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Page 48
[Illustration: THE SNOWFLAKE, LEUCOJUM VERNUM, AT DRINKSTONE
PARK.]
Coniferous trees are sometimes considered as out of place in park
scenery; this, however, does not hold good at Drinkstone, where Mr.
Powell has been displayed excellent taste in the way of improving the
landscape and creating a really charming effect by so skillfully
blending the dressed grounds with the rich greensward of the park
that it is not easy to tell where the one terminates or the other
commences.
The park, which covers some 200 acres, including a fine lake over
eight acres in extent, contains also various large groups or clumps of
such species as the Sequoia gigantea, Taxodium sempervirens, Cedres
deodora, Picea douglasii, Pinsapo, etc., interspersed with groups of
ornamental deciduous trees, producing a warm and very pleasing effect
at all seasons of the year. Among species which are conspicuous in the
grounds are fine, well-grown examples of Araucaria imbricata, some 30
feet high; Cedrus deodara, 60 feet in height; Abies pinsapo, 40 feet;
and fine specimens of Abies grandis, A. nobilis, and A. nordmanniana,
etc., together with Abies albertiana or mertensiana, a fine,
free-growing species; also Libocedrus gigantea, Thuiopsis borealis,
Thuia lobbii, Juniperus recurva, Taxas adpressa, fine plants; with
fine golden yews and equally fine examples of the various kinds of
variegated hollies, etc.
[Illustration: ODONTOGLOSSUM ROSSI MAJOR VAR. RUBESCENS, AT DRINKSTONE
PARK.]
Particular attention is here paid to early spring flowers. Drinkstone
is also celebrated as a fruit growing establishment, more particularly
as regards the grape vine; the weight and quality of the crops of
grapes which are annually produced here are very remarkable.--_The
Gardeners' Chronicle._
* * * * *
ON THE CHANGES WHICH TAKE PLACE IN THE CONVERSION OF HAY INTO
ENSILAGE.
By FREDK. JAS. LLOYD, F.C.S., Lecturer on Agriculture, King's
College.
The recently published number of the _Royal Agricultural Society's
Journal_ contains some information upon the subject of silage which
appears to me of considerable interest to those chemists who are at
present investigating the changes which take place in the conversion
of grass into silage. The data[1] are, so far as I know, unique, and
though the analytical work is not my own, yet it is that of an
agricultural chemist, Mr. A. Smetham, of Liverpool, whose work I know
from personal experience to be thoroughly careful and reliable. I have
therefore no hesitation in basing my remarks upon it.
[Footnote 1: _Royal Agricultural Society's Journal_, vol. xx.,
part i., pp. 175 and 380.]
We have here for the first time an accurate account of the quantity of
grass put into a silo, of the quantity of silage taken out, and of the
exact composition both of the grass and resulting silage. I desire
merely to place myself in the position of, so to speak, a "chemical
accountant."
The ensilage has been analyzed at three depths, or rather in three
layers, the first being 1 foot, the second 1 ft. to 1 ft. 6 in., and
the third 1 ft. 6 in. to 2 ft. from the bottom of the silo. By
doubling the figures of the bottom layer analysis, adding these to the
second and third layer analysis, and dividing by 4, we obtain a fair
representation of the average composition of the silage taken
throughout the silo, for by so doing we obtain the average of the
analyses of each 6-inch layer of silage. The results of the analyses
are as follows, calculated on the dry matter. The moisture was
practically the same, being 70.48 per cent, in the grass and 72.97 in
the silage.
_Composition of Grass and Silage (dried at 100�C.)._
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