John Young Buchanan

Summary

John Young Buchanan,  Popular Science Monthly (1881)

“ By far the greater part of the ocean is, for sounding purposes, practically still water. The surface-currents of any importance are easily recognized, and so also are the under-currents. Just as a physician can, by bringing his experience to bear on the sounds transmitted to him by the stethoscope, divine what is taking place inside the body of his patient, so the experienced seaman can, by observing the behavior of his sounding-line, form a fair diagnosis of what is taking place in the depths of the sea. When the sinker passes into a belt of under-current, the fact is very soon apparent ”
Source: Wikisource

John Young Buchanan,  Popular Science Monthly (1881)

“ Captain John Ross employed, during his Arctic voyage of 1818, one of the earliest satisfactory instruments for bringing up a considerable quantity of the bottom mud in deep water, with which he was able to ascertain the temperature at any depth.
A contemporary of Ross, the younger Scoresby, observed that, when in sounding at great depths the ordinary deep-sea line and lead are used, the increasing weight of line, in proportion as more of it is required, renders less certain the determination of the moment when bottom is reached.
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Source: Wikisource

John Young Buchanan,  Popular Science Monthly (1881)

“ It is necessary, in making a sounding in deep water, to load the end of the line with such a weight that in the deepest water that may be reasonably expected the velocity of descent shall not be diminished to an excessive extent by the friction of the increasing length of line in passing through the water. Wire has been largely employed for the line, and has great advantages in this respect over hemp. For example, in water of fifteen hundred fathoms a sinker weighing three hundred-weight is twenty minutes in reaching the bottom, with the best hempen sounding-line ”
Source: Wikisource

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