## Abstract Problems of frequent drought stress, low soil organic carbon (SOC) concentration, low aggregation, susceptibility to compaction, salinization and accelerated soil erosion in dry regions are accentuated by removal of crop residues, mechanical methods of seedbed preparation, summer clean
Carbon sequestration in dryland ecosystems of West Asia and North Africa
β Scribed by R. Lal
- Publisher
- John Wiley and Sons
- Year
- 2002
- Tongue
- English
- Weight
- 114 KB
- Volume
- 13
- Category
- Article
- ISSN
- 1085-3278
- DOI
- 10.1002/ldr.477
No coin nor oath required. For personal study only.
β¦ Synopsis
Abstract
The West AsiaβNorth Africa (WANA) region has a land area of 1.7 billionβha, and a population of 600 million. Desertification and soil degradation are severe problems in the region. The problem of drought stress is exacerbated by low and erratic rainfall and soils of limited available water holding capacity and soil organic carbon (SOC) content of less than 0.5 per cent. The SOC pool of most soils has been depleted by soil degradation and widespread use of subsistence and exploitative farming systems. The historic loss of a SOC pool for the soils of the WANA region may be 6β12βPg compared with the global loss of 66β90βPg. Assuming that 60 per cent of the historic loss can be resequestered, the total soilβC sink capacity of the WANA region may be 3β7βPg. This potential may be realized through adoption of measures to control desertification, restore degraded soils and ecosystems, and improve soil and crop management techniques that can enhance the SOC pool and improve soil quality. The strategies of soilβC sequestration include integrated nutrient management (INM) and recycling, controlled grazing, and growing improved fodder species on rangeland. Improved technologies for cropland include use of INM and biofertilizers, appropriate tillage methods and residue management techniques, crop rotations and cover crops, and water and nutrient recycling technologies. Through adoption of such measures, the potential of soilβC sequestration in the WANA region is 0.2β0.4βPgβCβyr^β1^. Copyright Β© 2002 John Wiley & Sons, Ltd.
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