We are concerned at the
moment only with the physical character of the materials making
up a soil or growing medium. This is not to say that their chemical
characteristics are not important, but it is easier to take one
thing at a time.
Picture the spaces between
the solid particles of a soil. If the particles are large and of
an irregular shape they will lie together with larger spaces than
those left when small particles are involved. Think of some familiar
objects (even if they are spheres): a large garbage can filled with
basket balls would leave much more space unoccupied in the can than
would be the case if you had filled the can with golf balls. If
you added water to the cans, you could put more into the can with
basket balls than into the one with golf balls. Exactly the same
is true with soil particles: a coarse sandy soil has more air space
than one made up of clay particles which are many times smaller
than a grain of sand.
Continuing to think of
our garbage cans full of water and balls, if we now make a hole
in the bottom of each can, a lot of water will run out. As it does,
the spaces between the balls refill with air. But if we had measured
how much water went in with the basket balls and with the golf balls,
we would find that almost all ran out of the basket ball can, but
not quite all came out of the golf ball set up. This is because
some water stayed as wetness on the surface of each ball. If our
containers had been comparing a pot of coarse sand with a pot of
clay, the difference in the amount held would have shown up even
more, because the spaces between the particles of clay are so small
that some of them stay filled with water. This is important because
what it says is that water added to sand will almost all drain through,
while water added to clay will mostly drain through but will leave
some behind in the smaller spaces. At least part of this will be
available to plant roots.
If you want to know the
physics of this, it is that each molecule of water is attracted
to objects around it. This force is called adhesion when
the water molecules stick to the surface of the soil particles,
and cohesion when they stick to each other. The water drains
as long as the downwards force due to gravity is stronger than the
forces of adhesion and cohesion. The cohesive forces are only strong
enough to hold water in tiny spaces, which is why the big spaces
drain. The way in which plant roots take in water uses a different
mechanism, so that the film of water on the surface of soil particles
and the water in quite tiny spaces is available to them.
The ideal growing medium,
then, should have a mixture of larger and smaller spaces so that
some drain freely, giving the roots air, and some hold water which
the roots can use. You can specify this mix of pore sizes by careful
mixing of the materials that go into your growing medium.
Back
to Part A | On to Materials to
make a growing medium
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