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Water Cycle
• Sources of water can be classified as surface
water and ground water.
• Oceans, rivers, lakes and backwaters are the
sources of fresh water. The water level in
these are very shallow.
• Wells, ponds, tube wells. etc are the sources
of ground water.
• Rain drops percolate into tiny pore spaces of
the soil and get collected there. There are
numerous pore spaces into the soil.
• Porosity is the term for the porous material.
Clay is an example for porous materials.
• Under normal conditions these pores will be
filled with air. These pores will be filled with
water when rain occurs.
• Some rocks are also porous. Such rocks can
absorb more water.
• But water will be available only at places where
the pores in the rocks are inter-connected. This
is due to the fact that water can move through
these pores. These quality of rocks is known as
permeability.
• All porous materials need no have permeability.
For example, clay has high porosity but low
permeability. This means that it will not permit
water to pass through. these why paddy fields
have water.
• Nature has arrangements to store rain water for
rainless periods.
• Water scarcity will be the result if we disrupt the
chances of water to percolate into ground.
• The soil moisture increases with depth.
• Water filled in these pores of the rock fills up the
pit through percolation.
• The abundance of water is because of the fact
that all the pores in this zone is filled with water.
• The surface of the water-rich part beneath the
ground is known as water table.
• The water stored beneath the ground is the
Underground water

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Water below the ground

  • 2. • Sources of water can be classified as surface water and ground water. • Oceans, rivers, lakes and backwaters are the sources of fresh water. The water level in these are very shallow. • Wells, ponds, tube wells. etc are the sources of ground water.
  • 3. • Rain drops percolate into tiny pore spaces of the soil and get collected there. There are numerous pore spaces into the soil. • Porosity is the term for the porous material. Clay is an example for porous materials. • Under normal conditions these pores will be filled with air. These pores will be filled with water when rain occurs. • Some rocks are also porous. Such rocks can absorb more water.
  • 4. • But water will be available only at places where the pores in the rocks are inter-connected. This is due to the fact that water can move through these pores. These quality of rocks is known as permeability. • All porous materials need no have permeability. For example, clay has high porosity but low permeability. This means that it will not permit water to pass through. these why paddy fields have water. • Nature has arrangements to store rain water for rainless periods. • Water scarcity will be the result if we disrupt the chances of water to percolate into ground.
  • 5.
  • 6. • The soil moisture increases with depth. • Water filled in these pores of the rock fills up the pit through percolation. • The abundance of water is because of the fact that all the pores in this zone is filled with water. • The surface of the water-rich part beneath the ground is known as water table. • The water stored beneath the ground is the Underground water