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  • 1995-1999  (2)
Material
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Year
  • 1
    Electronic Resource
    Electronic Resource
    Cambridge : Cambridge University Press
    The @British journal for the history of science 29 (1996), S. 155-169 
    ISSN: 0007-0874
    Source: Cambridge Journals Digital Archives
    Topics: History , Natural Sciences in General
    Notes: Between 1856 and 1858, a group of entrepreneurs and engineers led by the American Cyrus Field and the Englishmen J. W. Brett, Charles Bright and E. O. Wildman Whitehouse sought to lay a telegraph cable across the Atlantic from Ireland to Newfoundland. Their projected cable would be far longer, far more expensive, and far more difficult to lay than any previously attempted; that such an ambitious undertaking was launched and quickly drew financial backing was testimony to the technological enthusiasm of the mid-Victorian era. After many setbacks, the cable was successfully completed early in August 1858. The first messages it carried were met with rapturous excitement on both sides of the Atlantic – making its failure after just a few weeks of fitful service all the more humiliating. Identifying the causes of that failure, and assigning blame for them, became crucial to ensuring the future of transoceanic cable telegraphy. Were the causes of the failure intrinsic to the enterprise, and the vision of a network of transoceanic cables no more than an unrealistic dream? Or did the collapse of the cable result simply from a series of unfortunate and correctable errors? How those questions were answered in the autumn of 1858 would go far toward determining the prospects not only for renewing the Atlantic project, but also for any attempt to extend submarine cables more widely around the world.
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Ground water 37 (1999), S. 0 
    ISSN: 1745-6584
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Energy, Environment Protection, Nuclear Power Engineering , Geosciences
    Notes: A solution is obtained for stream flow depletion created by pumping from a well beside a stream. This solution assumes that streambed penetration of the aquifer and dimensions of the streambed cross section are all relatively small. It also assumes that the streambed is clogged and that a linear relationship exists between the outflow seepage through the streambed and the change in piezometric head across the semipervious clogging layer. The solution is general enough to include the earlier solutions of Theis, Glover and Balmer, and Hantush. A solution is also obtained for the drawdown at any point within the aquifer, and it is suggested that this solution might be matched with experimental field data to obtain estimates for aquifer and streambed leakage parameters.
    Type of Medium: Electronic Resource
    Library Location Call Number Volume/Issue/Year Availability
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