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TOPIC: SOIL FORMATION AND PROFILE DEVELOPMENT.
CONTENT:
Introduction: soil is very important factor for agricultural activity and survival of man. Soil is the loose weathered materials covering the surface of the earth, which supports life. It can also be defined as the outer most part of the earth that is formed from mixture of minerals and decaying organic matter which extends from the surface down to the limit of biological forces.
Sub topic 1:
Factors of soil formation:
The transformation of rocks into soil is referred to as soil formation. The first stage in the process of soil formation is the Weathering Of Rocks which involves the breaking of rocks into smaller particles and eventually into individual minerals that the rock is composed of. Weathering of rock can either be Physical such as through water, wind, Pressure, ice and temperature, or Chemical which involves changes in the chemical composition of the rock. There are a number of factors that influence the rate, type and quality of soil formed in a location.
FACTORS OF SOIL FORMATION:
There are five factors that determine or influence soil formation, namely:
Parent material: The type of materials, that is structure, texture, and mineral composition present in the parent rock will also determine the type of soil formed Parent materials are important in the following ways:
Climate:- This the average weather condition of a place over a long period of time.
Climatic factors include the following:
Rainfall: Helps in the dissolution of chemicals from the parent materials and also in transporting broken down materials.it determine the types of soil to be formed
Temperature: Effect of temperature leads to expansion and contraction of rocks. Rock mineral with low expansively will break away to form soil. Also rock holes may retain water which freezes up at night and melts during the day, leading to disintegration of rocks and eventually soil formation.
Wind: wind can carry materials which collide with rock surfaces leading to breaking of rocks into tiny particles.
Relative humidity: This can supply moisture thereby encouraging the breaking of rocks particles into soil.
Pressure: This can lead to the breaking of large rock particles into tiny soil particles.
High pressure on a rock may cause such rock to fall down and break into tiny pieces, resulting in the formation of soil.
TOPOGRAPHY:
Relief or topography refers to the surface features of the earth crust such as hills, valleys or flat land. It may also mean the shape of the land in relation to the underlying rocks of the
earth surface. The effect may include the following:
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