What is soil?
Soil is a mix of organic matter, minerals, water, air and organisms. It holds nutrients and water that plants use to grow, and also holds carbon.
Soil is structured in layers called horizons – the organic layer, topsoil, subsoil and parent material – which sit on top of a mass of unweathered rock called the bedrock. Most soil wildlife lives within the first five centimetres of the soil, which is rich in dead and decaying leaves and other organic matter.
Together, these horizons make up the soil profile, which tells the story of how the soil was formed. Not all soils were created equal, even in woodlands, with two main soil profiles affected by different flora, fauna and geology.
Soil in broadleaf woodland
The upper layers of soils in a broadleaf wood are mainly made up of the previous autumn’s dead leaves and twigs, along with other material that landed there. A few millimetres down you’ll find the fragmented organic remains from previous years, mixed up with old faecal remains from soil invertebrates, such as earthworms, that chew up leaf litter.
Soil in pine woodland
Pinewood soils, on the other hand, are very different. Since conifer trees tend not to drop their needles each year, the underlying soils lack organic matter. In addition, the soils that conifer trees thrive in tend to be much more acidic, which makes them hostile environments for most earthworms. This lack of worms means there isn’t anything to process the decaying matter in the soil, meaning it simply lies there and is broken down very slowly by fungi and soil arthropods.
There can be a layer of decaying pine needles around 10–20cm thick in pinewood soils, and it tends to heave with vast numbers of tiny animals, mainly mites and springtails.