The Formation of Vegetable Mould Through the Action of Worms: With Observations on Their HabitsDarwin, Charles
Science
The Formation of Vegetable Mould Through the Action of Worms: With Observations on Their Habits
Darwin, Charles
Earthworms; Humification; Soils
WE now come to the more immediate subject of this volume, namely, the
amount of earth which is brought up by worms from beneath the surface,
and is afterwards spread out more or less completely by the rain and
wind. The amount can be judged of by two methods,—by the rate at which
objects left on the surface are buried, and more accurately by weighing
the quantity brought up within a given time. We will begin with the
first method, as it was first followed.
Near Mael Hall in Staffordshire, quick-lime had been spread about the
year 1827 thickly over a field of good pasture-land, which had not since
been ploughed. Some square holes were dug in this field in the beginning
of October 1837; and the sections showed a layer of turf, formed by the
matted roots of the grasses, ½ inch in thickness, beneath which, at a
depth of 2½ inches (or 3 inches from the surface), a layer of the lime in
powder or in small lumps could be distinctly seen running all round the
vertical sides of the holes. The soil beneath the layer of lime was
either gravelly or of a coarse sandy nature, and differed considerably in
appearance from the overlying dark-coloured fine mould. Coal-cinders had
been spread over a part of this same field either in the year 1833 or
1834; and when the above holes were dug, that is after an interval of 3
or 4 years, the cinders formed a line of black spots round the holes, at
a depth of 1 inch beneath the surface, parallel to and above the white
layer of lime. Over another part of this field cinders had been strewed,
only about half-a-year before, and these either still lay on the surface
or were entangled among the roots of the grasses; and I here saw the
commencement of the burying process, for worm-castings had been heaped on
several of the smaller fragments. After an interval of 4¾ years this
field was re-examined, and now the two layers of lime and cinders were
found almost everywhere at a greater depth than before by nearly 1 inch,
we will say by ¾ of an inch. Therefore mould to an average thickness of
0.22 of an inch had been annually brought up by the worms, and had been
spread over the surface of this field.
Public-domain text, read in full here on John Shaqi.
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