GARDEN SOIL
We all
assume soil is just soil, but it is a very dynamic and variable material that
it is beneficial to understand exactly what we have in our garden so we can
know how to use it to get the best out of it for our plants.
Soil is a
mixture of sand, clay, silt, humus and stones and can vary in depth, colour,
drainage properties and nutrients available. No two soils are similar as they
will vary from one place to another depending on their location and history.
Some soils in the south of the UK sitting on the chalk downlands have a high pH
with problems of nutrients being locked up and unavailable to plants. Coastal
soils are often very dry if there is a lot of sand in the soil and these are
also very poor in nutrient availability as there is not much clay particles
which hold onto mineral nutrients. Some parts of Scotland in the north and west
have a high rainfall and poor drainage which favours the build up of organic
peat layers causing poor aeration and waterlogging.
However,
much of the UK has a fair mixture of sand, silt and clay which with the right
management can yield excellent results. The ideal soil for optimum plant growth
will have about 45% mineral sand, silt and clay with 5% humus and 50% pore
space to allow good water percolation and gaseous exchange. This will allow a
good environment for worms and other soil organisms, fungi and bacteria to
thrive and create a good soil colloidal crumb structure so that added organic
matter can be broken down into humus to improve structure and release
nutrients.
Formation of soils
Soil
formation is an ongoing process beginning with the weathering of rock. Volcanic
rock subjected to erosion by wind, water, acid rain and ice creates small
particles that get washed or blown down mountains till they accumulate in small
deposits. Algae and lichens can then grow on these and when they die they add a
small amount of humus. As the process continues the deposits grow bigger and
support more organisms then higher forms of plants life such as mosses and
ferns can grow. Eventually pioneer tree species will colonise the area with
roots that can penetrate deeper into the parent bedrock below the shallow soil
and help to disintegrate the rocks further.
Other
soils can be formed as tides and rivers deposit sand and silt every time there
is a flood creating alluvium plains which are usually very fertile. Retreating
glaciers from previous ice ages left behind deep deposits of boulder clays
found to be very fertile once cultivated, drained and the bigger rocks removed.
Soils can also be formed from areas of deep peat and silt once drainage has
been carried out, though peat soils lacking in clay content can be very low in
available nutrients.
Clay
soils may be subject to poor drainage and heavy to cultivate, but once well
drained and organic matter added they can be very fertile as clay can hold onto
and release its nutrients for the plants benefit. Clay particles are extremely
chemically active playing a very important role in holding and releasing plant
nutrients. However this activity is influenced by soil aeration, drainage and
pH levels.
The
optimum pH for healthy plant growth is about 6.5. Problems emerge when soil is
too acidic (well below pH6.0) or alkaline (above pH7.0) as some essential
nutrients are then locked up and unavailable to plants, and others may become
too readily available in toxic amounts.
Sandy
coastal soils may be very well drained, but can suffer in dry weather and lack
of clay content means they are usually very poor in nutrients. Adding manure,
compost or rotted seaweed can be very beneficial.
Soil improvements
To
support optimum plant growth soils need to be well drained, have adequate
organic matter such as manure or well rotted garden compost added to improve
the soil structure and provide the means for healthy soil organisms from worms
to bacteria to thrive.
Add a
green manure crop such as mustard, tares, clover, ryegrass or phacelia in
autumn or spring whenever the ground is free from crops. This will break up
heavy soils and increase air space, improving the soil colloidal structure, as
well as adding organic matter. Many of these green manures such as clover have
nitrogen fixing bacteria on their roots which greatly increase the availability
of nitrogen to the following crops. Crop rotation, liming once every four years
for the benefit of brassicas, and adding fertilisers will all help to increase
the soil fertility.
I am also
a great believer in double digging two feet deep and adding well rotted manure
or compost before planting long term permanent plants such as trees, roses and
fruit bushes.
However
those practitioners of the no dig camp at City Road allotments have certainly
been getting very impressive results on their vegetable crops, so we must keep
an open mind on the best practise way forward.
Pinus mugo the mountain pine is a dwarf pine that will
give character to rock gardens and heather borders. It is evergreen, easy to
grow and associates well with rocks and other hard landscaping. It is very
tough and tolerates a wide range of soils and exposure to winds. There are a
range of forms, so make sure you get a really dwarf type for rock gardens.
END