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Sustainable Agriculture and the Environment in the Humid Tropics (1993)
Board on Agriculture (BOA)

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Sustainable Agriculture and the Environment in the HUMID TROPICS

TABLE 1-2 Geographical Distribution of Soils of the Humid Tropics (in Millions of Hectares)a

Soil Order or Suborder

Humid Tropics Total

Humid Tropic Americab

Humid Tropic Africac

Humid Tropic Asiad

Oxisols

525

332

179

14

Ultisols

413

213

69

131

Inceptisols

       

Aquepts

120

42

55

23

Andepts

12

2

1

9

Tropepts

94

17

19

58

Subtotal

226

61

75

90

Entisols

       

Fluvents

50

6

10

34

Psamments

90

6

67

17

Lithic

72

19

14

39

Subtotal

212

31

91

90

Alfisols

53

18

20

15

Histosols

27

4

23

Spodosols

19

10

3

6

Mollisols

7

7

Vertisols

5

1

2

2

Aridisolse

2

1

1

Total

1,489

666

444

379

a Based on dominant soil in maps (scale of 1:5 million) of the Food and Agriculture Organization (FAO) of the United Nations.

b From Sanchez and Cochrane (1980) plus recent adjustments.

c From the FAO (1975) and Dudal (1980).

d From the FAO (1977, 1978). Includes 46 million ha of the humid tropics of Australia and Pacific Islands.

e Saline soils only (Salorthids).

SOURCE: National Research Council. 1982. Ecological Aspects of Developmentin the Humid Tropics. Washington, D.C.: National Academy of Sciences.

and are also found in Central America, the Amazon Basin, and humid coastal Brazil. Ultisols are usually deep, well-drained red or yellowish soils, somewhat higher in weatherable minerals than Oxisols but also acidic and low in nutrients.

Inceptisols and Entisols account for most of the remaining soils of the humid tropics (about 16 percent and 14 percent, respectively). These are younger soils, more limited in distribution, and range from highly fertile soils of alluvial and volcanic origin to very acidic and nutrient-poor sands.

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