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Cultivation indicators

In the last decades soil management has changed dramatically by introducing new land cultivation implements and especially the tractor. The availability of heavy powerful machinery favored deep soil plowing and high speeds in directions usually perpendicular to the contour lines. This resulted in the displacement of huge amounts of soil materials from the upper convex parts (summit, shoulder, back slope) of a hill slope to the concave parts (footslope, toeslope) and decreased significantly the production of the various crops. Such cultivation practices have greatly contributed to deterioration of soil quality for plant growth due to tillage erosion. Tillage erosion affects soil quality for long terms, by changing soil depth and consequently water holding capacity, nutrient availability, organic matter content, and crop yield. The effects of soil erosion on productivity depend largely on the thickness and quality of the topsoil and on the nature of the subsoil. Productivity of deep soils with thick topsoil and excellent subsoil properties may be virtually unaffected by erosion. However, most hilly soils are shallow or have some undesirable properties in the subsoil such as petrocalcic horizon, or bedrock that adversely affects yields. In either case, productivity will decrease as the topsoil gets thinner and undesirable subsoil is mixed into the Ap-horizon by tillage, or as water-storage capacity and effective rooting depth are decreased. Important indicators considered in this project for assessing land degradation and desertification risk are the following: (a) tillage operations, (b) tillage depth, (c) tillage direction, and (d) mechanization index (Table 8).

Table 8. Number of field sites in which indicators related to cultivation was recorded in the filled questionnaires

site no Study site Tillage operations Tillage depth Tillage direction Frequency of tillage Mechanization index
1 Nestos Basin, Maggana, Greece - - - - -
2 Mação, Portugal - - - - -
3 Gois, Portugal - - - - -
4 Djanybek, Russia 29 - - - -
5 Boteti Area, Botswana 22 10 10 0 8
6 Secano Interior, Chile 28 28 28 28 -
7 Rendina Basin, Basilicata, Italy 30 30 30 - 30
8 Novij, Saratov, Russia 84 22 22 0 -
9 Cointzio watershed, Mexico 37 37 37 36 -
10 Eskisehir, Turkey 70 70 70 0 -
11 Konya, Karapinar plain, Turkey 74 74 74 - 74
12 Santiago Island, Cape Verde 103 103 103 77 -
13 Zeuss-Koutine, Tunisia 120 120 120 69 -
14 Crete, Greece 155 155 155 0 -
15 Mamora/Sehoul, Morocco 120 120 120 120 -
16 Guadalentin Basin, Murcia, Spain 121 121 121 121 -
17 Loess Plateau, China 150 150 150 - 150
TOTAL 1143 1040 1040 451 262