1,834 research outputs found

    Silver-palladium braze alloy recovered from masking materials

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    Method for recovering powdered silver-palladium braze alloy from an acrylic spray binder and rubber masking adhesive used in spray brazing is devised. The process involves agitation and dissolution of masking materials and recovery of suspended precious metal particles on a filter

    Adenosine 5'-(2-bromoethyl)-phosphate. A new affinity label for adenine nucleotide sites in proteins

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    A new adenosine analogue adenosine 5'-(2-bromoethyl)-phosphate has been synthesized. The reactive moiety, a bromoalkyl group, has the ability to react with the nucleophilic side chains of several amino acids. This compound reacts with NAD-dependent isocitrate dehydrogenase from pig heart, causing inactivation. Addition of the allosteric regulator ADP to the reaction mixture protects the enzyme from loss of activity. A second adenosine analogue has been synthesized, adenosine 5'-(n-propyl)-phosphate, which is used to assess any effects that might arise from the noncovalent interaction of adenosine 5'-(2-bromoethyl)-phosphate with the enzyme. It is proposed that adenosine 5'-(2-bromoethyl)-phosphate reacts with an adenine nucleotide site on isocitrate dehydrogenase and that this compound may have general applicability as an affinity label of catalytic and regulatory adenine nucleotide sites in proteins

    Spin dynamics and disorder effects in the S=1/2 kagome Heisenberg spin liquid phase of kapellasite

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    We report 35^{35}Cl NMR, ESR, μ\muSR and specific heat measurements on the S=1/2S=1/2 frustrated kagom\'e magnet kapellasite, α\alpha-Cu3_3Zn(OH)6_6Cl2_2, where a gapless spin liquid phase is stabilized by a set of competing exchange interactions. Our measurements confirm the ferromagnetic character of the nearest-neighbour exchange interaction J1J_1 and give an energy scale for the competing interactions J10|J| \sim 10 K. The study of the temperature-dependent ESR lineshift reveals a moderate symmetric exchange anisotropy term DD, with D/J3|D/J|\sim 3%. These findings validate a posteriori the use of the J1J2JdJ_1 - J_2 - J_d Heisenberg model to describe the magnetic properties of kapellasite [Bernu et al., Phys. Rev. B 87, 155107 (2013)]. We further confirm that the main deviation from this model is the severe random depletion of the magnetic kagom\'e lattice by 27%, due to Cu/Zn site mixing, and specifically address the effect of this disorder by 35^{35}Cl NMR, performed on an oriented polycrystalline sample. Surprisingly, while being very sensitive to local structural deformations, our NMR measurements demonstrate that the system remains homogeneous with a unique spin susceptibility at high temperature, despite a variety of magnetic environments. Unconventional spin dynamics is further revealed by NMR and μ\muSR in the low-TT, correlated, spin liquid regime, where a broad distribution of spin-lattice relaxation times is observed. We ascribe this to the presence of local low-energy modes.Comment: 15 pages, 11 figures. To appear in Phys. Rev.

    Minerals information GIS for regional development and inward investment in Northern Highlands of Scotland

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    The principal aim of this project, funded by the Department of Trade and Industry (DTI), is to stimulate exploration for metalliferous minerals in the Northern Highlands of Scotland, thereby promoting inward investment, job creation and the development of infrastructure in the region. The Northern Highlands study area occupies about 27,000 km2 located to the north and west of the Great Glen, including the Hebrides, Orkney and Shetland. The regional geology is highly varied, comprising mainly Archaean and Proterozoic metamorphic rocks and Palaeozoic sedimentary rocks. Intrusive igneous rocks are also widely developed. This geological diversity enhances the potential of the region for the occurrence of a wide range of mineral deposit types. The Northern Highlands are under-explored, relative to other parts of Scotland; nevertheless, this study has documented more than 350 recorded mineral occurrences

