Karbonbinding i jord og innvirkning på klimaendringer og matsikkerhet

| Type artikkel: Publisert studie
Frekvensen av organisk karbonbinding i jord med bruk av anbefalte teknologier avhenger jordtekstur og struktur, nedbørsmengder, temperatur, dyrkingssystem og forvaltning av matjord.

Forfatter:

R. Lal

Publiseringssted:

Science 11 June 2004: Vol. 304 no. 5677 pp. 1623-1627

Årstall:

2004

The carbon sink capacity of the world’s agricultural and degraded soils is 50 to 66% of the historic carbon loss of 42 to 78 gigatons of carbon. The rate of soil organic carbon sequestration with adoption of recommended technologies depends on soil texture and structure, rainfall, temperature, farming system, and soil management.

Strategies to increase the soil carbon pool include soil restoration and woodland regeneration, no-till farming, cover crops, nutrient management, manuring and sludge application, improved grazing, water conservation and harvesting, efficient irrigation, agroforestry practices, and growing energy crops on spare lands. An increase of 1 ton of soil carbon pool of degraded cropland soils may increase crop yield by 20 to 40 kilograms per hectare (kg/ha) for wheat, 10 to 20 kg/ha for maize, and 0.5 to 1 kg/ha for cowpeas.

As well as enhancing food security, carbon sequestration has the potential to offset fossilfuel emissions by 0.4 to 1.2 gigatons of carbon per year, or 5 to 15% of the global fossil-fuel emissions.

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