The different modes of cultivating the pine-apple: From its first introduction into Europe to the late improvements of T.A. Knight, esq.Loudon, J. C. (John Claudius)
History
The different modes of cultivating the pine-apple: From its first introduction into Europe to the late improvements of T.A. Knight, esq.
Loudon, J. C. (John Claudius)
Pineapple
This is the latest printed account of Mr. Knight’s experiments on the
Pine Apple. It would be premature to draw any general conclusions in so
early a stage of their progress, and might excite prejudice to
anticipate the final result. That the Pine plant will grow and thrive
without what is technically called bottom heat, is an obvious truth,
since no plant in a state of nature is found growing in soil warmer than
that of the superincumbent atmosphere. But to imitate nature, is not
always the best mode of culture; for the more correct the imitation, the
less valuable would be the greater part of her products, at least as far
as horticulture is concerned. What would our celery, cabbage, and apples
be, if their culture were copied from nature? Though the Pine Apple will
grow well without bottom heat, it may grow with bottom heat still
better; and though the heat of the earth, in its native country, may
never exceed that of the surrounding atmosphere, it does not follow that
earth heated to a greater degree may not be of service to it, in a state
of artificial culture. But admitting, for the sake of argument, that the
Pine plant could be grown equally well with, as without bottom heat;
still it appears to us that the mass of material which furnishes this
heat, will always be a most desirable thing to have in a Pine stove, as
being a perpetual fund of heat for supplying the atmosphere of the
house, in case of accident to the flues or steam apparatus. Besides it
appears from nature, as well as from observing what takes place in
culture, that the want of a steady temperature and degree of moisture at
the roots of plants is more immediately and powerfully injurious to them
than atmospheric changes. Earth, especially if rendered porous and
spungelike by culture, receives and gives out air and heat slowly; and
while the temperature of the air of a country, or a hot-house, may vary
twenty or thirty degrees in the course of twenty-four hours, the soil at
the depth of two inches would hardly be found to have varied one degree.
With respect to moisture, every cultivator knows, that in a properly
constituted and regularly pulverized soil, whatever quantity of rain may
fall on the surface, the soil is never saturated with water, nor, in
times of great drought, burnt up with heat. The porous texture of the
soil and sub-soil being at once favourable for the escape of
superfluous water, and adverse to its evaporation, by never becoming so
much heated on the surface, or conducting the heat so far downwards as a
close compact soil.
Public-domain text, read in full here on John Shaqi.
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