UPSC MainsGEOLOGY-PAPER-II201910 Marks
Q24.

How is ground water of coastal areas contaminated by seawater intrusion and comment on its mitigation.

How to Approach

This question requires a detailed understanding of hydrogeology, particularly concerning coastal aquifers. The answer should begin by defining seawater intrusion and explaining the geological and hydrological factors that contribute to it. It should then elaborate on the various mitigation strategies, categorizing them into engineering, hydrogeological, and management approaches. Specific examples and case studies will strengthen the response. A structured approach – defining the problem, detailing causes, and outlining solutions – is recommended.

Model Answer

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Introduction

Groundwater constitutes a vital freshwater resource, especially in coastal regions where it often serves as the primary source of water for domestic, agricultural, and industrial purposes. However, these coastal aquifers are particularly vulnerable to contamination by seawater intrusion – the movement of saline water into freshwater aquifers. This phenomenon is exacerbated by over-extraction of groundwater, climate change impacts like sea-level rise, and geological formations. The increasing salinity renders the water unsuitable for many uses, posing a significant threat to water security and ecological balance in coastal communities. Understanding the mechanisms and mitigation strategies for seawater intrusion is therefore crucial for sustainable coastal resource management.

Understanding Seawater Intrusion

Seawater intrusion occurs due to the density difference between freshwater and saltwater. Freshwater, being less dense, normally overlies saltwater in coastal aquifers. However, when freshwater extraction exceeds recharge rates, the freshwater table declines. This reduction in freshwater head allows saltwater to migrate inland, contaminating the aquifer. Several factors influence the extent of intrusion:

  • Hydraulic Conductivity: Highly permeable aquifers are more susceptible to intrusion.
  • Aquifer Thickness & Geometry: Thinner aquifers and those with unfavorable geometry (e.g., confined aquifers with leaky boundaries) are more vulnerable.
  • Recharge Rate: Insufficient recharge from rainfall or surface water sources exacerbates the problem.
  • Sea Level Rise: Rising sea levels increase the hydraulic head of saltwater, pushing it further inland.
  • Tidal Fluctuations: Tidal cycles can cause periodic intrusion, especially in unconfined aquifers.

Mechanisms of Seawater Intrusion

Seawater intrusion manifests in several ways:

  • Saltwater Wedge: In confined aquifers, a sharp interface forms between freshwater and saltwater, creating a wedge-shaped intrusion.
  • Saltwater Finger: In unconfined aquifers, saltwater infiltrates as fingers or plumes, dispersing more widely.
  • Upconing: Pumping near the coastline can cause the freshwater-saltwater interface to cone upwards, accelerating intrusion.

Mitigation Strategies

Mitigation strategies can be broadly categorized into engineering, hydrogeological, and management approaches:

Engineering Approaches

  • Subsurface Barriers: Installation of impermeable barriers (e.g., slurry walls, sheet piling) perpendicular to the coastline to block saltwater movement.
  • Injection Wells: Injecting freshwater into the aquifer to create a hydraulic barrier and push back the saltwater.
  • Desalination: Treating seawater or brackish groundwater to produce potable water. This is a costly but effective solution.

Hydrogeological Approaches

  • Artificial Recharge: Enhancing groundwater recharge through techniques like rainwater harvesting, spreading basins, and managed aquifer recharge (MAR).
  • Freshwater Lens Management: Carefully managing pumping rates to maintain a sufficient freshwater lens and prevent saltwater intrusion.
  • Aquifer Storage and Recovery (ASR): Storing excess freshwater during wet seasons for later use during dry seasons.

Management Approaches

  • Groundwater Regulation: Implementing regulations to control groundwater extraction and prevent over-pumping.
  • Land Use Planning: Restricting development in vulnerable areas and promoting sustainable land use practices.
  • Monitoring Networks: Establishing comprehensive monitoring networks to track groundwater levels, salinity, and intrusion patterns.
  • Public Awareness: Educating the public about the importance of groundwater conservation and the impacts of seawater intrusion.

Example: The state of Kerala, India, faces significant seawater intrusion issues in its coastal districts. The Kerala Water Infrastructure Investment Fund Board (KWIFB) has approved projects for artificial recharge and desalination plants to address this problem (as of 2023). Similarly, in Gujarat, the implementation of check dams and rainwater harvesting structures has shown positive results in reducing saltwater intrusion in some areas.

Mitigation Strategy Advantages Disadvantages Cost
Subsurface Barriers Effective in blocking intrusion High initial cost, potential for clogging High
Artificial Recharge Sustainable, cost-effective Requires suitable recharge sites, potential for clogging Moderate
Desalination Provides a reliable water supply High energy consumption, brine disposal issues Very High

Conclusion

Seawater intrusion is a complex environmental challenge that demands a holistic and integrated approach. Effective mitigation requires a combination of engineering solutions, hydrogeological interventions, and robust management strategies. Prioritizing sustainable groundwater management practices, investing in artificial recharge infrastructure, and promoting public awareness are crucial steps towards safeguarding coastal freshwater resources. Furthermore, considering the impacts of climate change, particularly sea-level rise, is essential for long-term planning and adaptation in vulnerable coastal regions.

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

Salinity
The measure of dissolved salts in a body of water, typically expressed in parts per thousand (ppt) or practical salinity units (PSU).
Hydraulic Head
The total energy of water per unit weight, usually expressed as the elevation to which water will rise in a piezometer. It is a key factor determining the direction of groundwater flow.

Key Statistics

Approximately 20% of the world’s population relies on groundwater for drinking water, and a significant portion of this population lives in coastal areas vulnerable to seawater intrusion.

Source: UNESCO World Water Assessment Programme (WWAP), 2023 (Knowledge Cutoff)

Studies indicate that over 50% of the world’s large coastal cities are experiencing seawater intrusion to some degree.

Source: Custodio, E. (2010). Salinization of groundwater in coastal aquifers. Hydrogeology Journal, 18(3), 533-546.

Examples

The Nile Delta, Egypt

The Nile Delta is severely affected by seawater intrusion due to excessive groundwater pumping for agriculture and urbanization. This has led to reduced agricultural productivity and water quality issues.

Frequently Asked Questions

What is the role of climate change in exacerbating seawater intrusion?

Climate change contributes to seawater intrusion through sea-level rise, increased frequency and intensity of storms, and altered precipitation patterns, all of which can lower freshwater tables and increase saltwater intrusion.

Topics Covered

GeologyHydrogeologyEnvironmental GeologyGroundwater ResourcesCoastal ManagementWater Quality