Soil is the thin layer of broken-down rock and organic material that covers most of the Earth's land. It supports almost every plant on the planet, holds up almost every building, filters our water, and stores enormous amounts of carbon. A handful of healthy soil contains more living organisms than there are humans on Earth: bacteria, fungi, insects, worms, mites and many others. Soil takes hundreds or thousands of years to form, but it can be lost in a single bad rainstorm. Without it, life on land could not exist.
- Time to form100s to 1000s of yearsAbout 1 cm of soil per 100 years
- Main ingredients4Minerals, organic matter, water, air
- Layers (horizons)O, A, B, C, RFrom topsoil down to bedrock
- Organisms per gramApprox. 1 billionMostly bacteria
- % of soil lost each yearApprox. 1% globallyTo erosion, climate change and farming
- Best topsoil depthApprox. 30 cmWhere most plant roots live
What soil is made of
Healthy soil has four main ingredients in roughly equal amounts.
- Minerals (approx. 45%): tiny bits of broken-down rock, sand, silt and clay.
- Organic matter (approx. 5%): rotting plant and animal remains, plus living organisms.
- Water (approx. 25%): held in the spaces between the bits of mineral.
- Air (approx. 25%): also in those spaces.
The layers of soil
If you dig down through soil, you find several distinct layers called horizons.
- O horizon (top): dead leaves, twigs and other organic matter, sometimes called the litter layer.
- A horizon (topsoil): dark and rich with nutrients. Where most plant roots live and most farming happens.
- B horizon (subsoil): lighter, with fewer roots and less life. Often has minerals washed down from above.
- C horizon: broken-down parent rock, partly weathered.
- R horizon (bedrock): solid unweathered rock.
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