- minerals (rocks, sand, clay, chalk etc.)
- organic matter (this means the remains of plants and animals - but when this post talks about adding organic matter, it mainly means decayed vegetable matter like compost or the manure of herbivorous animals such as horses, rabbits and guinea pigs)
- living organisms that live in it (worms, insects, micro-organisms and even my mortal enemy, the slug).
What sort of soil you have largely depends on the mineral components in the soil. The main types are: clay, sandy, silt, loamy, chalky or lime-rich and peat soils. This last one isn't actually so much based on a mineral as on the organic matter - peat - but all the rest are characterised by the key minerals in them. Practically no one has peat soil in their garden (and presumably if you do, you live near a peat bog and know all about peat), so I'm mainly going to ignore that one.
If you live in the UK, you can find out what your soil's likely to be using this map: http://www.landis.org.uk/soilscapes/
According to the map, my soil is likely to be loamy. I say "likely to be" because my gardening course said soils could vary even across a single garden.
If you live in the UK, you can find out what your soil's likely to be using this map: http://www.landis.org.uk/soilscapes/
According to the map, my soil is likely to be loamy. I say "likely to be" because my gardening course said soils could vary even across a single garden.
If you don't live in the UK or want to double check whether what the map says makes sense for what you're seeing, here are two questions to help you easily identify if you have a strongly chalky or clay soil followed by some other questions if the answer turns out not to be obviously one of those:
1. Does it have pieces of chalk in it? They're white and you can easily use them to draw a line on other stones (just like the sticks of chalk you can buy for a blackboard). If so, you have chalky soil.
2. Does your soil act a lot like potters clay? It's dense, sticky or slimy and like moist clay, and hard to dig when it's been raining and very hard, cracked and dry clay-like and hard to dig when there's been no rain for ages, particularly when it's been hot. When it's moist, you can shape it and it stays that way, a bit like you can with pure clay. (You can possibly tell I once had a bad experience trying to help a friend dig his clay soil garden, it was much harder than I was used to).
Once you've got past those simple questions which show if your soil has a lot of obvious chalk or clay, things get a little more complicated. The first thing to do is feel your soil between your fingers.
How does the soil feel?
sticky and heavy (like moist clay) | clay soil |
slimy | clay soil |
gritty and light (a bit like sand on a beach, but often not sandy in colour) | sandy soil |
friable = easily crumbled | loamy soil (or in my experience, can also be sandy, as sandy soil sometimes seems as friable as it does gritty) |
slightly soapy, slippery | silt soil (pure silt soils are rare in gardens) |
If the answer is obvious, you can stop there, if not, ask:
What does the soil look like in the jam jar test?
Put about a tablespoon or two of soil in the bottom of an empty jam jar (no need to use a tablespoon, that's just a guide to the rough amount you're aiming for). Fill it up with water, give it a good shake, then leave it for an hour. After an hour, the organic parts of the soil should be floating on the surface. The question is what's happened to the rest:
What happens if you try to roll a sausage out of your soil when it's moist?
This all seems to back up Soilscape's view that I have a loamy soil.
What colour is the soil?
Put about a tablespoon or two of soil in the bottom of an empty jam jar (no need to use a tablespoon, that's just a guide to the rough amount you're aiming for). Fill it up with water, give it a good shake, then leave it for an hour. After an hour, the organic parts of the soil should be floating on the surface. The question is what's happened to the rest:
white bits floating in the water | chalky soil |
water might look a bit murky, but thin and the soil has sunk to the bottom; if you try and get the wet soil to stick together it either won't stick together at all or has difficulty sticking together, it feels a bit gritty | sandy soil |
the water either has bits of clay floating in it or is no longer transparent, but has formed an emulsion with the clay or both, any soil at the bottom doesn't feel gritty and can be clumped together into a ball that stays together quite well | clay soil |
like clay, but what's left at the bottom of the jar feels gritty | loamy soil, which is a mixture of clay, sand and silt |
Soil from my garden (loamy according to Soilscape) one hour after I shook the jar. No sign of chalk and not seeing much sign of clay. |
What happens if you try to roll a sausage out of your soil when it's moist?
rolls into a completely uncracked sausage, shiny when rubbed | high clay content |
rolls into a completely uncracked sausage and is a bit sticky, but not shiny when rubbed | clay soil, but lower clay content |
won't roll into a sausage at all | no clay content |
rolls into a cracked sausage, not sticky | I couldn't find a definitive answer on that. Possibly loamy soil. As far as I can make out, it's not a soil you'd refer to as a clay soil, but it may have some clay content. |
Me finding particles in my soil - could be sand or silt or both, but definitely not pure clay |
What colour is the soil?
very pale/greyish, chalky coloured soil | chalk (not being this colour doesn't mean no chalk) |
a bit orange or reddish | clay soil with a high clay content can look reddish or orangey (not being this colour doesn't mean no clay) |
lighter coloured soil | probably contains less organic matter |
darker coloured soil | probably contains more organic matter |
My soil (not dark brown, but definitely not chalky or greyish either) |
Well-rotted organic matter from the bottom of my compost heap |
Clay soil
The good news: clay
soils are very rich in nutrients. They are usually pH neutral
(neither acidic nor alkaline), which means that their pH is 7. Most
plants prefer pH 6.5-7, so they're good for most plants.
