Impacts of Irrigation (College Board AP® Environmental Science) : Study Guide

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What is salinization?

Definition of salinization

  • Salinization occurs when salts accumulate in the soil

    • This reduces soil fertility and harms plant growth

  • This happens when water evaporates from the soil, leaving behind salt deposits

  • Over time, excessive salt buildup can make soil toxic to plants

    • This can prevent crops from growing

Causes of salinization

Irrigation practices

  • Over-irrigation can cause water to seep into the soil, carrying salts that accumulate over time

  • Poor drainage systems allow water to stagnate and evaporate, leaving salt residues

  • Use of saline groundwater for irrigation increases soil salinity

High evaporation rates

  • In hot, arid regions, water evaporates quickly, leaving behind concentrated salts

    • Example: Dry climates like parts of California, Australia, and the Middle East experience high levels of salinization

Rising water tables

  • In areas with high groundwater levels, salts can rise to the surface through capillary action

  • This is common in low-lying agricultural lands where groundwater is heavily used

    • Agricultural lands at lower elevations tend to have higher groundwater levels

    • When farmers heavily use groundwater for irrigation, it can cause the water table to rise

    • As the groundwater moves upward, it brings dissolved salts to the surface through capillary action, contributing to soil salinization

Poor soil drainage

  • Clay soils and compacted land prevent proper water infiltration

    • This traps water and increases salt deposits

    • This means that agricultural fields with heavy clay content are more prone to salinization

Awaiting image: Causes of salinization
Image caption: Salinization can be caused by irrigation and a rising water table

Effects of salinization

Impact on plant growth

  • Salt stress disrupts plant metabolism, reducing water absorption and nutrient uptake

  • Symptoms include stunted growth, leaf burn, and reduced crop yields

Soil degradation

  • Loss of soil fertility: High salt levels kill beneficial soil microbes and reduce organic matter

  • Crust formation: Salt deposits can form a hard crust on the soil, making it difficult for plant roots to penetrate

Water quality issues

  • Salt runoff can enter freshwater sources, contaminating rivers, lakes, and groundwater

  • Reduces availability of clean drinking water and impacts aquatic ecosystems

    • Salt buildup in water bodies can alter pH levels and reduce oxygen availability, harming aquatic life

Preventing and managing salinization

Improved irrigation techniques

  • Drip irrigation delivers water directly to plant roots, reducing evaporation and salt buildup

  • Proper drainage systems help flush excess salts out of the soil

Soil management

  • Adding organic matter (compost, mulch) improves soil structure and increases water retention

  • Crop rotation with salt-tolerant plants helps maintain soil balance

    • Salt-tolerant plants absorb excess salts, reducing soil salinity over time

Water management

  • Using fresh, low-salinity water for irrigation prevents salt buildup

  • Flushing soil periodically with excess water can help remove accumulated salts (through leaching)

    • The water dissolves the accumulated salts and carries them downward through the soil layers, preventing salt buildup near plant roots

Examiner Tips and Tricks

In your exam, in addition to defining salinization, you may also need to explain how it happens. Make sure you are able to discuss the roles of evaporation, irrigation, and poor drainage in salt buildup.

Depletion of aquifers

What is aquifer depletion?

  • Aquifer depletion occurs when groundwater is withdrawn faster than it can be naturally replenished

  • Aquifers are underground layers of permeable rock or sediment that store and supply groundwater

  • Overuse, primarily for agriculture, industry, and urban water supply, can cause serious environmental and economic consequences

Causes of aquifer depletion

Agricultural irrigation

  • Irrigation accounts for around 70% of global freshwater use, with much of it drawn from aquifers

  • Excessive groundwater pumping for crop production, especially in dry regions, lowers water tables

    • Many farming regions rely on aquifers for year-round irrigation, even when rainfall is low

Urban and industrial water demand

  • Growing cities extract large volumes of groundwater for drinking water and industrial use

  • Unregulated pumping can deplete aquifers faster than they recharge

    • Many metropolitan areas experience groundwater shortages due to high population demands

Climate change and reduced recharge rates

  • Droughts and reduced precipitation slow the natural recharge of aquifers

  • Increased temperatures lead to higher evaporation rates, reducing available groundwater

Consequences of aquifer depletion

Land subsidence

  • Excessive groundwater withdrawal can cause land to sink (subsidence) as underground water-filled spaces collapse

    • For example, parts of California's Central Valley have experienced land sinking due to over-pumping

Reduced water availability

  • Wells and springs dry up, making it harder to access clean drinking water

  • Deeper drilling is required, increasing water costs

    • For example, farmers are forced to dig deeper wells, making groundwater extraction more expensive

Saltwater intrusion

  • In coastal areas, depleted aquifers allow saltwater to seep into freshwater supplies, contaminating drinking water

    • For example, Florida has experienced saltwater intrusion due to over-extraction of groundwater

Case Study

The Ogallala Aquifer

  • The Ogallala Aquifer (part of the High Plains Aquifer) is one of the largest freshwater aquifers in the world

  • It spans eight U.S. states: South Dakota, Nebraska, Wyoming, Colorado, Kansas, Oklahoma, New Mexico, and Texas

  • Provides water for agriculture, supporting one of the most productive farming regions in the United States

Overuse and depletion

  • Extensive irrigation for crops such as corn, wheat, and soybeans has significantly lowered the water table

  • Some areas have experienced a drop of more than 150 feet in water levels

  • Recharge rate is much lower than withdrawal, making depletion an ongoing issue

Consequences of depletion

  • Declining agricultural productivity: Less water availability reduces crop yields and threatens food security

  • Higher pumping costs: Farmers must drill deeper and use more energy to access water

  • Risk of economic decline: Farming communities dependent on groundwater face long-term sustainability issues

Potential solutions for the Ogallala Aquifer

  • More efficient irrigation methods: Transitioning to drip irrigation or soil moisture monitoring to reduce water use

  • Crop selection: Growing drought-resistant crops that require less water

  • Water conservation policies: Government regulations to manage water extraction sustainably

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