The mighty deep : $b and what we know of itGiberne, Agnes
Science
The mighty deep : $b and what we know of it
Giberne, Agnes
Marine biology; Nature study
An interesting experiment has been tried. A certain amount of hydrogen
gas and eight times as much of oxygen gas were weighed separately, by
means of very delicate instruments. Then through great heat the two
were caused to unite into water, and the water also was weighed. It
was found to be just as heavy as the two gases together had been; and
quite naturally so, since neither of the two gases had lost or gained
in weight. This kind of union is called “chemical.”
French people are fond of “eau sucré.” A lump of sugar is dropped into
a glass of water, and it disappears. But it has not been destroyed.
It has not ceased to be sugar. No mysterious union has taken place
between the sugar and the water. Neither water nor sugar has changed
its nature; and no fresh substance has come into existence in their
stead. The water is there, as it was before. The sugar is there too,
not visible, but to be found out by our sense of taste. It has only
been separated by the water into such minute particles that we cannot
see them. This is a case of mixing, not of chemical union.
When we think of the characteristics of Sea Water, as compared with
Fresh Water, we have to do with simple mixing. As sugar floats, unseen
but not untasted, in tea or coffee; so salt floats, unseen but not
untasted, in ocean waters.
Such a thing as absolutely pure water is very rare. No matter how clear
a stream may seem to us, it holds a vast number of specks of material,
collected from earth and air. Once a scientific man had some, most
carefully distilled, which seemed to be of crystal purity. But he put
it under the strong beam of an electric lamp, and, alas, for human
powers! after so doing he could only declare that the idea of purity
was ludicrous. If it is so with distilled water, the less said the
better about common drinking-water. It may be well for our peace of
mind that we have not stronger sight.
Ocean-water holds about two hundred times as much dissolved material as
ordinary fresh water. The different kinds of substances found in any
particular water-supply determine the character of that water, making
it sweet or sour or salt, rendering it health-giving or death-dealing.
Something has been said about the drying away of sea-water, and the
leaving of salt behind. A remarkable instance of salt thus left is seen
in the Rann of Cutch, a flat Indian plain, about a hundred and ninety
miles long, and half as wide.
During the south-west monsoon the ocean waters are forced by powerful
winds up the Gulf of Cutch to a considerable height, overspreading the
Rann, which for a time is turned into a shallow lake. When dry weather
comes, the water vanishes, partly retiring, partly evaporating; and a
salt-strewn desert is left, varied by sand-ridges, green spots, and
little lakes, but covered principally by “sheets of salt crust.” My
father, when there many years ago with his Regiment, noted down his
impressions of the scene.
Public-domain text, read in full here on John Shaqi.
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