Carbon management in dryland agricultural systems.
Dryland areas cover about 41 % of the Earth’s surface and sustain over 2 billion inhabitants.
Soil carbon © in dryland areas is of crucial importance to maintain soil quality and productivity and a range of ecosystem services.
Soil mismanagement has led to a significant loss of carbon in these areas, which in many of them entailed several land degradation processes such as soil erosion, reduction in crop productivity, lower soil water holding capacity, a decline in soil biodiversity, and, ultimately, desertification, hunger and poverty in developing countries.
As a consequence, in dryland areas proper management practices and land use policies need to be implemented to increase the amount of C sequestered in the soil.
When properly managed, dryland soils have a great potential to sequester carbon if financial incentives for implementation are provided.
Dryland soils contain the largest pool of inorganic C.
However, contrasting results are found in the literature on the magnitude of inorganic C sequestration under different management regimes.
The rise of atmospheric carbon dioxide (CO2) levels will greatly affect dryland soils, since the positive effect of CO2 on crop productivity will be offset by a decrease of precipitation, thus increasing the susceptibility to soil erosion and crop failure.
In dryland agriculture, any removal of crop residues implies a loss of soil organic carbon (SOC).
Therefore, the adoption of **no-tillage practices in field crops and growing cover crops in tree crops have a great potential in dryland areas due to the associated benefits of maintaining the soil surface covered by crop residues.
Up to 80 % reduction in soil erosion has been reported when using no-tillage compared with conventional tillage.
However, no-tillage must be maintained over the long term to enhance soil macroporosity and offset the emission of nitrous oxide (N2O) associated to the greater amount of water stored in the soil when no-tillage is used.