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