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  • Other Sources  (3)
  • Periodicals Archive Online (PAO)
  • American Geophysical Union (AGU)
  • Annual Reviews
  • 2000-2004
  • 1980-1984  (1)
  • 1975-1979  (2)
  • 1935-1939
  • 1
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    A significant upper limit for the rate of formation, of OCS from the reaction of OH with CS2 (1980)
    American Geophysical Union (AGU)
    In:  Geophysical Research Letters, 7 (10). pp. 797-800.
    Details
    Publication Date: 2020-07-30
    Description: The rate of reaction of OH with CS2 to form OCS by reaction (1) has been measured through observation of O14CS following 254 nm equation image photolysis of mixtures of H2O2 with 14CS2. The OH concentrations have been monitored through simultaneous measurement in the same cell of either (a) the oxidation of CO to CO2, or (b) the removal of a hydrocarbon such as C3H8 or iso-C4H10. The upper limit for the formation of OCS based on (a) corresponds to a rate constant k1 〈 0.3 × 10−14 cm³ molecule−1 sec−1. Other chemical reactions in the system have led to the formation of both 14CO and 14CO2, indicating the existence of a complex combination of reactions such that the observed O14CS need not have been formed by (1). The rate of reaction (1) is sufficiently slow that it is neither an important atmospheric sink for CS2 nor an important source for atmospheric OCS. The reaction of OH with OCS has not been measured in these experiments, but by analogy with k1 it is probably not an important atmospheric sink for OCS nor an important source of SO2.
    Type: Article , PeerReviewed
    Format: text
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  • 2
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    Quantifying Biostratigraphic Correlation (1978)
    Annual Reviews
    In:  Annual Review of Earth and Planetary Sciences, 6 (1). pp. 353-375.
    Details
    Publication Date: 2020-06-09
    Type: Article , PeerReviewed
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  • 3
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    Glacial Inception and Disintegration During the Last Glaciation (1978)
    Annual Reviews
    In:  Annual Review of Earth and Planetary Sciences, 6 (1). pp. 205-228.
    Details
    Publication Date: 2020-06-09
    Description: The causes of the growth and collapse of the large Pleistocene ice sheets is a topic of intense scientific debate. The amount of new data and ideas has been prodigious during the last ten years. This review concentrates on the shifting patterns of glacial advance and shrinkage during the last Glaciation. We also examine reconstructions of conditions during the maximum of this Glaciation about 18,000 BP, and the mechanisms that might have caused the rapid collapse of many of the world's ice sheets between 18,000 and 8000 BP. Our paper focuses on the North Atlantic sector because it is there that the major Pleistocene ice sheets grew, developed, and retreated.
    Type: Article , PeerReviewed
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