The bad news: they can
get very cloddy and tend to be hard to dig whether they're wet or
dry. They also hold a lot of water, which is sort of good because
they need watering less often, but bad because they tend to get
water-logged, which plants don't like. They also take longer to warm
up in spring, which means effectively spring comes later for your
plants. Also, they're easily damaged when water-logged, so don't dig
them or walk on them till they've dried up a bit (although completely
dry won't work either, as they can bake rock hard).
What to do to help: add
plenty of organic matter. This will break the clay down into crumbs,
which will make its nutrients more available to plants and also make
the soil warmer, easier to work and less prone to compaction. Also,
dig them in autumn or early winter when they're less wet to avoid
damaging them. If you leave them in narrow ridges after digging, this
could help drainage and encourage frost to help break them down
instead of you digging. Adopting a no-dig regime may be better for
the soil (and a lot less work for you) – I'll be talking more about
no-dig systems in later posts, as my bad back means no-dig' could be
really handy for me.
See here for more
information and advice from the RHS.
Sandy soil
The good news: these
are easy to dig and cultivate and generally to work. They warm up
quickly, which effectively means spring comes earlier for your
plants. They also tend not to get water-logged because they're free
draining, so plants that like it dry (don't like soggy roots) will
thrive. According to this article in the Telegraph, you may well be less troubled by slugs and snails than people with less freely draining soils.
The bad news: because
they're so free draining, they lose water easily and need a lot of
watering (hard work and/or bad for the environment). They're also
naturally low on nutrients unless they contain plenty of organic
matter. They can also be very acidic. Acidic soils are pH 6.9 and
below, and most plants prefer pH 6.5-7, so lower than 6.5 will not
suit quite a lot of plants.
What you can do to
help: add plenty of organic matter, this will bind the loose sand
into more fertile crumbs, stopping it from draining quite so quickly.
It also adds nutrients and makes the nutrients more easily available
to plants. Adding fertilisers can help provide the nutrients it's
missing. Choose plants that can cope without much water and add a
mulch to the top to preserve as much water as you can. Also, it may
pay to pH test your soil, and stick to plants that do well in its
level of acidity. I'm going to write more about soil pH in another
post.
See here for more
information and advice from the RHS.
Silt soil
The good news: these
are fertile, fairly well drained and hold more moisture than sandy
soil.
The bad news: these
soils are made up of fine particles (even finer than sand) and can be
easily compacted by treading and use of garden machinery. They are
prone to washing away and to wind erosion if left exposed to the
elements without plant cover.
What to do to help: add
plenty of organic matter. This will bind the silt particles into more
stable crumbs.
Loams
The good news: lucky
you, these are considered to have a perfect balance of all soil
particle types, they're 40% sand. 40% silt and 20% clay. This means
they're fertile, well drained and easily worked.
The bad news: slugs seem very happy in loamy soil (they're certainly present in large numbers in my garden and this article in the Telegraph seems to imply that slugs are happy in soils that can retain moisture well). You may well have a lot of them.
What you can do to
help: even though this soil type is great, the advice is that you
should still regularly add organic matter. I assume this is to
replenish nutrients your plants are using up. Also, according to the descriptions of different types of loamy soils on Soilscape's map, not all loamy soils are high in nutrients.
Chalky soil
The good news: some of
Britain's most productive agricultural soils are chalky. They warm up
quickly in spring and brassicas (plants including cabbage,
cauliflower and broccoli) are less likely to get clubfoot. Light
chalky soils rarely flood because they're free draining.
The bad news: because
chalk soils are alkaline (i.e. they have a pH of 7.1 or more – the
higher the pH the more alkaline it is) they won't support lime-hating
plants or ericaceous plants that need acid soil conditions, and you
can't acidify a chalk soil. A lot of chalky soils are shallow, i.e.
if you dig down through the soil, you'll get through it and hit the
layer of rock below quite quickly. They're also free-draining (i.e.
need watering regularly) and low in nutrients, but where clay is
present, nutrient levels might be higher and they might be able to
retain more water. Organic matter often breaks down quickly in chalky
soils.
What to do to help:
Choose plants that will thrive in alkaline conditions (also known as
calcioles or lime-loving plants). If you want to plant acid-loving
plants or lime-hating plants (also known as calcifuges), plant them
in a pot or a raised bed that you've filled with a suitable soil
you've bought (with a raised bed if you just use acidic compost it
will eventually sink away into your soil, so actually buy acidic soil
rather than compost. That can't happen with a pot, so acidic compost
should be fine). Add organic matter very frequently.
See the RHS's website
for more information and tips on chalky soil.
Peat soil
The good news: they've
usually very fertile and contain a high proportion of organic matter
(peat). It warms up quickly in the spring. It's great for plant
growth if fertiliser is added.
The bad news: highly
water retentive, so may require drainage if the water table is neat
the surface. Fewer nutrients because because the soil’s acidic
nature inhibits decomposition or organic matter (which is a reason
there's so much of it).
What to do to help: add
fertiliser. Unlike the other soils, presumably adding organic matter
doesn't help because it's already full of it.
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