CONTROLLING EROSION
(Page 11 of 19)
Rills. The easiest way of stopping a gully
is to catch it early. Whenever you see small rills (or
channels), get right to work. Use a mattock or a hoe to
break them up. Work in some compost or rotted manure, if
you can, and rake the area smooth. Then treat the area as
you would for sheet erosion — seed it, mulch it, or
possibly use brush mats or contour trenches.
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Gully monsters. A neglected rill may grow
up to be a monster gully. In the next two pages I'll tell
you how to go about fighting and conquering gullies. It's a
long, complicated fight, but very much worth the trouble.
We no longer have fire-eating dragons, but we do have
land-eating gullies to fight. Just to make sure you can
find your way through the following instructions, here is
an outline of the battle plans.
[1] Stabilize the gully bottom. The bottom is more
important than the sides. If the gully continues to dig
deeper, no matter what else you do, the sides will cave and
slump. You've got to prevent the gully from getting any
deeper, and you should even attempt to build up the bottom.
[2] Grade the walls of the gully to their angle of
repose — the angle at which they will no longer
slump or slide.
[3] Stop or reduce the flow of water entering the gully.
[4] Plant an immediate cover of grasses and legumes that
will hold everything together for a season or two.
[5] Plant a permanent cover of native shrubs, trees, vines,
and grasses that will eventually stabilize the area,
perpetuate themselves, build up soil fertility, encourage
wildlife, and completely restore the land.
Check dams. The way to stabilize the gully
bottom and build it up again is with check dams. Please
don't be intimidated by the thought of building a dam.
You're not going to be competing with Grand Coulee or
Aswan. In fact, your check dams won't even hold any water.
They are merely obstructions that will slow the water down.
And the best of all possible obstructions (as we all know
from our various misadventures in life) is a big mess.
Basically that is what a check dam is: a big mess of brush
or perhaps straw packed into the bottom of the gully, with
a simple structure to hold it all in place.
Why a check dam works. I think we all have
an intuitive sense of why a check dam works: A slow-moving
stream carries far less silt and does far less damage than
a raging torrent. But to understand how dramatically true
this is, you might want to consider a few hard-core
engineering facts. If you reduce the speed of the flow of
water by one-half, here (according to certain laws of
hydraulics) is what happens:
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