Humus is the end product of the composting process. It is formed after hundreds of years, when organic matter has been fully broken down to compost, and finally to humus. It can be summed up as the 'life-force' of the soil. The humification is mostly the result of bacteria and microbes. Once humus is formed, it is gone after 2,5 years; being transformed into mineral substances. The degradation of humus occurs more quickly with sandy soils.

Physically humus can be differentiated from organic matter in that the latter is rough looking material, with coarse plant remains still visible, whilst once fully humified it become more uniform in appearance (a dark, spongy, jelly-like substance) and amorphous in structure. That is, it has no determinate shape, structure or character.

more humus: soil gets a more darker color, contains water better, more soil life

Plant remains (including those that have passed through an animal and are excreted as manure) contain organic compounds, sugars, starches, proteins, carbohydrates, lignins, waxes, resins and organic acids. The process of organic matter decay in the soil begins with the decomposition of sugars and starches from carbohydrates which break down easily as saprophytes initially invade the dead plant, while the remaining cellulose breaks down more slowly. Proteins decompose into amino acids at a rate depending on Carbon:Nitrogen ratios. Organic acids break down rapidly, whilst fats, waxes, resins and lignins remain relatively unchanged for longer periods of time. The humus that is the end product of this process is thus a synthesis of compounds and complex life chemicals of plant, animal or microbial origin which has many functions and benefits in the soil as outlined below;

  • The mineralisation process that converts raw organic matter to the relatively stable substance that is humus feeds the soil population of micro-organisms and other creatures thus maintaining high and healthy levels of soil life.
  • Effective and stable humus (see below) are further sources of nutrients to microbes, the former providing a readily available supply whilst the latter acts as a more long term storage reservoir.
  • Humification of dead plant material causes complex organic compounds to break down into simpler forms which are then made available to growing plants for uptake through their root systems.
  • Humus is a colloidal substance, and increases the soil's Cation Exchange Capacity, hence it's ability to store nutrients on clay particles, thus whilst these nutrient anions are accessible to plants they are held in the soil safe from leaching away by rain or irrigation.
  • Humus can hold the equivalent of 80-90% of it's weight in moisture, thus increases the soil's capacity to withstand drought conditions.
  • Humus has a light, fluffy texture, allowing greater aeration of the soil.
  • The biochemical structure of humus enables it to moderate- or buffer- excessive acid or alkaline soil conditions.
  • During the Humification process microbes secrete sticky gums- these contribute to the desirable crumb structure of the soil by holding particles together. Toxic substances such as heavy metals, as well as excess nutrients, can be chelated (that is, bound as a compound within a complex organic molecule) and prevented from entering the wider ecosystem.
  • The dark colour of humus (usually black or dark brown) helps to warm up cold soils in the spring.

Humification of leaf litter and formation of clay-humus complexes

Humus which is readily capable of further decomposition is referred to as effective or active humus. It is principally derived from sugars, starches and proteins and consists of simple organic (fulvic) acids. It is an excellent source of plant nutrients, but of little value regarding long term soil structure and tilth. Stable (or passive) humus consisting of humic acids, or humins, on the other hand, are so highly insoluble (or tightly bound to clay particles that they cannot be penetrated by microbes) that they are greatly resistant to further decomposition. Thus they add few readily available nutrients to the soil, but play an essential part in providing it's physical structure. Some very stable humus complexes have survived for thousands of years. Stable humus tends to originate from woodier plant materials, eg, cellulose and lignins.

Humus should not be thought of as 'dead'- rather it is the 'raw matter' of life- the transition stage between one life form and another. It is a part of a constant process of change and organic cycling, thus must be constantly replenished- for when we are removing prunings and crops for the kitchen we are depriving nature's cycle of potential humus. This is why we need to substitute compost and other sources of organic matter to maintain the fertility of our productive land.

Humus quantities in different types of soil[edit | edit source]

Quantity of carbon_X_1,72 = humus quantity in the soil

Material Carbon quantity Humus
Sand 2,3% 2,3_X_1,72=?
Sand-loam 1,4% 1,4_X_1,72=?
Loam 1,4% 1,4_X_1,72=?
Clay 2,1% 2,1_X_1,72=?

Too much humus -->generates too much nitrogen/nitrate

See also[edit | edit source]

External links[edit | edit source]

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Keywords composting, elements
Authors Eric Blazek, KVDP
License CC-BY-SA-3.0
Ported from (original)
Language English (en)
Translations Chinese, Japanese
Related 2 subpages, 26 pages link here
Impact 1,309 page views
Created April 21, 2006 by Eric Blazek
Modified October 23, 2023 by Maintenance script
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