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GARDEN
SOIL
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SOIL OR
DIRT?
The old gardener's joke goes that "soil" is what you grow your plants in, and
"dirt" is what's under your fingernails.
Garden soil, where it all begins...
During several Pennsylvania winters, Bob taught adult-education Landscaping classes in Peters
Township.
Bob's
students always felt that way too much time was spent on soils.
B-O-R-I-N-G stuff they said!
But his curriculum never changed.
Why?
Because everything
begins with the soil. Once you understand the basics of soil science and begin to
apply what you've learned, plants will start to grow much better for you.
Hopefully,
this page and its links will teach you the basics of soil science. Even though these
pages specifically address soil conditions in Southwestern Pennsylvania, much of the
material here also applies to soil everywhere.
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SOIL.
. .
by the book!
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Soil is like a layer
cake:
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HORIZON |
NAME |
DEPTH |
FORMED
BY |
| A |
Topsoil |
6
- 12 inches |
Intermixing
of organic matter with mineral matter |
| B |
Subsoil |
10
- 20 inches |
Losses
from the "A" horizon |
| C |
Parent
material |
- |
The
material from which topsoil evolves |
Soil
Shredder

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Soil is loaded into the
hopper on the right where it is shredded into smaller particle sizes. It then
travels up the conveyor belt into a rolling screen. The "shredded and
screened" soil falls into a pile below for sale by the ton or cubic yard. The discarded soil and debris travels out the open end of the screen barrel
down the chute into a discard pile to be sold as "fill dirt." |
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So what
is soil?
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Average soil profile (by
weight):
95% to 99% - mineral
matter
5% to 1% - organic matter
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Average soil profile
(by volume):
50% solid -- 25% water -- 25% air
Therefore, 50% of the
average soil profile is "pore space" (25% air + 25% water = 50% pore
space). It's this pore space where plant roots actually grow. Think about it:
Plant roots actually grow "between" the soil, not "in" the soil.
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50%
SOLID |
25% WATER |
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25% AIR |
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Also, it's this pore space that gets reduced when soil is
"compacted." Everyone knows heavy equipment can compact soil, but most people
don't think about how much compaction can occur from ordinary foot traffic, such as on a
golf green. Compaction is an ongoing problem on athletic fields, especially if
fields are used when the soil is wet.
Sand, Silt or Clay?
Soil is classified
by particle size, with sand being the coarsest and clay being the finest. Pittsburgh
soils tend to be predominantly clay.
Clay soils have the "bad rap" since they can exhibit poor drainage
characteristics. However, clay soil has good nutrient-holding capability (a high
C.E.C.) and will hold moisture much longer than sandy soil. Most eastern U.S.
subsoils are 70% clay.
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| Soil
separates |
Diameter
(mm) |
| Clay |
<
0.002 |
| Silt |
0.002
- 0.02 |
| Sand |
0.02
- 2.0 |
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Soil Structure
DEFINITION: The
combination or arrangement of the primary soil particles (sand, silt, clay) into secondary
particles ("units" or "peds"). Rototilling soil that is too wet
breaks down soil structure and causes a crusted surface.
Soil pH
The activity of
Hydrogen ions in the soil determines its pH as being either acidic, neutral or alkaline.
Rainfall (H2O) in S.W. Pennsylvania continually introduces Hydrogen (H) ions into the soil
solution, causing soil to revert back to an acidic condition. (This is
why soil should be tested
every 3 to 5 years to determine its changing needs for lime)
The logarithmic scale measuring pH extends from zero to 14, with 7 being neutral.
Soil with a pH of 6 is 10-times more acid than soil with a pH of 7, while soil with a pH
of 5 is 100-times more acid than pH 7. Generally speaking, most plants grow best in
a soil pH of 6.5 to 7.2
Most soils we have tested in Washington County and Allegheny County range from pH 5.5 to
7. Unless "acid loving" plants are growing in these areas, agricultural
lime is used to raise the soil pH into a better plant growing range. (See
Soil pH
for more information)
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Some other "soil
basics"
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- Never
rototill or "work" soil when it is too wet! Tilling wet soil will ruin
soil structure and result in the formation of hard clumps. Always allow time for
your soil to dry enough for proper cultivation.
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When
tilling the soil, don't overdo it. It is best not to rototill the soil into a
powdery consistency.
Heavy
clay soils can be improved by working in organic matter. (See amendments for more information) The addition
of lime (if needed) or gypsum, will also help improve "heavy" soils.
Correcting
your soil pH will "unlock" nutrients which are already present in the soil, and
help maximize dollars spent on fertilizer.
Some
chemicals move very slowly down through the soil profile, and should be mixed-in with the
soil at planting time. These include phosphorus and calcium.
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Other Pages
For all of your
gardening needs, the internet is your best source. Whether you
are looking into buying
fruit tree seeds, or you need information about the soil you are
planting your trees in, the internet can help. Sign online today
and find out where your
local garden store is located. No matter what
shrubs and plant seeds you are looking for, you'll find the best
prices!
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Other
soil pages
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