Ground Water Overview (2024)

Table of Contents
AQUIFERS WATER QUALITY FAQs

Approximately 3 million residents are served by public water systems that use groundwater, and more than 2.9 million Michigan residents draw groundwater through a private well.

AQUIFERS

Groundwater is stored in aquifers, which are spaces below ground in which water is trapped within layers of sand and gravel. The water stored in aquifers originates as rain and snowmelt that flows downward from the surface through the different layers of soil. This movement acts as a natural filtration system and removes many of the harmful particles accumulated from the surface. Water flows until it reaches bedrock, there, the water fills the open spaces between the sediment grain, saturating the soil and acting as storage for the fresh, filtered water.

The depth and availability of groundwater depends heavily on type of soil and minerals present in the local area. Some areas may be situated on very dense rocks that trap and pressurize the groundwater creating flowing springs, or artesian aquifers. Other areas may be located on looser soil that easily allows water to pass through.

The amount of precipitation and the amount of water pumped from an aquifer has a significant impact on the groundwater levels in a given area. If a region does not receive enough precipitation or if a significant amount of water is pumped out, the groundwater may be used faster than it is recharged, or replaced. This can lead to shrinking lakes, dry riverbeds, and the need for deeper wells.

GOOD TO KNOW

Bedrock: a deposit of solid rock that is typically buried beneath the soil and other broken or unconsolidated material, often containing an underground, confined aquifer (Britannica.com)

WATER QUALITY

Usually as water passes through soil and porous rock it is naturally filtered improving its overall quality. However if manmade and naturally-occurring contaminants are present, groundwater can become contaminated.

Michigan has naturally-occurring deposits of arsenic and nitrate, which may contaminate groundwater as it passes over mineral deposits.

Synthetic chemicals may be released from a variety of sources including underground storage tanks, old gas stations, landfills, improperly handled hazardous materials, agricultural operations or lawn care chemicals.

The Michigan Department of Environmental Quality (MDEQ) has established cleanup standards for more than 300 different chemicals that affect Michigan’s land and groundwater including arsenic, nitrate, and volatile organic compounds (VOCs).

GOOD TO KNOW

Volatile Organic Compound (VOC): wide range of chemicals that make up materials such as industrial solvents, landfill leachate, and oil spills.

The Michigan Environmental Mapper provides a map of known sites of contamination.

Some contaminated sites have been carefully monitored, while others have little data to show where contamination may have spread. If a property owner knows they have contaminated groundwater that has spread under their neighbor’s property, they are required to notify the owners of the affected properties.

If one of these sites is in your area, and you utilize a private well, regular testing of your water is recommended. In some areas, local ordinances prohibit private wells to ensure the public is not exposed to potential contamination.

Ground Water Overview (2024)

FAQs

What is the overview of groundwater? ›

Ground water is the water that seeps through rocks and soil and is stored below the ground. The rocks in which ground water is stored are called aquifers. Aquifers are typically made up of gravel, sand, sandstone or limestone.

What is groundwater answers? ›

Groundwater is water that exists underground in saturated zones beneath the land surface. The upper surface of the saturated zone is called the water table.

What is ground water quizlet? ›

Ground water. water found below the surface of the Earth, usually stored in aquifers. Aquifer. an underground layer of sand, gravel, or rock that holds water.

What is groundwater and why is it important to us? ›

Groundwater, which is in aquifers below the surface of the Earth, is one of the Nation's most important natural resources. Groundwater is the source of about 37 percent of the water that county and city water departments supply to households and businesses (public supply).

What is groundwater 3 facts? ›

Today, groundwater supports 40% of irrigated crop production, sustains drinking water for more than a quarter of the world's population, and helps maintain nearly half of all freshwater ecosystems.

What are the 3 parts of groundwater? ›

The unsaturated zone, capillary fringe, water table, and saturated zone. Water beneath the land surface occurs in two principal zones, the unsaturated zone and the saturated zone.

How deep is groundwater? ›

The top of the saturated zone (called the water table) may be only a foot below the ground's surface, or it may be hundreds of feet down. The water table may be shallow or deep; and may rise or fall depending on many factors.

What makes groundwater? ›

Groundwater is a part of the natural water cycle (check out our interactive water cycle diagram). Some part of the precipitation that lands on the ground surface infiltrates into the subsurface. The part that continues downward through the soil until it reaches rock material that is saturated is groundwater recharge.

What is groundwater 2 facts? ›

1. The amount of available groundwater is 20 to 30 times larger than all U.S. lakes, streams, and rivers combined. 2. 44% of the U.S. population depends on groundwater for its drinking water supply.

What is the definition of groundwater? ›

Definition. Groundwater is fresh water located in the subsurface pore space of soil and rocks. It is also water that is flowing within aquifers below the water table.

What is the greatest use of groundwater? ›

About 70% of groundwater withdrawn globally—including in the U.S.—is used for agriculture. In some arid countries, 90% of groundwater use is for irrigation.

Which is the top layer of groundwater? ›

The upper surface of this water-filled area, or "zone of saturation", is called the water table. The saturated area beneath the water table is called an aquifer, and aquifers are huge storehouses of water.

What are the 3 main uses of groundwater? ›

Groundwater supplies drinking water for 51% of the total U.S. population and 99% of the rural population. Groundwater helps grow our food. 64% of groundwater is used for irrigation to grow crops. Groundwater is an important component in many industrial processes.

What is an example of groundwater? ›

Groundwater can be accessed through several sources. Some examples of sources of groundwater are artesian wells, man-made wells, springs, and aquifers.

How to identify ground water? ›

Sand or gravel areas in the bottom of valleys will often be home to groundwater. These layers can be covered by clay or silt, so it's prudent to check these areas thoroughly. Natural springs usually indicate groundwater is nearby. A spring that flows year-round will likely reveal a productive aquifer.

What is groundwater and how does it occur? ›

It is difficult to visualize water underground. Some people believe that ground water collects in underground lakes or flows in underground rivers. In fact, ground water is simply the subsurface water that fully saturates pores or cracks in soils and rocks.

What is groundwater and how does it form? ›

Groundwater is a part of the natural water cycle (check out our interactive water cycle diagram). Some part of the precipitation that lands on the ground surface infiltrates into the subsurface. The part that continues downward through the soil until it reaches rock material that is saturated is groundwater recharge.

What is the groundwater of the Earth? ›

Groundwater is defined as water that is found beneath the surface of the Earth in conditions of 100 percent saturation (if it is less than 100 percent saturation, then the water is considered soil moisture). Ninety-eight percent of Earth's available fresh water is groundwater.

How does groundwater work? ›

Groundwater exists and flows within the small spaces between soil particles and fractured rock. The area where water fills these spaces is called the saturated zone. The top of the saturated zone (called the water table) may be only a foot below the ground's surface, or it may be hundreds of feet down.

Top Articles
Latest Posts
Article information

Author: Ouida Strosin DO

Last Updated:

Views: 6197

Rating: 4.6 / 5 (76 voted)

Reviews: 83% of readers found this page helpful

Author information

Name: Ouida Strosin DO

Birthday: 1995-04-27

Address: Suite 927 930 Kilback Radial, Candidaville, TN 87795

Phone: +8561498978366

Job: Legacy Manufacturing Specialist

Hobby: Singing, Mountain biking, Water sports, Water sports, Taxidermy, Polo, Pet

Introduction: My name is Ouida Strosin DO, I am a precious, combative, spotless, modern, spotless, beautiful, precious person who loves writing and wants to share my knowledge and understanding with you.