Soil profile: the organic matter content, the backbone of living soil
|
|
Time to read 5 min
|
|
Time to read 5 min
Summary
The composition of the soil tells the story of the earth's life. It reveals its layers, from the surface layer of plant debris down to the bedrock. We can read its structure, moisture, color… and above all, its organic matter (OM), this mixture of decomposing plant and animal remains and living organisms. Understanding OM means understanding the fertility, resilience, and capacity of a soil to sustainably nourish plants.
Organic matter acts everywhere at once. It stabilizes soil aggregates (improving porosity), retains water (reducing water stress), nourishes soil life (microbes, fungi, earthworms), and serves as a reservoir of nutrients released gradually (mineralization). It also plays a climatic role by storing carbon in the surface horizons. In France, the 0–30 cm layer of soils stores several billion tons of organic carbon. Soil rich in organic matter is more tolerant of extremes: heavy rainfall, drought, trampling, and repeated tilling.
It all starts with inputs: dead leaves, roots, mulch, green manure, compost, and manure. Fauna and microflora decompose these materials. Some mineralize (making nutrients available), while some transform into humus (stable organic matter) which accumulates mainly in the topsoil. For a garden, simple practices like home composting and mulching regularly replenish nutrients and organic matter.
There is no single organic matter content that is universally applicable. Climate, soil texture ( clay / silt / sand ), land use, and management history all influence what are considered "normal" levels. A robust approach is to consider soil organic carbon (SOC) and aim for at least one level that supports productivity. A global meta-analysis suggests that yields tend to increase with SOC up to approximately 2% SOC (or about 3.4% organic matter when applying the usual conversion factor). This value is not an absolute, but a useful benchmark for temperate garden and crop soils.
Here are the simple steps to monitor organic matter:
Take a soil sample (e.g., 0–30 cm).
Send to laboratory to measure the SOC (TOC) and the C/N ratio.
Observe the soil profile: color, structure (clumps), life (worms, roots).
Repeat the measurements every 2 to 3 years.
Throughout the seasons, organic matter helps the soil maintain its balance. It makes the soil more supple, retains moisture, limits nutrient loss, and prevents it from deteriorating too quickly. These effects are visible in the soil profile: the top layer is darker, more crumbly, and full of small roots or worm burrows. It is this richness that we seek to protect, as it is what keeps the soil alive and productive.
Managing heavy metals is expensive: analysis, removal, treatment. But ignoring pollution leads to far greater costs:
Legal proceedings.
Health risks for local residents.
Land devaluation of polluted land.
From a regulatory standpoint, priority is given to recovery rather than storage (Environmental Code, Article L.541-1). BRGM guides are references for determining the number of analyses, thresholds, and appropriate disposal channels.
Here are the simple steps to monitor organic matter:
Take a soil sample (e.g., 0–30 cm).
Send to laboratory to measure the SOC (TOC) and the C/N ratio.
Observe the soil profile: color, structure (clumps), life (worms, roots).
Repeat the measurements every 2 to 3 years.
Here is a table detailing the purpose of each indicator:
| Indicator | What this reveals | Suggested frequency |
|---|---|---|
| SOC / COT (lab analysis) | Size of the carbon reserve / quantity of organic carbon | Every 2–3 years |
| C/N ratio | Decomposition equilibrium | At the same time as SOC |
| observed soil profile | Structure, life, depth (color, structure, visible roots) | With each major change |
| Soil life (worms, microbes) | Soil biological vitality (insects, worms, fungi) | 1–2 times a year |
Deep plowing accelerates the loss of organic matter . It exposes humus to oxygen, causing it to disappear more quickly. In contrast, no-till or reduced-till methods better preserve surface organic matter. They promote plant cover and reduce erosion. This also helps to store more carbon.
The soil profile shows you where organic matter is concentrated. It's often denser near the surface (dark color, clumps, roots). This allows you to target improvements: avoid disturbing the surface too much, add compost in the right place, and preserve this fertile layer.
Three simple actions are very effective:
These simple practices increase organic matter in just a few years.
As a general rule, aiming for ~2% SOC (≈ 3.4% OM) gives good results for temperate soils.
C/N = %C / %N. A ratio around 10–12 indicates good decomposition and good nitrogen release for plants.
Every 2–3 years in the laboratory. In between, you can observe the soil profile with the naked eye.
Deep plowing accelerates the loss of organic matter. No-till or reduced tillage better preserves the soil.
Pouryère supports you throughout the entire soil analysis process. Our sampling kits come with a comprehensive guide to walk you through the process. Once you've completed the analysis, simply send us your samples for full analysis and interpretation, which takes approximately ten days.
Each soil analysis kit is specialized and pursues a specific purpose: