Including rocky surfaces, deserts, and ice-covered areas, there is 130,575,894 km 2 land area in the globe. About 38.5 million km 2 (29.45 % of the earth's ice-free land surface) is too dry for human habitation, and about 20.2 million km 2 (15.46 %) of the land occurring in the cold tundra zone is not much suitable for normal agriculture. Saline and alkaline soils occur in 3,105,000 km 2 (2.4 % of the land surface), and soil acidity affects 18,420,100 km 2 (14.1 % of the total land). Only about 12 % of the land surface is suitable for food and fi ber production, 24 % is grazing land, and about 31 % is forestland; the remaining 33 % has many constraints for most uses. The lands are classifi ed into eight land capability classes based on their productivity, limitations, climate, and soil conservation requirements. Class I land is the most suitable agricultural land, and Classes VII to VIII are not suited for cultivation. Agricultural soils are again classifi ed into nine land quality classes based on the integration of three soil performance classes and three soil resilience classes. Land quality I is the prime land. Suitability of cropping and productivity gradually decrease from Class I to Class IX. The global arable land area is estimated to be 1.351 billion hectares, and 38 % of the arable land has been degraded at variable intensities. The principal cause of soil degradation is the land mismanagement. GLASOD identifi ed fi ve main causes of soil degradation, including deforestation, overgrazing, mismanagement of agricultural land, overexploitation of vegetation, and (bio-) industrial activities. There are fi ve types of land/soil degradation: water erosion, wind erosion, physical deterioration, chemical deterioration, and degradation of biological activity. With this background, ten "laws of sustainable soil management" have been suggested.