Water Resources Flashcards
The ease with which fluids pass through a rock is determined by the rock’s
Permeability
Which of the following would probably have the highest porosity?
Sandstone
Most of the water in the hydrosphere is found in
The oceans
The vadose zone is also known as the
Unsaturated Zone
The water table
Is the top of the zone of saturation
When the groundwater leaves the aquifer via escaping the surface in a spring or flowing into a stream it results in
Discharge
To be useful as a source of water, a rock must be
Both porous and permeable
Artesian conditions require
A confined aquifer
If the water were unconfined, the height to which the water’s pressure would raise the surface is called as the _______ surface
Potentiometric
Groundwater flow is best explained by
Darcy’s Law
Hard water is
Water containing high levels of dissolved calcium and magnesium
Limitations on the use of surface water as a water source include
All choices correct- Look up
The largest reservoir of unfrozen freshwater is
Groundwater
Around an actively pumped well in an unconfined aquifer, a ____________ may develop in the water table
Cone of Depression
Possible consequences of excessive groundwater withdrawal include
Surface Subsidence
Recharge of groundwater
Varies according to the geology and climate of the region and so groundwater may have been underground a few years (Karst regions) to 10,000 years or more (southwestern USA).
Most of the water consumed in the United States is consumed by
Agricultural Activities
A problem associated with aquifers in coastal regions is
Saltwater Intrusion
The quality of water can be measured using which of the following ways:
All- look up
Along its length, the Colorado River
Is greatly reduced in volume by heavy use and evaporation loss from reservoirs
What is groundwater?
Typically not “underground lakes and streams” but occurs in tiny pore spaces. In sediment or sedimentary rocks, adjacent grains do not fit together, so there is PORE SPACE between the grains where groundwater can be stored. All types of rocks have FRACTURES that provide openings in which groundwater can accumulate. If the fractures are connected, the water can flow. Some rocks (like limestone) get eroded by water, forming CAVES that can be filled with water.
What controls how water flows through rocks?
- Porosity
- Permeability
- Hydraulic Conductivity
Porosity
Volume percentage of rock that consists of voids or openings. Porosity is a measure of the rock’s ability to hold water. It is the proportion of the volume of rock that is open space. PRIMARY is during rock formation and SECONDARY is after rock forms (joints, dissolution, fractures)
Permeability
Capacity of a rock to transmit fluid through pore space and fractures. Rocks that allow water to flow easily are referred to as permeable, while those that do NOT are referred to as impermeable. It really is the ability of a fluid to move through a rock or sediment… proportional to the void spaces, conduits like number, size, straightness, and also measured in terms of water velocity.
Hydraulic Conductivity
The ease with which a material will transmit a fluid. Takes into consideration properties of the material (permeability) and the fluid (density and viscosity)
How do permeability and porosity relate to groundwater?
Confined and unconfined aquifers.
Acquifer
Large body of permeable, saturated material through which groundwater can flow
How and where does groundwater flow?
- Water table has the same general shape as the overlying land surface
- The water table is deeper under mountains, so the slope is subdued here
- Groundwater flows downslope
- Where groundwater intersects the land surface, lakes, rivers, or wetlands may occur.
What controls the rate of groundwater flow?
- Permeability
- The rate of flow is strongly controlled by the permeability of a rock type. Flow is fastest in highly permeable cavernous limestone.
- Flow is moderately fast in a porous conglomerate or well-sorted sandstone.
- Flow is slower in shale, which has small pores, and in a granite with poorly connected fractures. - Hydraulic Gradient
- To a lesser degree, the rate of flow is controller by the steepness of the water table.
Potentiometric Surface
Heigh to which the water’s pressure would raise the water if the water were confined
How do we mine groundwater?
Qanats used for past 3000 years. They are a water management system used to provide a reliable supply of water to human settlements in hot, arid, and semi-arid climates.
Using ground water, what do you want?
Good Supply– adequate volume, as pure as possible
At low cost – for drilling, pumping, treat, transporting
What happens when we OVER mine groundwater?
- Cone of depression: mining groundwater can lower the surrounding water table
- Land subsidence: groundwater depletion
- Saltwater intrusion
Where does your water come from?
- Kaw river treatment plant
2. Clinton reservoir water treatment plant
As water travels over land surface, it dissolves natural occurring minerals and can pick up substances?
viruses and metals, salts, pesticides and herbicides, organic chemicals from industrial or petroleum use.