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L3 : Soil Horizon - Soil, Science, Class 7 Video Lecture

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FAQs on L3 : Soil Horizon - Soil, Science, Class 7 Video Lecture

1. What is a soil horizon?
Ans. A soil horizon refers to a distinct layer within the soil profile that has unique characteristics and properties. It is formed over time due to various processes such as weathering, deposition, and organic matter accumulation.
2. How many soil horizons are there?
Ans. There are generally four main soil horizons, namely O horizon, A horizon, B horizon, and C horizon. Each horizon has different properties and composition that contribute to the overall soil profile.
3. What is the role of the O horizon in soil?
Ans. The O horizon, also known as the organic horizon, is the topmost layer of soil. It consists of decomposed organic matter such as leaf litter, humus, and other organic debris. This horizon plays a vital role in nutrient cycling, water retention, and supporting plant growth.
4. How does the composition of soil horizons change with depth?
Ans. The composition of soil horizons changes with depth due to various factors such as weathering, leaching, and accumulation of organic matter. The upper horizons (such as O and A) are typically richer in organic matter and nutrients, while the lower horizons (such as B and C) may contain more minerals and have different physical properties.
5. What factors influence the formation of soil horizons?
Ans. The formation of soil horizons is influenced by several factors, including climate, parent material, topography, time, and organisms. These factors determine the rate of weathering, leaching, deposition, and organic matter accumulation, which ultimately shape the characteristics of each soil horizon.
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