Tropical Red Soils Latosols Zonal Soils of Equatorial Regions • Occur in the continents of South America, Africa and South Asia. • They are found near the equator. • For example in Brazil. • These countries all have an equatorial climate, that is very warm and very wet. • Called Latosols. Characteristics of Latosols • • • • Low humus Heavy leaching Red colour Sometimes can have a brick like surface. • Short nutrient cycle • Can support very rich vegetation. Causes of Characteristics…. • Low humus content is due to the rapid breakdown of organic material due to the very hot and very wet climate. • Leaching is intense, only iron and aluminium compounds remain,this gives soil its red colour. • The nutrient cycle is short because there is fast plant growth and rapid decomposition. This means humus is formed and used before leaching occurs. Main Process Involved Laterisation Laterites • Loose topsoil is eroded. • Iron and aluminium layers are exposed. • The high temperatures bake this into a hard brick like surface. • This surface cannot be cultivated. • It is known as a laterite. Latosol Soil Profile Latosol Soil Profile • O Horizon; A lot of organic matter, rapid decomposition. • A Horizon; Very thin layer due to short nutrient cycle. • B Horizon; Very deep, intense leaching. • C Horizon; Parent rock. Uses of Latosol Soils • In many areas with latosol soils there are tropical rainforests. • The soil type can be an obstacle to the development of profitable agriculture. • If forest or vegetation is removed the soil can become infertile within a couple of years. Exam Questions • Compare and contrast the characteristics of any two soil types which you have studied. (80 marks) – Characteristics; Colour, Texture, Structure, Humus, PH Value, Water content, Fertility. – Also contrast the processes causing these characteristics, climate, locations and uses.