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World’s Soil Resources

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3 - Sustainable land management mapping.<br />

In each unit of the national map, the prevailing land management practices were inventoried using a<br />

standard methodology (Liniger et al., 2011). This allowed the characterization of practices in terms of type of<br />

intervention (agronomic, vegetative etc) and in terms of objectives (prevention, mitigation or rehabilitation).<br />

At the same time, the extent, trend and efficiency of the conservation practices were assessed. Examples of<br />

outputs are given for the main conservation types used in the country (Figure 13.8.) and for the impact of soil<br />

degradation on ecosystem goods and services (Figure 13.9.).<br />

13.6 | Conclusions<br />

Although there is a wealth of local and national studies on soil change in the region, a systematic and<br />

standardized approach is lacking. Results on the extent and intensity of soil change processes still refer to the<br />

GLASOD study carried out in the late 1980s.<br />

The degradation of natural resources in arable lands is considered as one of the main threats to agricultural<br />

production in all countries of the region. Ecosystem service quality and capacity is greatly reduced by degradation<br />

caused by salinity, erosion, contamination and poor management that leads to a loss of soil organic matter.<br />

Water erosion is predominant in that part of the region which has sloping lands. Where rainfed agriculture<br />

is practiced, water erosion may even occur in gently sloping areas. Wind erosion is also a causative factor of<br />

topsoil removal. Population increase has resulted in soil disturbance due to uncontrolled human activities<br />

such as mining and open quarries that have triggered and accelerated erosion processes. Degradation due to<br />

salinity and sodicity varies geographically with climate, agricultural activities, irrigation methods and land<br />

management policies and is mainly restricted to irrigated farming systems. Causative factors are of intrinsic<br />

origin, seawater intrusion or irrigation from groundwater with elevated salt content. Degradation due to<br />

contamination is mainly found in countries with high population, high oil production or heavy mining. In<br />

irrigated farming systems with overuse of chemicals, the load of toxic elements in groundwater is increased.<br />

Salinity has greatly reduced crop yields and increased economic annual losses across the region to nearly<br />

US$1 billion, equivalent to as much as US$1 604 ha -1 to US$2 748 ha -1 . In some countries the reduction in soil<br />

productivity was estimated to be in the range of 30-35 percent of the potential productivity.<br />

Responses to degradation caused by erosion include improving soil resilience by increasing C inputs. This can<br />

be achieved using organic manures, compost and synthetic soil conditioners and soil conservation measures<br />

on sloping lands. Policies and regulation and socio-economic factors at individual country level were found<br />

to help reverse land degradation due to erosion. Ways of reclaiming salt-affected soils include: salt leaching<br />

and drainage interventions, crop-based management, chemical and organic amendments, fertilizers, salt<br />

tolerant plants, crop management and phytoremediation. Measures to contain degradation caused by oil<br />

contamination include farming techniques that partly eliminate hydrocarbons through decomposition,<br />

and bio-remediation using some grass species. With effective desertification control, the potential annual<br />

C sequestration rate could reach values between 0.2 to 0.4 Pg C yr -1 , compared to the 1.0 Pg C yr -1 in drylands<br />

worldwide. Ranking of soil threats is given in Table 13.3.<br />

Status of the <strong>World’s</strong> <strong>Soil</strong> <strong>Resources</strong> | Main Report Regional Assessment of <strong>Soil</strong> Changes<br />

430<br />

in the Near East and North Africa

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