Soil Structures
In Nature, the earth is not tilled, and fertilizers
(dead plants and animals, fallen leaves, etc.) begin as mulches on the soil's
surface. Beneath this mulch layer, undisturbed soils develop two distinct
features central to the natural interactions between plants and soils. One of
these features consists of the soil "horizons" which result from the tendency
of the soil to separate into horizontal strata (i.e., mulch, topsoil, and
subsoil). The other is a valuable, spongy condition called "crumb structure."
Tilling both mixes the soil's horizons and destroys its crumb structure,
interfering with the processes and organisms which have evolved to depend upon
these features.
Soil Horizons
The soil horizons include the mulch, topsoil, and
subsoil layers. The mulch layer consists of plant and animal remains, and is
the primary source of the soil's fertility. The topsoil consists of mineral
soil, huge numbers of soil organisms, dissolved nutrients, organic matter
brought down from the mulch layer, and humus (humus results from the breakdown
of organic matter and has an enormous capacity to absorb moisture, hold
nutrients, and buffer pH extremes). It is in the topsoil that the majority of
the soil's fertility is stored, in the form of soil life and as nutrients held
in solution by the soil's humus and clay. The subsoil consists mostly of
mineral particles, leached nutrients, and the deeper water- and mineral-seeking
plant roots.
Crumb Structure
Crumb structure is a spongy state developed and
maintained by the movement of earthworms and plants' roots through the soil.
The crumb structure is held together by soil colloids (gel-like substances
created by decay organisms), and by earthworms' secretions, used to aid their
movement through the soil. Natural crumb structures are quite stable and remain
largely intact after rains. The sponginess of the crumb structure is extremely
conducive to soil aeration, and to infiltration of water and dissolved
nutrients into the soil.
Using Rock Powders to Increase Fertility
Since no-till gardening
relies on earthworms to do all the digging (which includes mixing mineral
powders into the soil), prior to each mulching a rock-powder mix is applied at
the rate of about 4 to 5 pounds per 100 square feet. A good mix consists of
roughly equal parts of soft rock phosphate (for slow-release phosphorous),
gypsum (for a non-alkaline source of calcium - use lime if your soil is
acidic), hardwood ashes (potassium and trace minerals), and bone meal (more
phosphorous and calcium). These rock powders will then be slowly and evenly dug
in by the worms and the rain as the mulch is consumed.
Tilling and Soil Structure
Tilling mixes organic matter from the
mulch layer into the topsoil where is decomposes too quickly for plants to
completely utilize (creating a feast-or-famine nutrient cycle) and also mixes
mulch materials into the subsoil where they are attacked by anaerobic bacteria
(which excrete metabolic byproducts toxic to plant life and soil organisms).
Tilling exposes the topsoil's extremely valuable and slowly-forming humus to
the air where it can be oxidized and lost, and destroys the soil's existing
crumb structure. Tilling decimates the earthworm population, thereby slowing
reestablishment of a new crumb structure, and can cause the formation foa
hardpan by dislocating fine soil particles and allowing them to be washed
downward toward the subsoil where they collect and form a dense sedimentary
layer. In short, naturally occurring soil horizons and crumb structures serve
vital functions which are interrupted, not aided, by tilling. And since natural
patterns always begin to reestablish themselves immediately once disturbed, the
gardener who tries to circumvent or override them has to work constantly to
prevent their return.
Mulch and Soil Tilth
From these facts it is clear that tilling is an
ineffective and at best temporary approach to increasing soil tilth and
fertility. Rather than attempting to enforce our own idea of soil tilth on our
gardens, we are better advised to cooperate with and use the soil's own natural
method for improving fertility - a thick, rich mulch of organic materials to
feed soil organisms and plants, which then work toghether to establish natural
soil tilth.
Applying Mulches
The most important single strategy in a no-till
garden, then, is keeping a thick mulch on the beds at all times to feed the
earthworms and the soil. The right proportions are as important for mulches as
they would be for compost. The mulch must contain enough grass clippings or
other sources of nitrogen to suppoly decomposition microorganisms, or it will
temporarily rob the soil of nitrogen (thereby starving plants). Also needed are
high-carbon materials like tree leaves, which create humus and keep nitrogenous
materials from packing into a mucky layer which would exclude rainwater and air
from the soil. By spreading mulches directly on the soil, instead of first
converting them to compost, organic materials do double duty - serving as
mulch, and as a slow-release organic fertilizer, soil coniditioner, and worm
food. Furthermore, the fertilizing value of the materials is more fully
utilized, since in a compost pile much of the nitrogen, humus, and minerals are
lost through conversion to gases and by rainwater leaching.
The Nazarenes of Mount Carmel
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