Soils are generally described according to the predominant type of soil particle
present - sand, silt, or clay. By conducting a simple soil test, you can easily
see what kind of soil you're dealing with. You may want to repeat this test
with several different soil samples from your lawn and garden.
Fill a quart jar about 1/3 full with topsoil and add water until the jar
is almost full.
Screw on the lid and shake the mixture vigorously, until all the clumps
of soil have dissolved.
Now set the jar on a windowsill and watch as the larger particles begin
to sink to the bottom.
In a minute or two the sand portion of the soil will have settled to the
bottom of the jar (see illustration). Mark the level of sand on the side of the jar.
Leave the jar undisturbed for several hours. The finer silt particles will
gradually settle onto the sand. You will find the layers are slightly different
colors, indicating various types of particles.
Leave the jar overnight. The next layer above the silt will be clay. Mark
the thickness of that layer. On top of the clay will be a thin layer of organic
matter. Some of this organic matter may still be floating in the water. In
fact, the jar should be murky and full of floating organic sediments. If not,
you probably need to add organic matter to improve the soil's fertility and
structure.
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