Good soil is the basis of a good garden. By understanding, managing and improving your soil you will be able to use less water, while maintaining an attractive looking garden, even in the toughest times. Understanding your soil will also help you choose the right plants for your conditions.
Understanding soil
The water holding capacity of a soil directly relates to the soil type, especially its structure and texture.
Soil structure and soil texture
A good soil consists of peds (soil particles held together by humus) with spaces between them called ‘soil pore space’.
These spaces can accommodate air, water, micro-organisms and roots of plants. The amount and type of pore space varies with soil texture and structure. A good soil has up
to 50 per cent pore space by volume
.
Soil structure relates to the arrangement of soil particles and their pore space.
Texture relates to the soil particle sizes from gravels through to coarse sands, fine sands through to silts, and finally clays which have the smallest of soil particles.
The infiltration rate of the soil relates to the rate at which water will soak into soil. A good textured and structured soil should have a good infiltration rate.

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A simple test to determine your soil
type
Take a handful of your soil and make it just
damp. Try forming it into a ball or sausage in
your palm. If it forms a ball that readily stays
in shape then your soil is clay. If it tends to
hold its shape, but is a bit crumbly, then it is
loam. A sandy soil will not hold shape but fall
apart very quickly.
Loam
A loamy textured soil with a crumbly
structure and with good pore space will allow
water to move through it by capillary action
similar to how water moves when it soaks
through blotting paper.
Well-structured clays and sandy loams with
lots of organic matter are the best soils for
holding the largest amounts of water for plant
growth.
Clay soil
If your soil is clay you may want to add
gypsum to help break it up. This helps water
get in more easily, and also breaks up the
crust that often forms and makes water run
off the surface, rather than soak in. Gypsum
is available in both a powder and spray-on
formula.
Clay soils may need deep-ripping or breaking
up when almost dry to help with initial
aeration, but it is bad practice to cultivate
wet or very dry clay soils.
Sandy soil
Sandy soils lose their moisture very quickly.
Many are also hard to wet again once
they have dried out. With sandy soils it is
important to constantly add old organic
matter. |