Raumtemperatur. Bei niedrigeren Temperaturen friert die Fehlordnung unter Bildung von NO2--Zick-Zack-Ketten und Symmetrieerniedrigung zu P21 aus. Aufgrund der Fehlordnung der NO2--Ionen ergeben sich für die OH(2)--Ionen vier verschiedene Anordnungen mit entsprechend unterschiedlich starken H-Brücken (H…O). Die OH(1)--Ionen bilden H…N-Wasserstoffbrücken zum freien Elektronenpaar des N-Atoms der NO2--Ionen.
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  • 4
    Publication Date: 2018-06-11
    Description: Home Plate is a layered plateau in Gusev crater on Mars. It is composed of clastic rocks of moderately altered alkali basalt composition, enriched in some highly volatile elements. A coarse-grained lower unit is overlain by a finer-grained upper unit. Textural observations indicate that the lower strata were emplaced in an explosive event, and geochemical considerations favor an explosive volcanic origin over an impact origin. The lower unit likely represents accumulation of pyroclastic materials, while the upper unit may represent eolian reworking of the same pyroclastic materials.
    Keywords: Lunar and Planetary Science and Exploration
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  • 5
    Publication Date: 2019-07-13
    Description: The primary MER objectives have been successfully completed. The total integration time of all MB measurements exceeds the duration of the primary 90-sols-mission for Spirit's MB spectrometer, and approaches this value for Opportunity's MB spectrometer. Both MB spectrometers continue to accumulate valuable scientific data after three years of operation (data is available for download [13]) The identification of aqueous minerals such as goethite in Gusev crater and jarosite at Meridiani Planum by the MER Mossbauer spectrometers is strong evidence for past water activity at the two landing sites.
    Keywords: Lunar and Planetary Science and Exploration
    Type: European Planetary Science Congress 2007; Aug 19, 2007 - Aug 24, 2007; Potsdam; Germany
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  • 6
    Publication Date: 2019-07-13
    Description: The two Miniaturized Moessbauer Spectrometers (MIMOS II) on board the two Mars Exploration Rovers Spirit and Opportunity have now been collecting important scientific data for more than four years. The spectrometers provide information about Fe-bearing mineral phases and determine Fe oxidation states. The total amount of targets analized exceeds 600, the total integration time exceeds 260 days for both rovers. Since landing, more than five half-lives of the Co-57 MB sources have past (intensity at the time of landing approx. 150 mCi). Current integration times are about 50 hours in order to achieve reasonable statistics as opposed to 8 hours at the beginning of the mission. In total, 13 different mineral phases were detected: Olivine, pyroxene, hematite, magnetite and nanophase ferric oxide were detected at both landing sites. At Gusev, ilmenite, goethite, a ferric sulfate phase and a yet unassigned phase (in the rock Fuzzy Smith) were detected. At Meridiani, jarosite, metallic iron in meteoritic samples (kamacite), troilite, and an unassigned ferric phase were detected. Jarosite and goethite are of special interest, as these minerals are indicators for water activity. In this abstract, an overview of Moessbauer results will be given, with a focus on data obtained since the last martian winter. The MER mission has proven that Moessbauer spectroscopy is a valuable tool for the in situ exploration of extraterrestrial bodies and for the study of Febearing samples. The experience gained through the MER mission makes MIMOS II a obvious choice for future missions to Mars and other targets. Currently, MIMOS II is on the scientific payload of two approved future missions: Phobos Grunt (Russian Space Agency; 2009) and ExoMars (European Space Agency; 2013).
    Keywords: Lunar and Planetary Science and Exploration
    Type: 39th Lunar and Planetary Science Conference; Mar 10, 2008 - Mar 14, 2008; League City, TX; United States
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  • 7
    Publication Date: 2019-07-13
    Description: Light-toned, subsurface soil deposits have been excavated by the Mars Exploration Rover (MER) Spirit in six distinct locations along its traverse across the Columbia Hills of Gusev Crater. Samples at two of these sites have been analyzed in detail by the M ssbauer (MB) and Alpha Particle X-ray Spectrometers (APXS), providing information on iron mineralogy and elemental chemistry, respectively. These soils are referred to as "Paso Robles" class deposits.
    Keywords: Lunar and Planetary Science and Exploration
    Type: Lunar and Planetary Science Conference; Mar 12, 2007 - Mar 16, 2007; Houston, TX; United States
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  • 8
    Publication Date: 2020-02-12
    Keywords: 550 - Earth sciences
    Type: info:eu-repo/semantics/article
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  • 9
    Publication Date: 2020-02-12
    Description: Abstract Permian carbonate reservoir rocks (Stassfurt-Carbonate) of the CO2-province (Lower Saxony Basin, NW Germany) are locally characterised by high amounts of CO2 leading to serious problems on exploration. In order to receive information on the major CO2 sources and CO2 migration and accumulation processes mineralogical, geochemical and stable isotope analyses (13C, 18O) were carried out on authigenic precipitations within the Stassfurt carbonate rocks (Ca2). These rocks contain early diagenetic (e.g., formed in soft sediment) carbonate minerals (calcite, dolomite) and anhydrite in concretions and small cracks. In addition, large (up to 2 cm wide) carbonate-cemented fractures formed in solid Ca2 rocks. Semi-quantitative estimates of the diagenetic mineral content showed variations between the investigated rock cores. Nine out of 12 Ca2 rock cores are derived from wells situated in the area of modern CH4-rich reservoirs and have distinct fracture systems developed. In contrast, the other three rock cores are from wells characterised by CO2-rich reservoirs and lack fractures of similar thickness. The assumed relationship between tectonically induced fractures and the gas content of the Ca2 reservoir rocks implies CO2 degassing of the Ca2 rocks at approximately 102 °C to 150 °C (assumed δ18Opore water variation from 0‰ to + 4‰ SMOW). REE distribution indicates at least three types of fracture- and crack-filling carbonates. Two carbonate generations formed from evolving diagenetic pore waters whereas one type reflects carbonate formation under hydrothermal influence. The ages of these cementations derived from Rb/Sr and U/Pb isotope analyses indicate their formation during late stage of/or after the inversion of the Lower Saxony Basin in Late Cretaceous times. The stable carbon isotope composition of the authigenic carbonate minerals reflects at least two carbon source endmembers available during diagenesis. Whereas many early-formed carbonates are related to the Permian 13C-rich carbon source, those carbonates which precipitated or recrystallised during early to late stage diagenesis and/or were induced by local tectonic events incorporated 12C-enriched CO2 from organic degradation processes. The stable oxygen isotope values of authigenic carbonates probably still reflect low temperatures of mineral formation from Permian sea water (as it is assumed for “non” recrystallised carbonates) or late-stage high-temperature (up to 150 °C) precipitation from sea water-derived pore waters which may have been locally influenced by 18O-enriched fluids. However, most of the carbonate samples investigated are recrystallised (crystal enlargement of concretionary and fracture carbonate is observed) and hence, these carbonates are at least partly re-equilibrated (original 18O-content reduced) with surrounding pore waters at elevated temperature. Similar to the authigenic carbonate at least two sources may explain the concentration/carbon isotope relationship of modern CO2 present in the Ca2 reservoir rocks. An organic-derived CO2 endmember source (δ13C near − 20‰) is present in relatively low concentrations whereas large CO2 concentrations derived from an endmember source with an isotope value near 0‰. Although the latter source is unknown such “heavy” CO2 sources are most likely attributed to carbonate decomposition processes.
    Keywords: 550 - Earth sciences
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  • 10
    Publication Date: 2020-02-12
    Keywords: 550 - Earth sciences
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