UPSC MainsGEOGRAPHY-PAPER-II202210 Marks
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Q3.

The process of desertification leads to soil desiccation and soil loss. Explain.

How to Approach

This question requires a detailed explanation of the processes of soil desiccation and soil loss as consequences of desertification. The answer should define desertification, explain the mechanisms leading to soil desiccation (drying) and loss, and discuss the interconnectedness of these processes. Structure the answer by first defining desertification, then detailing soil desiccation, followed by soil loss, and finally linking the two. Include examples and relevant data to strengthen the response.

Model Answer

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Introduction

Desertification, a globally pressing environmental issue, refers to the degradation of land in arid, semi-arid, and dry sub-humid areas, caused primarily by human activities and climatic variations. It’s not simply the advance of deserts, but a complex process resulting in the loss of biological and economic productivity. According to the United Nations Convention to Combat Desertification (UNCCD), approximately 40% of the planet’s land is degraded, directly affecting half the world’s population. This degradation manifests prominently through soil desiccation – the excessive drying of soil – and subsequent soil loss, impacting agricultural productivity, biodiversity, and livelihoods.

Understanding Desertification and its Drivers

Desertification is driven by a combination of factors, including climate change (leading to increased temperatures and altered precipitation patterns), unsustainable agricultural practices (overgrazing, deforestation, intensive farming), and poor water management. These factors create a vicious cycle of land degradation, where the land’s ability to support life diminishes over time.

Soil Desiccation: The Drying Process

Soil desiccation is a critical component of desertification. It refers to the significant reduction in soil moisture content, leading to a dry and brittle soil structure. Several mechanisms contribute to this:

  • Reduced Precipitation: Decreased rainfall, a direct consequence of climate change and altered weather patterns, is a primary driver of soil desiccation.
  • Increased Evaporation: Higher temperatures, also linked to climate change, accelerate the rate of evaporation from the soil surface, further reducing moisture levels.
  • Loss of Vegetation Cover: Deforestation and overgrazing remove the protective layer of vegetation, exposing the soil directly to sunlight and wind, increasing evaporation and reducing infiltration.
  • Improper Irrigation Practices: In arid and semi-arid regions, inefficient irrigation techniques can lead to salinization (salt buildup) in the soil, hindering water absorption by plants and exacerbating desiccation.
  • Changes in Soil Organic Matter: Reduced vegetation cover and unsustainable agricultural practices lead to a decline in soil organic matter, which acts like a sponge, holding water in the soil.

Soil Loss: Erosion and Degradation

Soil desiccation significantly increases the vulnerability of soil to erosion and loss. Once the soil is dry and lacks the binding properties of moisture and organic matter, it becomes easily detached and transported by wind and water. The key processes involved are:

  • Wind Erosion: Dry, loose soil particles are readily lifted and carried away by wind, particularly in areas with sparse vegetation cover. This is prevalent in regions like the Sahel in Africa.
  • Water Erosion: Although seemingly counterintuitive in arid regions, infrequent but intense rainfall events can cause significant water erosion on desiccated soils. The lack of vegetation cover means there is little to intercept rainfall and slow down runoff.
  • Sheet Erosion: The removal of a uniform layer of soil.
  • Gully Erosion: The formation of larger channels due to concentrated water flow.
  • Loss of Topsoil: The most fertile layer of soil, rich in organic matter and nutrients, is often the first to be lost, severely impacting agricultural productivity.

The Interlinkage: Desiccation Leading to Loss

Soil desiccation and soil loss are not independent processes; they are intrinsically linked in a feedback loop. Desiccation weakens the soil structure, making it more susceptible to erosion. Soil loss, in turn, further reduces the soil’s capacity to retain moisture, exacerbating desiccation. This cycle continues until the land becomes unproductive and potentially transforms into a desert-like environment.

Impacts of Soil Loss:

Impact Area Consequences
Agriculture Reduced crop yields, food insecurity, increased reliance on fertilizers.
Biodiversity Habitat loss, species extinction, disruption of ecosystems.
Water Resources Reduced water infiltration, increased runoff, sedimentation of rivers and reservoirs.
Socio-economic Poverty, migration, social unrest.

Conclusion

Desertification, manifested through soil desiccation and subsequent soil loss, represents a significant threat to global environmental sustainability and human well-being. Addressing this challenge requires a multi-faceted approach encompassing sustainable land management practices, climate change mitigation, improved water resource management, and community participation. Investing in land restoration, promoting agroforestry, and implementing policies that incentivize sustainable agriculture are crucial steps towards reversing desertification and ensuring food security for future generations. A holistic and integrated approach is essential to break the cycle of degradation and restore the productivity of vulnerable lands.

Answer Length

This is a comprehensive model answer for learning purposes and may exceed the word limit. In the exam, always adhere to the prescribed word count.

Additional Resources

Key Definitions

Salinization
The process by which water-soluble salts accumulate in the soil, hindering plant growth and reducing agricultural productivity. Often caused by improper irrigation practices in arid and semi-arid regions.
Infiltration Capacity
The maximum rate at which soil can absorb water. Reduced infiltration capacity, often due to soil compaction or loss of organic matter, contributes to increased runoff and erosion.

Key Statistics

Approximately 12 million hectares of productive land become barren every year due to desertification and drought globally.

Source: UNCCD (as of 2023 knowledge cutoff)

India has approximately 29.32% of its total geographical area undergoing land degradation (as per the Desertification and Land Degradation Atlas of India, 2021).

Source: Desertification and Land Degradation Atlas of India, 2021

Examples

The Aral Sea Disaster

The shrinking of the Aral Sea in Central Asia is a stark example of desertification caused by unsustainable water management practices. Diversion of water from the Amu Darya and Syr Darya rivers for irrigation led to a dramatic decline in the sea’s water level, exposing vast areas of salt flats and causing widespread ecological and socio-economic damage.

Frequently Asked Questions

Can desertification be reversed?

Yes, desertification can be reversed through land restoration techniques such as afforestation, reforestation, soil conservation practices (terracing, contour plowing), and sustainable water management. However, it requires long-term commitment and investment.

Topics Covered

EnvironmentGeographyLand DegradationSoil ScienceClimate Change