Soils, their formation, properties, composition, and relations to climate and plant growth in the humid and arid regionsHilgard, Eugene W. (Eugene Woldemar)
Science
Soils, their formation, properties, composition, and relations to climate and plant growth in the humid and arid regions
Hilgard, Eugene W. (Eugene Woldemar)
Soils
_Specific Heat._—Considering next, the column showing the “specific
heat” of water as compared with other substances, we see that it
exceeds all other known bodies in the amount of heat required to change
its temperature; hence again, _its_ heat capacity is taken as the unit
to which all others are compared. The figures given in the table show
that even ice and steam require for equal weights only about half as
much heat (or burning of fuel) to change their temperature (_e. g._,
1 degree) as would liquid water. But earthy matters, such as clay or
soil and glass, require only one-fifth as much heat for a similar
change; charcoal only about one-fourth as much. But vegetable matter as
represented by wood on the one hand, and gold and lead on the other,
require only about one-thirtieth as much heat as an equal weight of
water; zinc about one-tenth as much, steel somewhat more.
It is thus plain that masses of water act powerfully, more than any
other substance, as moderators of changes of temperature by their
mere presence. The body of an animal or plant is protected against
violent changes by the presence of from 60% to 90% of liquid water,
the temperature of which can only be raised or lowered slowly; and
the presence of the sea tempers the climates of coasts and islands
as compared with the heat or cold occurring in the interior of the
continents.
_Ice._—Again, it is shown in the table that the heat required to _melt
ice_ is greater than in the case of any other substance, especially
the metals; which when once heated to the fusing point, require only a
very little more heat to become liquid. The fusion of salts (including
silicate rocks) requires more heat than does that of the pure metals.
_Vaporization._—In the amount of heat required for its _vaporization_
water is also especially pre-eminent, and potent in its influence upon
organic life. The table shows that the evaporation of water requires
six hundred heat units[67] as compared with alcohol, requiring only two
hundred; while spirits of turpentine, the representative of a large
proportion of vegetable fluids, needs but sixty-seven.
[67] A heat unit, or “calorie,” is the amount of heat required to raise
the temperature of a unit-weight (pound, kilogram, or gram) of water
one thermometric degree. According to the unit-weight and thermometric
scale used, the figures will vary, but in this text the basis is
understood to be kilograms and the centigrade scale.
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