994 resultados para Fernando VI, King of Spain-Funeral Orations
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Mode of access: Internet.
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Margaret, daughter of James I. of Scotland, dauphine of France, by H. E. Butler.--Elizabeth of Bohemia, daughter of James I. and VI., by R. H. Hodgkin.--Mary of Orange, daughter of Charles I. and mother of William III., by A. Cecil.--Henrietta of Orleans, daughter of Charles I., by J. S. C. Bridge.--Sophia of Hanover, grand-daughter of James I. and VI., and mother of George I., by the editor.
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Mode of access: Internet.
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Photostat (negative) of copy in the British museum.
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Mode of access: Internet.
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Mode of access: Internet.
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Mode of access: Internet.
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"Account of the province of Vilcapampa and a narrative of the execution of the Inca Tupac Amaru, by Captain Baltasar de Ocampo (written in 1610) translated from a manuscript in the British museum": p. [203]-247.
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Half-title of v. 4: Bohn's historical library.
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Mode of access: Internet.
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Mode of access: Internet.
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This paper presents the results of an electrochemical study of the anodic characteristics of arsenopyrite in strongly alkaline solutions and of the cathodic reduction of ferrate( VI) and of dissolved oxygen at an arsenopyrite surface at potentials which are relevant to the oxidation reactions. Cyclic voltammetry at both arsenopyrite disc and arsenopyrite disc/platinum ring electrodes has shown that arsenic(III) is the main product of the anodic process at potentials in the region of the rest potential during oxidation by either ferrate( VI) or oxygen. Evidence for partial passivation of both the anodic and cathodic reactions has been obtained from potentiostatic current - time transients. The initial stage of oxidation by ferrate( VI) has been shown to be mass-transport controlled and this is also true of the oxidation by oxygen in dilute solutions of sodium hydroxide.
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Chemical Stratigraphy, or the study of the variation of chemical elements within sedimentary sequences, has gradually become an experienced tool in the research and correlation of global geologic events. In this paper 87Sr/ 86Sr ratios of the Triassic marine carbonates (Muschelkalk facies) of southeast Iberian Ranges, Iberian Peninsula, are presented and the representative Sr-isotopic curve constructed for the upper Ladinian interval. The studied stratigraphic succession is 102 meters thick, continuous, and well preserved. Previous paleontological data from macro and micro, ammonites, bivalves, foraminifera, conodonts and palynological assemblages, suggest a Fassanian-Longobardian age (Late Ladinian). Although diagenetic minerals are present in small amounts, the elemental data content of bulk carbonate samples, especially Sr contents, show a major variation that probably reflects palaeoenvironmental changes. The 87Sr/86Sr ratios curve shows a rise from 0.707649 near the base of the section to 0.707741 and then declines rapidly to 0.707624, with a final values rise up to 0.70787 in the upper part. The data up to meter 80 in the studied succession is broadly concurrent with 87Sr/86Sr ratios of sequences of similar age and complements these data. Moreover, the sequence stratigraphic framework and its key surfaces, which are difficult to be recognised just based in the facies analysis, are characterised by combining variations of the Ca, Mg, Mn, Sr and CaCO3 contents