Cover Image
close this bookBetter Farming Series 28 - Water: Where Water Comes from (FAO, 1981, 31 p.)
View the document(introduction...)
View the documentPreface
close this folderWhy we study water
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View the documentRainfall
View the documentWater In the ground
View the documentThe water table
View the documentWater on the surface
View the documentEvaporation
View the documentTranspiration
View the documentThe process begins again
close this folderWhen rain falls
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View the documentHow much rain falls
View the documentKind of soil
View the documentSlope of the land
View the documentPlants
close this folderWater in the ground
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View the documentWater and the soil
View the documentWater and the subsoil
View the documentWater and parent rock
close this folderWhere to find water in the ground
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View the documentWells
View the documentSprings
close this folderWater on the surface
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View the documentGroundwater can become surface water
View the documentSurface water run- off
close this folderWhere to find surface water
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View the documentSwamps, pond and lakes
View the documentStreams and rivers

Groundwater can become surface water

87. When it rains, water sinks into the ground and mixes with the water already in the ground.

88. When there is more water in the ground, the water table becomes higher.

89. If the land is low and the water table is high enough, it may lie above the surface of the ground. Then there is more surface water.


Water lies above the surve of the ground

90. When it does not rain, there is less water in the ground and the water table becomes lower.


There is less water in the ground

91. Then there will be less surface water. This can be seen in dry times in swamps, lakes and streams.

92. The effect of groundwater on surface water is hard to see for it happens very slowly.


The effect is hard to see