Decomposition and its steps · Biology Class 11–12 | StemPy Lab
Course 30.2·Lesson 3 of 3
Decomposition and its steps
A dead leaf does not stay on the ground for ever. This lesson follows its breakdown through the five steps, from fragmentation to mineralisation. It shows what makes the breakdown fast or slow. Then it gives a simple model of the mass that is left.
about 30 min1 simulation1 practice question
Lesson 3 of 3Show all lessonsHide
Try the code and the simulations beside the lesson.
What happens to a fallen leaf?
In autumn a tree drops its leaves. By the next spring, most of them have disappeared. Where did the leaves go? They were decomposed. The decomposers and the detritivores broke them down, and the nutrients returned to the soil.
The raw material is detritus: dead leaves, bark, flowers, the dead remains of animals and the faecal matter. Decomposition is a long chain of small steps, and NCERT names five.
The five steps
Fragmentation. The detritivores, such as the earthworm, break the detritus into smaller particles. More surface is then open to the microbes.
Leaching. Water carries the water-soluble inorganic nutrients down into the soil. There they may be precipitated as salts that the plants cannot use.
Catabolism. The enzymes of bacteria and fungi break the detritus into simpler inorganic substances.
Humification. A dark, amorphous substance, humus, builds up. It is highly resistant to the action of microbes, and it decays at an extremely slow rate. It is colloidal, so it is a reservoir of nutrients.
Mineralisation. Some microbes break the humus down and release inorganic nutrients.
Fragmentation, leaching and catabolism go on at the same time on the detritus. Humification and mineralisation happen in the soil.
A flow diagram of decomposition. At the top is a box of detritus: dead leaves, bark, flowers, dead animals and faecal matter. Three boxes below it are drawn side by side and marked as working at the same time: fragmentation by detritivores, leaching by water, and catabolism by the enzymes of bacteria and fungi. An arrow runs down to humification, which makes humus, a dark amorphous substance resistant to microbial action that acts as a reservoir of nutrients. A last arrow runs to mineralisation, which releases inorganic nutrients.
What controls the rate?
NCERT gives two sets of factors.
The chemical composition of the detritus.
Decomposition is slower when the detritus is rich in lignin and chitin.
Decomposition is faster when the detritus is rich in nitrogen and in water-soluble substances such as sugars.
The climate. The important factors are temperature and soil moisture.
A warm and moist environment favours decomposition.
A low temperature and anaerobiosis (no oxygen) slow it down. Dead matter then builds up.
Decomposition is largely an oxygen-requiring process. This is why waterlogged soils and cold places, such as bogs, store a lot of undecayed organic matter.
A model of the litter that is left
The next part is not in the NEET syllabus, but A-Level and IB use it. A simple model says that each year the litter loses a share of what is left. Then the mass falls in a smooth, bending curve:
mt=m0e−kt
Here m0 is the starting mass, t is the time and k is the rate. A larger k means a faster decay. The half-life is the time for half of the litter to go, and it is ln2/k, which is 0.693/k.
A graph of the mass of leaf litter left, in per cent of the starting mass, against time in years from 0 to 6. Three curves fall from 100 per cent. The fastest curve, in green, is for a warm and moist place with litter that is rich in nitrogen, and it is almost at zero by year 4. A middle curve, in orange, is for a cool place, and it is near 13 per cent at year 6. The slowest curve, in red, is for a cold place with litter rich in lignin, and it is still near 47 per cent at year 6. All three curves are made with a model whose numbers are chosen for the lesson.
You should find that a warmer place and a lower lignin share both raise k, so the litter goes faster, as NCERT says.
Try it in Python
The program follows 100g of litter for six years.
The second program matches events to the five steps.
Practise with new numbers
Common mistakes
Putting the steps in a strict order. Fragmentation, leaching and catabolism go on together.
Saying that humus decays fast. It is highly resistant and decays very slowly. It stores nutrients.
Confusing leaching with catabolism. Leaching is done by water and washes soluble nutrients away. Catabolism is done by microbial enzymes.
Thinking that cold, wet soil speeds up decay. Low temperature and anaerobiosis slow it.
Remember these
Detritus: dead leaves, bark, flowers, dead animals and faecal matter.