PRACTICAL USE OF LEAVES.

There are two facts in the functions of the leaf, which are worth

consideration on account of their practical bearings. The food of

plants is, for the most part, taken in solution, through its roots.

Various minerals—silex, lime, alumen, magnesia, potassa—are passed

into the tree in a dissolved state. The sap passes to the leaf, the

superfluous water is given off, _but not the substances which it held

in solution_. These, in part, are distributed through the plant, and,

in part, remain as a _deposit in the cells of the leaf_. Gradually the

leaf chokes up, its functions are impeded, and finally entirely

stopped. When the leaf drops, it contains a large _per cent._ of

mineral matter. An autumnal or old leaf yields, upon analysis, a very

much larger proportion of earthy matter than a vernal leaf, which,

being yet young, has not received within its cells any considerable

deposit. It will be found also, that the leaves contain a very much

higher _per cent._ of mineral matter, than _the wood of the trunk_.

The dried leaves of the elm contain more than eleven _per cent._ of

ashes (earthy matter), while the wood contains less than two _per

cent._; those of the willow, more than eight _per cent._, while the

wood has only 0.45; those of beech 6.69, the wood only 0.36; those of

the (European) oak 4.05, the wood only 0.21; those of the pitch-pine

3.15, the wood only 0.25 _per cent._[5]

It is very plain, from these facts, that, in forests, the mineral

ingredients of the soil perform a sort of _circulation_; entering the

root, they are deposited in the leaf; then, with it, fall to the

earth, and by its decay, they are restored to the soil, again to

travel their circuit. Forest soils, therefore, instead of being

impoverished by the growth of trees, receive back annually the

greatest proportion of those mineral elements necessary to the tree,

and besides, much organized matter received into the plant from the

atmosphere; soils therefore are gaining instead of losing. If owners

of parks or groves, for neatness’ sake, or to obtain leaves for other

purposes, gather the annual harvest of leaves, they will, in time,

take away great quantities of mineral matter, by which the soil,

ultimately, will be impoverished, unless it is restored by manures.

Leaf-manure has always been held in high esteem by gardeners. But many

regard it as a purely _vegetable substance_; whereas, it is the best

mineral manure that can be applied to the soil. What are called

vegetable loams (not peat soils, made up principally of decomposed

_roots_), contain large quantities of earthy matter, being

mineral-vegetable, rather than vegetable soils.

Every gardener should know, that the best manure for any plant is the

decomposed leaves and substance of its own species. This fact will

suggest the proper course with reference to the leaves, tops, vines,

haulm, and other vegetable refuse of the garden.

The other fact connected with the leaf, is its function of

_Exhalation_. The greatest proportion of crude sap which ascends the

trunk, upon reaching the leaf, is given forth again to the atmosphere,

by means of a particularly beautiful economy. The _quantity_ of

moisture produced by a plant is hardly dreamed of by those who have

not specially informed themselves. The experiments of Hales have been

often quoted. A sun-flower, three and a half feet high, presenting a

surface of 5.616 square inches exposed to the sun, was found to

perspire at the rate of twenty to thirty ounces avoirdupois every

twelve hours, or seventeen times more than a man. A vine with twelve

square feet exhaled at the rate of five or six ounces a day. A

seedling apple-tree, with twelve square feet of foliage, lost nine

ounces a day.[6]

These are experiments upon very small plants. The vast amount of

surface presented by a large tree must give off immense quantities of

moisture. The practical bearings of this fact of vegetable exhalation

are not a few. Wet forest-lands, by being cleared of timber, become

dry; and streams, fed from such sources, become almost extinct as

civilization encroaches on wild woods. The excessive dampness of

crowded gardens is not singular, and still less is it strange that

dwellings covered with vines, whose windows are choked with shrubs,

and whose roof is overhung with branches of trees, should be

intolerably damp; and when the good housewife is scrubbing, scouring

and brushing, and nevertheless, marvelling that her house is so

infested with mold, she hardly suspects that her troubles would be

more easily removed by the axe or saw, than by all her cloths and

brushes. A house should never be closely surrounded with shrubs. A

free circulation of air should be maintained all about it, and

shade-trees so disposed as to leave large openings for the light and

sun to enter. Unusual rains in any season produce so great a dampness

in our residences that no one can fail to notice its effect, both on

the health of the occupants, and upon the beauty and good condition of

their household substance.

* * * * *

The following method to destroy weeds is pursued at the mint in Paris,

with good effect: 10 gallons water, 20 lbs. quicklime And 2 lbs.

flowers of sulphur are to be boiled in an iron vessel; after settling,

the clear part is thrown off and used when needed. Care must be taken,

for if it will destroy weeds it will just as certainly destroy edgings

and border flowers if sprinkled on them. Weeds, thus treated, will

disappear for several years.

[5] See Dr. Grey’s Botanic Text Book, an admirable work,

which every horticulturist should own and study.

[6] Lindley’s Horticulture, p. 42-44. Grey’s Botany, p. 131.

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