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Fig.: Soil Atlas 2015
Heinrich Boll Foundation
HUMUS & SOIL LIFE
THE INVISIBLE ECOSYSTEM
At least centuries, rather millennia and millions of years pass before what we call soil develops.
The near-surface soil layer with the mostly dark, brown-black color - the humus - is teeming with life. In addition to earthworms, woodlice, spiders, mites and springtails, there are more microorganisms (such as bacteria, fungi or amoebas) in a handful of soil than there are people on earth. These creatures decompose dead plant parts, convert them into humus and distribute this fertile substance in the soil. At around 1,500 billion tons, humus binds almost three times more carbon than the entire living biomass, i.e. all living things including trees, shrubs and grasses together
The "Green Revolution" began as early as the 1960s. Intensive land use with high-yielding varieties, the use of fertilizers and pesticides , and artificial irrigation increased the yield per area in the short term. But through the use of these 'modern' techniques, 45% of Europe's soils have lost a significant amount of organic matter, particularly humus and soil organisms. With decreasing humus content, the natural fertility of the fields decreases, which cannot be compensated for by any fertilization. T he soil structure decays to lifeless substrate. In addition, the use of heavy agricultural machinery compacts the soil, disrupting its natural functions:
the habitat function (species diversity, biodiversity),
the regulatory function (water intake, storage, purification, decomposition of pesticides) as well as
the production function (nutrient exchange, natural fertility).
Irrespective of this, the consumption of mineral fertilizers has increased more than fivefold over the past 50 years due to land use driven by purely economic interests, although mineral fertilizers are expensive and devour high agricultural subsidies.