
Soil and lawn establishment
How to assess the soil beneath your lawn
A feel test, inspection pit and infiltration test reveal soil type, compaction and the path of water. Find out what to check before establishing a lawn.
Published by InteliDomeUpdated
In this article
The soil looks fine on the surface. But what will the roots find a few centimetres below? There may be a compacted layer that holds water, or sand that quickly loses moisture. Before ordering soil and amendments, find out what your garden actually needs. A feel test, a small inspection pit and an infiltration test will indicate where to act — and where to save yourself work because the soil already functions well.

Imagine a typical spring scenario: your new lawn comes up beautifully, everything is a fresh green and you water diligently. Then heavier rain arrives and persistent puddles appear on the lawn. Or a few hot days strike and the grass starts to weaken before your eyes. We reach for fertiliser, add more water and sow more seed.
Yet the problem often lies below the surface. Beneath ten centimetres of neatly spread soil, a layer compacted by construction machinery may still remain. No mower will remove it, and even the best fertiliser will not force a path through it for the roots.
Surprisingly, the most expensive soil beneath a lawn is often not the costly load delivered by a lorry. It is the soil we forget to check before sowing. We cannot choose the right preparation until we know what type of soil we have in the garden.
Is it mainly sandy, clay or loamy? Its type gives us clues about how it handles water and air; what helps one soil may be unnecessary in another. By also checking how water moves through it, we can choose suitable preparation for the grass roots.
Only then does it make sense to think about grass seed. Understanding this sequence can also save you unnecessary spending on work your garden does not need. Take a spade and a little water, and let us get our hands dirty — a simple feel test will give us the first clue.
The feel test: sand, clay or loam? Your hand can tell you
We often use the word “soil” as a catch-all for whatever sticks to our boots. For a lawn, though, that is not precise enough. As a starting point, we divide soil into three groups: heavy clay, medium loam and light sandy soil. Although many intermediate types exist in nature, this grouping tells us the most important thing — how the soil handles water and air.
The terms “heavy” and “light” do not describe how much a filled bucket will weigh. They describe how difficult or easy the soil is to work. The difference lies in the size of the mineral particles. Sand has the largest grains, silt is finer, and clay is the finest of all.
Gaps form between these particles, known as soil pores. These hold water and air. Healthy soil must do both: retain water for a while after rain, but release the excess in time for vital oxygen to return to the roots.
Test your garden without a laboratory

Choose at least three different places in the area of your future lawn. Add more if the garden is large or visibly varied. Remember to test places where water collects and strips that excavators have driven over.
Take a little soil from roughly 10 centimetres deep at each location (keep the samples separate). Remove stones and small roots. Then moisten a handful of soil gradually and rub it in your hand. It should feel evenly moist. Water should not run out when you squeeze it in your palm.
Now try rolling the soil into a ball and then into a roll about as thick as an ordinary pencil. Watch what happens. Does the soil feel gritty? Does it stick? And what happens when you try to bend the roll?
- Heavy clay soil: If the material is sticky, mouldable and smooth rather than gritty, and you can bend the roll without it cracking, you have clay in your hand. This is the type of soil that readily sticks to your soles after rain, but hardens and cracks in summer. Its fine particles give clay an enormous surface area, and it holds water and nutrients very well — an advantage. Trouble starts when it becomes compacted. It loses its large pores, water stands in it, and some of the water is held so tightly by the clay that plants cannot draw it out. Wet soil therefore does not necessarily mean well-watered roots. Always check clay for compaction and drainage. The aim is to create conditions through which both water and air can pass. The conditions for amending clay soil are explained in the overview of model mixes.
- Medium loamy soil: The ball holds its shape, but the roll is harder to form and cracks when you try to bend it. The soil crumbles, feels a little gritty and a little sticky, but none of these qualities is extreme. You are fortunate: this is an ideal compromise. The mix of different particles retains water while letting the excess pass through. The rule for loamy soil is simple: preserve what works. Correct only specific shortcomings. If water infiltrates, do not buy unnecessary mountains of sand. But take care: even excellent loam can be ruined by driving machinery over it when wet. When to preserve loamy soil and when to amend it is explained in the overview of model mixes.
- Light sandy soil: You can clearly feel sharp grains between your fingers. The ball falls apart, and you cannot form a roll at all. Digging with a spade is easy, but after a warm day the soil is bone dry. Sand has very large pores. Air and water pass through it immediately, but dissolved nutrients are also carried away with the water. What we struggle to create in clay, sand has in abundance. Your task here is to help the soil retain water and nutrients. Definitely do not add more sand. How to help poor sandy soil is explained in the overview of model mixes.
This home test will point you in the right direction. If you are unsure, or are planning a major and expensive replacement of soil materials, arrange a laboratory particle-size analysis. It makes sense to do this before buying, so that you do not purchase something that will not help.
The soil inspection pit: what awaits the roots twenty centimetres lower?
After a house has been built, the surface of the plot may look inviting — dark topsoil has been neatly spread across it. Grass seed will readily germinate in it. But as soon as the roots head deeper, they meet the hardened ground below.
So take a spade and dig an inspection pit roughly 30 centimetres deep in several places. Look at its vertical wall, known as the soil profile. Examine the layer at a depth of 10 to 15 centimetres carefully, then the bottom itself. Repeat the ball feel test for every layer that looks different.

