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The Economics of Desertification, Land Degradation, and Drought

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those that affect economic plant yields, similar to those used for the 1983 assessment. Results indicate<br />

70 percent l<strong>and</strong> degradation <strong>of</strong> the assessed l<strong>and</strong>. Although estimates are considerably better than the<br />

1983 estimates, the database <strong>and</strong> information upon which calculations were made were still poor, with<br />

an upward bias.<br />

Global Assessment <strong>of</strong> Human-Induced Soil <strong>Degradation</strong> by the International Soil<br />

Reference <strong>and</strong> Information Centre (1987–1990)<br />

<strong>The</strong> Global Assessment <strong>of</strong> Human-Induced <strong>L<strong>and</strong></strong> <strong>Degradation</strong> (GLASOD) study, which was carried<br />

out by the World Soil Information Center <strong>and</strong> commissioned by the United Nations Environment<br />

Program (UNEP) between 1987 <strong>and</strong> 1995, was the first major global assessment <strong>of</strong> soil degradation.<br />

<strong>The</strong> project represented “the basis <strong>of</strong> the most recent UN studies <strong>of</strong> global l<strong>and</strong> degradation <strong>and</strong><br />

desertification” (Thomas <strong>and</strong> Middleton 1996: 119). Within three years (by 1990), GLASOD<br />

developed a world map <strong>of</strong> human-induced soil degradation (Oldeman, Hakkeling, <strong>and</strong> Sombroek<br />

1991b). <strong>The</strong> approach defines soil degradation as “human-induced phenomena, which lower the<br />

current <strong>and</strong>/or future capacity <strong>of</strong> the soil to support human life” (UNEP 1997b). <strong>The</strong> map was<br />

originally produced for the United Nations Conference on Environment <strong>and</strong> Development (UNCED)<br />

in 1992.<br />

<strong>The</strong> GLASOD project was conducted using expert opinions <strong>of</strong> about 250 experts drawn from<br />

21 regions <strong>of</strong> the world (Nachtergaele et al. 2010). Soil degradation was mapped by types <strong>and</strong> by<br />

country using the following degradation attributes: soil erosion by wind <strong>and</strong> water, chemical soil<br />

deterioration, <strong>and</strong> physical soil deterioration (for further explanation <strong>of</strong> types <strong>of</strong> degradation, see<br />

“Types <strong>of</strong> <strong>L<strong>and</strong></strong> <strong>Degradation</strong>” in Section 3). <strong>The</strong> authors then identified different degrees as light,<br />

moderate, severe, <strong>and</strong> very severe l<strong>and</strong> degradation (Oldeman, Hakkeling, <strong>and</strong> Sombroek 1991a). <strong>The</strong><br />

study observed that 38 percent <strong>of</strong> the global l<strong>and</strong> area affected by human-induced l<strong>and</strong> degradation<br />

was lightly degraded, 46 percent was moderately degraded <strong>and</strong> 15 percent was strongly degraded<br />

Oldeman 1998). Water erosion was identified as the most important form <strong>of</strong> soil degradation,<br />

followed by wind erosion, both <strong>of</strong> which accounted for about 84 percent <strong>of</strong> l<strong>and</strong> area degraded (Table<br />

2.1 <strong>and</strong> Figure 2.1). <strong>The</strong> most degraded area was Europe (25 percent), followed by Asia (18 percent)<br />

<strong>and</strong> Africa (16 percent); North America reported the smallest area degraded.<br />

Table 2.1—GLASOD (1991) extent <strong>of</strong> human-induced soil degradation (in million hectares)<br />

Type <strong>of</strong> l<strong>and</strong><br />

degradation World Asia<br />

West<br />

Asia Africa<br />

Latin<br />

American<br />

Countries<br />

13<br />

North<br />

America<br />

Australia<br />

<strong>and</strong><br />

Pacific Europe<br />

% <strong>of</strong><br />

total<br />

Water erosion 1,094 440 84 227 169 60 83 115 55.70<br />

Wind erosion<br />

Nutrient<br />

548 222 145 187 47 35 16 42 27.90<br />

depletion 135 15 6 45 72 - + 3 6.87<br />

Salinity 76 53 47 15 4 - 1 4 3.87<br />

Contamination 22 2 + + + - - 19 1.12<br />

Physical 79 12 4 18 13 1 2 36 4.02<br />

Other 10 3 1 2 1 - 1 2 0.51<br />

Total 1,964 747<br />

38.0<br />

287 494 306 96 103 218 100.00<br />

% <strong>of</strong> total<br />

3 14.61 25.15 15.58 4.89 5.24 11.10<br />

Source: Oldeman, Hakkeling, <strong>and</strong> Sombroek 1991a.<br />

Notes: + means increasing l<strong>and</strong> degradation; - means decreasing l<strong>and</strong> degradation.<br />

<strong>The</strong> GLASOD study was useful in formulating a number <strong>of</strong> global conventions <strong>and</strong><br />

international <strong>and</strong> national l<strong>and</strong> management development programs. GLASOD has also been quite<br />

useful in raising the attention <strong>of</strong> the extent <strong>and</strong> severity <strong>of</strong> soil degradation.

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