accumulation

decomposition

nutrients

acidity

This kind of soil is basically formed by the accumulation of dead and decayed organic matter, it naturally contains much more organic matter than most of the soils. It is generally found in marshy areas. Now the decomposition of the organic matter in Peaty soil is blocked by the acidity of the soil.

This kind of soil is formed in wet climate. Though the soil is rich in organic matter, nutrients present are fewer in this soil type than any other type.

Peaty soil is prone to water logging but if the soil is fertilized well and the drainage of the soil is looked after, it can be the ideal for growing plants.