Look for three things:
- Does the type of soil change suddenly at a particular depth?
- Do you suddenly hit an extremely hard layer?
- Can you see buried rubble, old boards or other construction waste?
Tip: If plants are already growing there, look at their roots. If they flatten out along one level or turn sharply sideways, they are revealing an unseen obstruction.
It is essential to distinguish between two terms here: texture and structure. Texture describes the particles that make up the soil (our roll test). Structure describes how those particles are arranged together.
Even the best loamy soil can be compressed so tightly by an excavator that it no longer functions well. Compaction alone does not turn it into clay, but it becomes just as impermeable to water. Conversely, even clay soil with a good, natural structure can function surprisingly well.
Assess soil resistance and hardness when it is slightly moist. Dry clay will stop a spade even if no excavator has ever crossed it. Look for an abrupt change at one particular depth and flat, dense pieces of soil.
Your aim is to reach a clear conclusion. For example, you might find ten centimetres of excellent loam with a concrete-hard crust beneath it. In that case, you must physically break up the deeper layer.
Or you may find that the soil is sandy all the way down to thirty centimetres. You then need to work out how to retain moisture in it. Buying the same universal growing medium for both gardens would make no sense.
If you find a compacted layer, follow the subsoil preparation guide. Remove the obstruction to roots and water first, then choose the mix.
The infiltration test: where does water go, and why can waterlogging make grass dry out?
It may sound like a paradox, but grass desperately needs oxygen to live. Oxygen is used in cellular respiration, through which the plant gains energy below ground from sugars made in its leaves in sunlight.
If water fills the soil pores for a long time and displaces the air, the roots begin to suffocate and suffer irreversible damage. When the sun then comes out and temperatures rise, the grass starts to wilt, even though it was standing in a puddle until recently. Switching on irrigation at that point only makes the problem worse.
How can you check drainage? First, walk around the garden after genuinely heavy rain. Map the places where puddles remain and any routes by which water flows in from neighbouring land or a slope. Check the garden again the next day. One lingering puddle in a hollow is a very different problem from an evenly soaked, squelching plot.

Then carry out an infiltration test:
- Dig a pit 30 cm deep and 10 to 30 cm wide. If you have smoothed the walls with the spade while digging, roughen them slightly so that the pores are not sealed.
- Fill the pit with water and let it soak away completely. This moistens the soil naturally. (Measuring infiltration in dry, cracked soil would give an inaccurate result.) If water is still standing in the pit the next day, skip the next step — you have a serious waterlogging problem.
- If the first fill has soaked away, fill the pit again. Lay a straight batten across the rim and measure the distance from the batten to the water surface.
- Wait 15 minutes and measure how far the water level has dropped. Multiply that drop by four. (If, after 15 minutes, the level has dropped by 1 cm, the infiltration rate is 4 cm per hour.)
The result gives you a clue:
- A drop below 2.5 cm per hour: Water drains slowly. You must find out why it is being held. Is there a hollow? Water flowing in from the surroundings? Or a compacted layer below that you found when examining the profile? Break up that layer at a suitable moisture level and repeat the test. If water even flows into the pit from below, you need to address drainage across the area, including subsurface drainage. No bag of sand will fix that. The next steps are summarised in the guide to preparing the subsoil before establishing a lawn.
- A drop of 2.5 to 7.5 cm per hour: A broadly suitable result for this test. If the soil profile also functions well, preserve suitable loamy soil and address only specific shortcomings.
- A drop above 7.5 and up to 10 cm per hour, inclusive: The result is above the indicative suitable range, but is not yet in the category above 10 cm/h. Watch whether the soil retains moisture between waterings; the number alone is no reason to change its composition automatically.
- A drop above 10 cm per hour: Water escapes very quickly. If you have sandy soil, every drop will count, and you must improve its ability to retain water. A pit that empties quickly is not a victory. The conditions and amendment options are explained in the model for a poor sandy garden.
Carry out the test in several places. Sideways drainage and cracks also affect the result; it is indicative and does not by itself confirm soil fertility. If water is still standing in the pit the next day, postpone sowing.
You must shape the ground into a gentle slope away from the house (roughly 1 to 2 %, or 1–2 centimetres for every metre of length) towards a place that can receive the water. Remember that subsurface drains need somewhere to discharge. If you dig a hole in impermeable clay and fill it with gravel, you have not created a drain, only an underground bath that will soon fill up.
Assess your soil infiltration test
CalculatorFrequently asked questions about assessing soil
The feel test, inspection pit and infiltration test complement each other. Use their results to decide whether the soil needs intervention, and postpone sowing if waterlogging persists.
How can I tell whether I have clay, loam or sand?
Moisten separate samples from at least three places and try to form a ball and a roll. Clay feels smooth and sticky, and the roll bends. Loam crumbles and the roll cracks. Sand feels gritty and the ball falls apart. The soil should be moist, without water running out.
What is an infiltration test, and what is a good result?
In a pit 30 cm deep, let the first fill of water soak away. After filling it a second time, measure the drop over 15 minutes and multiply it by four. As a guide, a rate of 2.5–7.5 cm/h is suitable. Below 2.5 cm/h, look for the cause of slow drainage. Above 7.5 and up to 10 cm/h, inclusive, watch whether the soil retains moisture between waterings; the result alone does not yet mean that amendments are needed. Above 10 cm/h, water escapes very quickly and you need to check the soil’s ability to retain moisture. If water is still standing the next day, address waterlogging first.
What if water stays in the soil for a long time?
First check for compaction and how water moves into the subsoil. A new layer of soil alone will not remove an obstruction beneath it. The infiltration result is indicative; postpone sowing if waterlogging persists.
Key takeaways
Now you have a foundation to build on.
- Feeling the soil in your hand gives an initial indication of whether it is clay, loamy or sandy.
- An inspection pit reveals compacted layers and obstructions below the surface.
- An infiltration test indicates where water goes and what to check next.
In the next article
What will help your soil, and what does it not need?
The same amendment may help one garden and be unnecessary in another. Discover what sand, biochar, zeolite and Actino can do, and how to choose them.
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