C:N Ratio Calculator
Calculate C:N ratio for soil biology, decomposition rate, and nutrient cycling.
Why 25:1 Is the Threshold
Decomposer microbes have body tissue around 8:1 and use roughly two thirds of the carbon they consume for respiration rather than growth. That combination sets the balance point at approximately 25:1 in the substrate.
| Substrate C:N | Microbial nitrogen balance |
|---|---|
| < 20:1 | Mineralisation — surplus N released to soil |
| 20–30:1 | Approximately balanced |
| > 30:1 | Immobilisation — N drawn from soil |
Above roughly 30:1 there is not enough nitrogen in the residue to build microbial biomass, so decomposers take it from surrounding soil. Nitrogen immobilisation temporarily starves plants, which is why incorporating fresh sawdust or straw causes visible nitrogen deficiency in a crop.
The effect reverses as decomposition proceeds. Carbon is lost as CO2 while nitrogen is retained, so the ratio falls and immobilised nitrogen is eventually released — but the lag can span a growing season.
| Material | C:N |
|---|---|
| Urea | 0.5:1 |
| Poultry manure | 10:1 |
| Grass clippings | 20:1 |
| Finished compost | 15–20:1 |
| Fresh leaves | 20–60:1 |
| Straw | 80:1 |
| Paper | 170:1 |
| Sawdust | 400–500:1 |
Composting Practice
The target for active composting is 25–30:1, and the failure modes at each end are distinct. Too much nitrogen and excess ammonia volatilises, producing the characteristic smell and losing the nutrient. Too much carbon and the pile simply fails to heat, since microbial growth is nitrogen-limited.
A common confusion: the ratio is calculated by mass of carbon and nitrogen, not by volume of material. Bulky low-density inputs like leaves contribute far less mass than their volume suggests, so volume-based recipes systematically overestimate the carbon fraction.
Finished compost stabilises around 15–20:1, close to soil organic matter, which is why it releases nitrogen slowly rather than immobilising it.
Worked Examples
Common Mistakes
C:N is a mass ratio. Bulky materials such as leaves contribute far less mass than their volume implies, so volume-based recipes overestimate carbon.
Sawdust and straw immobilise soil nitrogen for months. Either compost first or add supplementary nitrogen alongside.
It is temporarily held in microbial biomass. As carbon is respired away the ratio falls and nitrogen is released — but the lag can exceed a growing season.
Lignin content matters as much. Woody material resists decomposition regardless of ratio, because lignin is chemically recalcitrant.