Ground water and surface waters Flashcards
The most important hydrological quantity associated with water supply is
Run-off.
Run-off describes how much water that has been raining flows on the ground and into the surface waters.
What influences the amount of run-off?
Rain and evaporation.
What is groundwater?
Groundwater refers to water that has been filled the open spaces of soil and bedrock.
'’The substance or energy shall not be treated in such a way that the quality of groundwater may become hazardous to health or otherwise materially deteriorate or become unfit for the purpose for which it could be used.’’
Groundwater areas are classified to three categories:
- Areas of groundwater for water supply. The area is defined as those used or will be used within 20 to 30 years for AT LEAST 10 household needs.
- Other groundwater areas suitable for water supply. Suitable, but no demonstrable use for them.
- The exploitation of groundwater in category 3 areas require further classification.
Groundwater formation in Finland?
Most Finland’s soils have formed of poorly water-permeable clay and morennum deposits.
So, the best groundwater reserves in Finland are located in ridges and various gravel deposits that have formed during Ice Age.
What is groundwater exploration?
A multi-stage process in which field studies provide the basis for actual test bumps and the construction of production wells, as well as generally for determining the hydrogeology of the area.
The most important for the formation and sourcing of groundwater is?
The deposits and coarsely sorted material.
Coarse-grained earth deposits have a high pore volume and good water conductivity.
Why is water supply easier in the edges?
Because the groundwater level is closer to the ground surface than in the central parts of the formations.
How is earth water zone formed?
In the earth water zone between ground surface and groundwater, water fills the soil’s pores and bedrock hair cracks only partially.
How is groundwater zone formed (last step)?
Bedrock cracks completely and filled with water. Groundwater flows toward the lowest points on the terrain and erupts in some places into the ground or water bodies by gravity or pressure.
Gravitational sinking water
Downward moving water under the influence of gravity
Capillary water
Attached to and between the earth grains by surface tension forces and is available to plants
Hygroscopic water
Electronically bound to the surface of soil particles in a thin layer.
Absorbtion of water
Formed of a layer of several water molecules adhered to the surface of earth particles by Van der Waal forces
Crystal water
Structurally bound to minerals, rich in clay minerals. (100 to 400 C heating relieves it)
Groundwater levels in Finland
Usually 1-4 meters, in ridges and bedrock depths of up to 20 meters.
Groundwater is at its highest in spring when snow has melted, lowest in late winter.
What determine the slope at which the surface water is set above the discharge levels?
The amount of groundwater formed and the water conductivity of the layers.
Variations in groundwater surfaces depends mostly on?
Precipitation and evaporation.
Atmospheric pressure.
Also abstraction, construction, drainage, tides and winds.
How can we increase the production of water in groundwater areas when it is not enough?
By absorbing additional water.
In direct artificial groundwater method, the surface water is led (by pumping) into the groundwater area.
Indirect groundwater method?
The formation of groundwater is increased by placing the water supply wells close to the surface water.