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Why Rainfall is imprtant factor in active soil formation
Of the various climatic elements that take part in active soil formation, rainfall or precipitation is the most important factor. It supplies water whose movement through the parent material controls the nature of the soil body to a very large extent. As it percolates and moves from one part of the parent material to another, it carries with it substances in solution as well as in suspension. The substances so carried are either redeposited in another part of the parent material when the movement of water stops or leached out and completely removed from the soil body. The movement may take place downward, upward or even lateral. As a result of this, one part of soil body is deprived of some constituents and other enriched.
Explain Interferon Interferon interferes with viruses (hence the name) and is produced by most cells in the body. Interferons, like antibodies and complements, are proteins, an
data structures used by operating system for file management
Examining sand with a magnifying glass Study a small amount of sand with a magnifying glass or under the low power of a microscope if there is single available. The nearly colo
Stereo isomerism:- Stereo isomerism occurs when the same compound due to different spatial arrangement of the groups attached to its asymmetric carbon atom exists in m
Trans power : 20dBm Channel loss = 60dB We know that Received power (dBm) = Tx Power (dBm) + Tx Antenna Gain (dBi) + Rx Antenna Gain (dBi) - loss (db) as Tx and Rx antenna gains ar
Explain Glucagon Glucagon is secreted by a-cells of Islets of Langerhans. It is a hormone containing 29 amino acids. Its effects are opposite to that of insulin.
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The Asteroid Belt-Rubble of the Solar System: There is a gap of 547 million kilometers, between the orbits of Mars and Jupiter. In this gap are thousands of bodies made of ro
how is there a chemical change
1. Apply the k-means clustering to the following points in R4: (4:1, 3:6, 4:8, 5:5) (7:4, 3:0, 3:2, 6:1) (3:7, 4:9, 6:5, 6:1) (5:1, 5:6, 4:3, 5:4) (3:3, 4:0, 4:3, 5:
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