INTRODUCTION TO SOIL SCIENCE
| Institution | COLLEGE |
| Course | Diploma in Agribusin... |
| Year | 1st Year |
| Semester | Unknown |
| Posted By | stephen oyake rabilo |
| File Type | |
| Pages | 31 Pages |
| File Size | 883.69 KB |
| Views | 4824 |
| Downloads | 0 |
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Description
SOIL is a naturally occurring unconsolidated material on the earth surface that has been influenced by parent material, climate, organisms and relief, all acting over a period of time to produce a soil that may differ from the material from which it was derived from in terms of physical, chemical, mineralogical, biological and morphological properties.
Soil is composed of particles of broken rock that have been altered by chemical and mechanical processes that include weathering, erosion and precipitation. Soil is altered from its parent rock due to interactions between the lithosphere, hydrosphere, atmosphere, and the biosphere
Soil therefore is a dynamic and complex media developing under the influence of external factors i.e hydrosphere (water), atmosphere (air) and biosphere (flora and fauna).
Soil science. Is the study of properties and reactions of soils and materials, its relationship with man and how it can be used in the benefit of man.
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Upon completing this topic, you should be able to factorise and solve polynomials of degree higher than 2
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Upon completing this topic you should be able to understand the binomial theorem and it’s application in the expansion of expressions and in approximations.
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282.84 KB
SMA 2104: Mathematics for Sciences - Lesson 9 TRIGONOMETRY
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Upon completing this topic, you should be able to Define, manipulate and apply trigonometric functions. Define the basic trigonometric ratios, sine, cosine and tangent of an angle and derive the other trigonometric ratios; cosecant, secant and cotangent using the basic trigonometric ratios. Derive identities involving the trigonometric ratios
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Get a copy Factorisation Practice Questions, this is suitable for your revision
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SMA 2104: Factorisation Practice Questions Answers
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