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About Lecture Note - Tropical Residual Soils Rev 1
This document provides an overview of tropical residual soils. It discusses how tropical soils are formed primarily through in situ weathering processes, making them residual soils. The high temperatures and rainfall in tropical regions lead to stronger chemical weathering that can penetrate deeper than in other climates. Weathering starts on rock joints and propagates inward and in the direction of jointing. Most soil mechanics concepts were developed from studying sedimentary soils, but residual soils behave differently since they are not depositional. The degree of weathering is an important factor, and a six-grade classification scheme is presented. The development of tropical soils is controlled by weathering processes, parent rock type, climate, relief, drainage, and cementation.
Detailed Information
| Author: | ['Mikiyas Mohammed'] |
|---|---|
| Publication Year: | 2024 |
| Pages: | 73 |
| Language: | English |
| Format: | |
| Price: | FREE |
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