Groundwater is freshwater that is stored beneath the Earth’s surface in soil and rock.
When it rains, some water flows over the land, but much of it seeps into the ground.
This water moves through spaces, or pores, between particles in soil and rock.
Rocks that allow water to pass through easily are called permeable rocks, similar to how a sponge lets water flow through it.
Water keeps moving down through these layers until it reaches a rock that blocks its path. This is called an impermeable rock.
The water builds up above this layer, filling all the tiny spaces in the rock. This area is called the saturated zone.
The water table is at the very top of this saturated zone. It can rise after heavy rain and drop during dry weather.
Above the water table is the unsaturated zone, where rock and soil are not fully filled with water.
If the saturated rock holds a lot of water, it’s called an aquifer. An aquifer is like an underground water storage tank.
Groundwater is the water located beneath Earth's surface in soil pore spaces and in the fractures of rock formations. It plays a crucial role in the hydrologic cycle, acting as a reservoir that feeds springs, wells, and aquifers. Understanding groundwater helps us comprehend how water moves through Earth's systems and supports various ecosystems.
Scientists develop models to describe the cycling of water through Earth's systems, illustrating how groundwater interacts with surface water and the atmosphere. These models help in visualizing the movement and storage of water underground.
Activity Ideas:
Groundwater is part of a larger Earth system involving the movement and storage of water. Understanding this system helps us see how water enters, moves through, and exits underground environments. These systems are influenced by natural conditions and human activities, and changes to one part can affect the whole system.
Examples:
Recognizing groundwater as a system helps scientists and communities predict water availability, prevent contamination, and plan for sustainable use of this vital resource.
Groundwater is a hidden but powerful part of Earth’s water system. By modeling how it works and recognizing it as a system, we can see its importance in our daily lives and take steps to keep it clean and available for the future.
Groundwater is freshwater that is stored beneath the Earth’s surface in soil and rock.
When it rains, some water flows over the land, but much of it seeps into the ground.
This water moves through spaces, or pores, between particles in soil and rock.
Rocks that allow water to pass through easily are called permeable rocks, similar to how a sponge lets water flow through it.
Water keeps moving down through these layers until it reaches a rock that blocks its path. This is called an impermeable rock.
The water builds up above this layer, filling all the tiny spaces in the rock. This area is called the saturated zone.
The water table is at the very top of this saturated zone. It can rise after heavy rain and drop during dry weather.
Above the water table is the unsaturated zone, where rock and soil are not fully filled with water.
If the saturated rock holds a lot of water, it’s called an aquifer. An aquifer is like an underground water storage tank.
Groundwater is freshwater that is stored beneath the Earth’s surface in soil and rock.
When it rains, some water flows over the land, but much of it seeps into the ground.
This water moves through spaces, or pores, between particles in soil and rock.
Rocks that allow water to pass through easily are called permeable rocks, similar to how a sponge lets water flow through it.
Water keeps moving down through these layers until it reaches a rock that blocks its path. This is called an impermeable rock.
The water builds up above this layer, filling all the tiny spaces in the rock. This area is called the saturated zone.
The water table is at the very top of this saturated zone. It can rise after heavy rain and drop during dry weather.
Above the water table is the unsaturated zone, where rock and soil are not fully filled with water.
If the saturated rock holds a lot of water, it’s called an aquifer. An aquifer is like an underground water storage tank.
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