Soil Resources of The Indian Sub-Continent Agriculture In India

Soil is one of the most precious resources; it is an abiotic resource that is scarce; it defines the quality of the land; it supports and manages plants; and plants offer food for animals, and people. Soil is essential for the survival of life on the planet. India is a huge nation with diverse geology, terrain, temperature, and vegetation. As a result, India has a wide range of soil types distinct from one another. Soils also provide a substrate for attenuating pollutants and surplus water, groundwater recharging, nutrient cycling, and habitat for microbes and biota, among other services.

What is Soil?

Soil is the loose surface layer that covers the surface of the earth. There are both inorganic and organic particles in it. Soil is an unconsolidated mineral or organic material on the earth’s surface that has been exposed to and exhibits the impacts of genetic and environmental variables such as climate (including water and temperature effects), macro-and microbes, and relief-conditioned parent material throughout time. leaching, weathering, and microbiological activity all combine to produce a wide range of soil types

Indian Soil Resources

•         Alluvial Soils- the largest and most significant soil category in India is alluvial soils. They sustain a variety of crops such as rice, wheat, sugarcane, etc., since they are one of India’s most significant and productive soils. However, they are lacking in nitrogen, phosphorus, and humus. They are depositional soils transported and deposited by rivers and streams. They are found in Indus, Ganga and Brahmaputra, Punjab, Haryana, Uttar Pradesh, Uttarakhand, parts of Rajasthan & Gujarat Bihar & West Bengal, east coast of India.
•         Black Soils- the black Soil gets its name from the black colouration of the basalt rock that forms under semi-arid conditions. Because it is most suited for cotton production, it is also known as ‘regur.’
•         Red Soil- the reddish tint of red Soil distinguishes it from other types of Soil. It’s also known as terra Rossa, which means “red earth” in Italian. Red dirt may be found in tropical and subtropical places when warm and humid environments. It is normally fertile and suitable for farming. The weathering of iron oxide-containing rocks produces red Soil. Basalt is the most frequent form of rock that contributes to red Soil. The weathering process breaks down the basalt into tiny fragments, subsequently broken down further into silt and clay.
•         Laterite Soil is mostly tropical-based Soil with high temperatures and considerable seasonal rainfall. Laterite comes from the Latin term ‘later,’ meaning ‘brick.’  It encourages soil drainage as a result of this. Lime and silica are always washed away by rain. Farraginous aluminous rock is believed to be found in laterite soils. Decomposition is what gives them their shape. Bacteria that flourish in high temperatures quickly deplete the Soil’s humus content. The rocks have been leached away, leaving large iron and aluminium residue. Laterite soils in India are not very productive and can only be used with manure and fertiliser.
•         Mountain soil is typically described as underdeveloped, skeletal, shallow, acidic, and infertile. They’re also very varied, and because of differences in exposure and steepness, they can vary a lot, even within small regions. In general, as elevation rises, they become less fruitful and developed.

 Significance of Soil as a Resource

Soils are necessary for life because they offer a growing substrate for plants, provide a home for many insects and other species, operate as a filtering system for surface water, store carbon, and maintain atmospheric gas levels. let’s look at each of these in more detail:

Medium For Plant Growth:

Soils aid root growth by supporting and maintaining their upright position. Soil provides essential minerals and nutrients to plants. Soils act as a channel for gas exchange between roots and the world around them. Soils protect plants from erosion and other detrimental physical, biological, and chemical processes. Soils may hold water (moisture) and provide enough aeration.

Habitat For Many Insects And Other Organisms:

Insects and microorganisms (extremely small single-celled critters) rely on soils for food and oxygen. Worms and termites are among the many organisms that live in Soil. They provide the moisture and oxygen that organic compounds require to degrade. Many animals, including insects, use them to lay and hatch eggs, while rats use them to give birth to new offspring.

Carbon Store and Maintenance of Atmospheric Gases:

Soils act as carbon sinks, allowing the quantity of carbon dioxide in the atmosphere to be controlled. Because peat soils have a high acid and water content, some organic matter decomposition does not occur completely during humification (a process in which soil organisms build complex and stable organic matter). On a worldwide scale, soils retain around twice as much carbon as the atmosphere and three times as much as plants. As a result, the Soil collects a vast quantity of carbon-rich organic matter. Nitrogen, phosphorus, and other nutrients are stored, transformed, and cycled in the Soil.

Conclusion

Because it nourishes all living things, Soil is a valuable natural resource. Unlike many natural resources that cannot be restored once exhausted, the Soil may be protected via prudent farming practices. Soil is one of the most precious resources; it is an abiotic resource that is scarce; it defines the quality of the land; it supports and manages plants; and plants offer food for plants, animals, and people.