| One of the most protracted arguments I’ve had began
when my buddy Leo goaded me by saying, “Dirt and soil are the same damn
thing.” Now, having spent many an early morning listening to my soils professor
express outrage at anyone who equated dirt with soil, I felt a moral obligation
to fire back the words I’d heard a hundred times: “Dirt is the stuff
trapped beneath your fingernails; soil is a miracle of nature that took thousands
of years to make... ya dufus.” Yes, the last bit was mine, but my point
is I thought I’d won until my friend pulled out a dictionary and pointed
to this: “dirt n. earth or garden soil.” What do dictionaries know?!
Therein lies the problem. Soil is the lifeblood of plants, yet we treat it
like... well, dirt. Not only do we demand complete servitude from it, we assume
it’ll provide us with wonderful plants year after year. So, in tribute to
this overworked and under appreciated stuff that’s erroneously (Yes, Leo,
erroneously!) called dirt, I thought a little soil primer was in order.
Simply put, soil is comprised of four ingredients: minerals, organic matter,
water and air. Minerals typically make up the bulk of soils and are one of three
types: sand, silt or clay. A soil balanced in these three minerals is called loam,
and loam is considered the ideal blend because it holds water and air in the right
proportions for plants. Shift the percentages in favour of one mineral, and you
can have a sandy loam, a silty loam or a clay loam—all of which can still
be good, depending on the climate.
For example, even though loam is considered the
soil paradigm, plants grown in drier regions of the prairies are usually a little
better off in clayey loam because it holds more water. In wetter regions, such
as those on the West Coast, plants often do better when grown in a sandier loam
because of the increased drainage it provides.
The one golden rule for gardeners from coast to coast is to add organic matter
to their soils every year. Organic matter is comprised of microscopic and
macroscopic organisms (think decaying and living critters) that provide plant
nutrients and “glue”
mineral fractions together into a nice, porous network that aids in the flow of
air and water to plants. The thing to remember, however, is that organic matter
is con- stantly being consumed as carbon dioxide by soil microorganisms or washed
and blown away through water and wind erosion. Simply adding a two-centimetre
blanket of compost or well-rotted manure to the soil each year and tilling it
in will not only stem the loss of organic matter but also allow it to build up.
It’s that easy.
The amounts of the last two soil ingredients, water and air, will be dictated
by the mineral and organic matter fractions of your soil. Soils that are loose
allow for good air infiltration. As for the amount of available soil water, that
will depend entirly on what both Mother Nature and you are prepared to provide.
So if you’re planning on gardening this year, take moment to think before
you dig. Give your soil a fraction of the TLC you give your plants, and remember
that no matter what people tell you, soil is not a dirty word. |