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  • Other Sources  (3)
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  • 1
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    Unknown
    Cambridge University Press
    In:  Geological Magazine, 99 (02). pp. 164-172.
    Publication Date: 2020-07-31
    Description: The results of an examination of one quarry within the gneisses of the Bartica Assemblage are described and the validity of these results throughout the whole of the Bartica Assemblage is discussed. The foliation and banding of the gneisses at Kereti Quarry are mainly the results of tectonism; concomitant metamorphism within the Amphibolite Facies was succeeded by a two-phase metasomatism involving successive additions of Na and K. These results appear valid throughout the Bartica Assemblage and it is further suggested that the main rock type distribution in the Bartica Assemblage is also controlled by tectonism.
    Type: Article , PeerReviewed
    Format: text
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  • 2
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    Cambridge University Press
    In:  Journal of Fluid Mechanics, 12 (04). p. 481.
    Publication Date: 2020-07-24
    Description: The energy flux in a finite-depth gravity-wave spectrum resulting from weak non-linear couplings between the spectral components is evaluated by means of a perturbation method. The fifth-order analysis yields a fourth-order effect comparable in magnitude to the generating and dissipating processes in wind-generated seas. The energy flux favours equidistribution of energy and vanishes in the limiting case of a white, isotropic spectrum. The influence on the equilibrium structure of fully developed wave spectra and on other phenomena in random seas is discussed briefly.
    Type: Article , PeerReviewed
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  • 3
    Publication Date: 2019-09-30
    Description: These data suggest that calcium may be lost during heavy sweating conditions (up to 20 mg calcium/hour) and that this loss should be considered in establishing recommended allowances for calcium. It was observed that 7 men consuming 441 mg of calcium a day in a study extending for 48 days, excreted 8.1, 11.6 and 20.2 mg/hour of calcium when living at 70, 85 and 100°F. This accounted for 21.8, 25.1 and 33.2% of the total calcium excreted. These observations are important since they show an additional calcium loss, which has not been reported in previous calcium balance studies in the literature. It is questionable whether an individual, consuming a low calcium diet, ever really attains calcium balance (equilibrium), under heavy sweating conditions. It was observed that (a) the calcium excreted in sweat, in men working at a moderate rate in extreme heat (100°F), was still fairly high after acclimatization, averaging 17 mg/hour after the first 4 days, and (b) that the daily total calcium in sweat increased as the sweat rate increased. Therefore it appears that the calcium requirements may be increased under these conditions. It was shown that even after acclimatization the urinary calcium did not decrease in compensation for the losses of calcium in sweat. It is recognized that changes in the urinary excretion of calcium in adjusting to different levels of dietary calcium and the various other metabolic factors, may require months to achieve.
    Type: Article , PeerReviewed
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