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Soil indicators

Soil is a dominant factor of the terrestrial ecosystems in the semi-arid and dry sub-humid zones, particularly through its effect on plant growth. Vegetation degradation will proceed, in a certain landscape, when the soil is not able to provide the plants with adequate rooting space for water and nutrients adsorption. One of the most important processes of desertification is soil erosion, particularly affecting hilly areas. Desertification due to soil erosion is a serious threat to the soil quality and land productivity. The effects of soil erosion on land productivity depend largely on the thickness and quality of the topsoil and on the nature of the subsoil. Any loss of soil volume from marginal lands greatly reduces the potential for biomass production, ultimately leading to desertification. In the semi-arid and the sub-humid zones, the land becomes irreversibly desertified when the rootable soil depth is not capable of sustaining a certain minimum vegetation cover. There are cases where desertification proceeds even on deep soils, when their water balance is not capable of meeting the needs of plants.

Soil quality indicators used for the purposes of the DESIRE project to define desertification risk are related to water availability, and erosion characteristics. Selection of soil quality indicators considering the multiple functions of soil in maintaining productivity and environmental well-being is a complicated issue and it requires integrating physical, chemical and biological soil attributes that define those functions. The indicators selected for this study are simple soil properties or characteristics given in regular soil survey reports, such as: drainage, soil depth, soil texture, parent material, slope gradient, slope aspect, stoniness, water storage capacity, degree of erosion, rock outcrops exposure, organic matter content in the surface horizon, and soil electrical conductivity.

Table 3. Number of field sites in which the indicators related to soils was recorded in the filled questionnaires

site no Study site Drainage Parent material Rock fragments Slope aspect Slope gradient Soil depth Soil texture Water storage capacity Rock outcrop Organic matter Degree of soil erosion Electrical conductivity
1 Mação, Portugal - - - 31 - 31 - - - - 31 -
2 Nestos Basin, Maggana, Greece 30 30 - - - 30 30 30 - - - 30
3 Rendina Basin, Basilicata, Italy - 30 30 - 30 30 30 - - 30 30 -
4 Secano Interior, Chile - 28 28 28 28 28 28 28 28 28 28 -
5 Boteti Area, Botswana 24 50 48 49 48 54 55 47 45 36 40 7
6 Eskisehir, Turkey - 70 70 70 70 70 70 70 70 70 70 -
7 Konya, Karapinar plain, Turkey 74 74 74 74 74 74 74 74 74 74 74 -
8 Loess Plateau, China - 150 150 - 150 150 150 - - 150 150 -
9 Novij, Saratov, Russia 100 122 84 84 84 122 122 122 84 22 22 38
10 Djanybek, Russia 98 138 69 69 69 138 138 138 69 40 40 69
11 Santiago Island, Cape Verde - 103 103 103 103 103 103 103 103 103 103 -
12 Mamora/Sehoul, Morocco - 120 120 120 120 120 120 120 120 120 120 -
13 Zeuss-Koutine, Tunisia - 120 120 120 120 120 120 120 120 120 120 -
14 Guadalentin Basin, Murcia, Spain - 121 121 121 121 121 121 121 121 121 121 -
15 Crete, Greece 114 269 155 155 155 269 269 269 155 155 155 114
16 Cointzio watershed, Mexico - 67 67 87 67 87 67 67 67 67 87 -
17 Gois, Portugal - - - 30 - 30 - - - - 30 -
TOTAL 440 1492 1239 1141 1239 1577 1497 1309 1056 1136 1221 258