Curiosities of Science, Past and Present: A Book for Old and YoungTimbs, John
Science
Curiosities of Science, Past and Present: A Book for Old and Young
Timbs, John
Science
A person travelling may ascertain his rate of walking by the aid
of a slight string with a piece of lead at one end, and the use of
a seconds watch; the string being knotted at distances of 44 feet,
the 120th part of an English mile, and bearing the same proportion
to a mile that half a minute bears to an hour. If the traveller,
when going at his usual rate, drops the lead, and suffers the
string to slip through his hand, the number of knots which pass in
half a minute indicate the number of miles he walks in an hour.
This contrivance is similar to a _log-line_ for ascertaining a
ship’s rate at sea: the lead is enclosed in wood (whence the name
_log_), that it may float, and the divisions, which are called
_knots_, are measured for nautical miles. Thus, if ten knots are
passed in half a minute, they show that the vessel is sailing at
the rate of ten knots, or miles, an hour: a seconds watch would
here be of great service, but the half-minute sand-glass is in
general use.
The rapidity of a river may be ascertained by throwing in a light
floating substance, which, if not agitated by the wind, will move
with the same celerity as the water: the distance it floats in a
certain number of seconds will give the rapidity of the stream; and
this indicates the height of its source, the nature of its bottom,
&c.--See _Sir Howard Douglas on Bridges_. _Thomson’s Time and
Time-keepers._
SAND IN THE HOUR-GLASS.
It is a noteworthy fact, that the flow of Sand in the Hour-glass is
perfectly equable, whatever may be the quantity in the glass; that is,
the sand runs no faster when the upper half of the glass is quite full
than when it is nearly empty. It would, however, be natural enough to
conclude, that when full of sand it would be more swiftly urged through
the aperture than when the glass was only a quarter full, and near the
close of the hour.
The fact of the even flow of sand may be proved by a very simple
experiment. Provide some silver sand, dry it over or before the fire,
and pass it through a tolerably fine sieve. Then take a tube, of any
length or diameter, closed at one end, in which make a small hole, say
the eighth of an inch; stop this with a peg, and fill up the tube with
the sifted sand. Hold the tube steadily, or fix it to a wall or frame
at any height from a table; remove the peg, and permit the sand to flow
in any measure for any given time, and note the quantity. Then let the
tube be emptied, and only half or a quarter filled with sand; measure
again for a like time, and the same quantity of sand will flow: even if
you press the sand in the tube with a ruler or stick, the flow of the
sand through the hole will not be increased.
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