    Ground State and Intrinsic Susceptibility of the Kagome Antiferromagnet Vesignieite as seen by 51V NMR

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    The intrinsic magnetic susceptibility and local magnetization of the near-kagome quantum magnet vesignieite, Cu3BaV2O8(OH)2, are presented as measured using 51V NMR. The NMR line shift gives an accurate measurement of the intrinsic susceptibility of the kagome sites which closely resembles that of the quantum spin liquid herbertsmithite [A. Olariu et al. Phys. Rev. Lett. 100, 087202 (2008)]. It is therefore surprising that, at Tc ~ 9 K, a transition to a heterogeneous ground state is observed. A gradual wipeout of half the NMR intensity indicates a slowly fluctuating spin liquid component and a detailed analysis of the linewidth reveals the onset of static magnetism at the remaining half of the sites. It is proposed that this transition and unusual ground state originate from a nearby quantum critical point induced by the Dzyaloshinskii-Moriya interaction.Comment: 5 pages, 4 figure

    A luminescent 1D silver polymer containing [2.2]paracyclophane ligands

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    Funding: UK EPSRC Grant Number(s) EP/P014082/1, EP/M02105X/1, EP/R035164/1).[2.2]Paracyclophane scaffolds have seen limited use as building blocks in supramolecular chemistry. Here, we report the synthesis and characterization of a 1D coordination polymer consisting of silver(I) ions bound to a [2.2]paracyclophane scaffold functionalized with two 4-pyridyl units. The structure of the polymer has been determined from single crystal X-ray diffraction analysis and reveals two different silver coordination motifs that alternate along the 1D coordination polymer. The coordination polymer exhibits strong blue and sky-blue fluorescence in solution and in the crystalline solid state, respectively.Publisher PDFPeer reviewe

    Gridmapping the northern plains of Mars: Geomorphological, Radar and Water-Equivalent Hydrogen results from Arcadia Plantia

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    A project of mapping ice-related landforms was undertaken to understand the role of sub-surface ice in the northern plains. This work is the first continuous regional mapping from CTX (“ConTeXt Camera”, 6 m/pixel; Malin et al., 2007) imagery in Arcadia Planitia along a strip 300 km across stretching from 30°N to 80°N centred on the 170° West line of longitude. The distribution and morphotypes of these landforms were used to understand the permafrost cryolithology. The mantled and textured signatures occur almost ubiquitously between 35° N and 78° N and have a positive spatial correlation with inferred ice stability based on thermal modelling, neutron spectroscopy and radar data. The degradational features into the LDM (Latitude Dependent Mantle) include pits, scallops and 100 m polygons and provide supporting evidence for sub-surface ice and volatile loss between 35-70° N in Arcadia with the mantle between 70-78° N appearing much more intact. Pitted terrain appears to be much more pervasive in Arcadia than in Acidalia and Utopia suggesting that the Arcadia study area had more wide-spread near-surface sub-surface ice, and thus was more susceptible to pitting, or that the ice was less well-buried by sediments. Correlations with ice stability models suggest that lack of pits north of 65-70° N could indicate a relatively young age (~1Ma), however this could also be explained through regional variations in degradation rates. The deposition of the LDM is consistent with an airfall hypothesis however there appears to be substantial evidence for fluvial processes in southern Arcadia with older, underlying processes being equally dominant with the LDM and degradation thereof in shaping the landscape

    Radiocarbon ages of pre-bomb clams and the hard-water effect in Lakes Michigan and Huron

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    Five radiocarbon ages, all determined by accelerator mass spectrometry, have been obtained for two pre-bomb bivalves from Lake Michigan and one from Lake Huron. After correcting those ages for the fractionation of 14 C in calcite and for the radioactively inert CO 2 in the atmosphere, we find residual ages, caused by the hard water effect, of about 250 years for Lake Michigan and 440 years for Lake Huron.Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/43072/1/10933_2004_Article_BF00682596.pd
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