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Where is Earth's water located ?

Where is Earth's water located ?. Earth’s Balancing act :. The Earth is a "closed system,“ That means that the Earth neither gains nor loses much matter, including water. Water is continually moving around, through, and above the Earth as water vapor, liquid water, and ice

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Where is Earth's water located ?

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  1. Where is Earth's water located?

  2. Earth’s Balancing act: • The Earth is a "closed system,“ That means that the Earth neither gains nor loses much matter, including water. • Water is continually moving around, through, and above the Earth as water vapor, liquid water, and ice • Although some matter, such as meteors from outer space, are captured by Earth, very little of Earth's substances escape into outer space.

  3. Thanks to the Water Cycle: • The same water that was on the Earth millions of years ago is still here. • the same water is continually being recycled all around the globe. • It is entirely possible that the water you drank for lunch was once used by Mama Allosaurus to give her baby a bath.

  4. Where is Earth's water located and in what forms does it exist? • about 97% of all water is in the oceans. • About 3% is fresh water. • Of the 3% fresh: 69% is locked up in glaciers & icecaps • 30.1% is ground water • .9% is other • .3% is Surface water • Of the .3% surface water: 2% is Rivers • 11% Swamps • 87% Lakes

  5. How much of Earth's water is available for our uses? • 99% of all water (oceans, seas, ice, most saline water, and atmospheric water) is NOT available for our uses • ONLY 1% can be used by us • Of this 1%: 99% is ground water • .86% comes from Lakes • .02% comes from Rivers

  6. Groundwater Storage • Groundwater storage is water existing for long periods below the Earth's surface. • Most of the water in the ground comes from precipitation that infiltrates downward from the land surface • The upper layer of the soil is the unsaturated zone, where water is present in varying amounts that change over time, but does not saturate the soil. • Below this layer is the saturated zone, where all of the pores, cracks, and spaces between rock particles are saturated with water.

  7. Aquifers • Another term for ground water is "aquifer," • This term is usually used to describe water-bearing formations capable of yielding enough water to supply peoples' uses. • Aquifers are a huge storehouse of Earth's water and people all over the world depend on ground water in their daily lives • Aquifers are replenished by the seepage of precipitation that falls on the land,

  8. Aquifers of Texas

  9. To find water underground, look under the water table • The top of the pool of water in this hole is the water table. • the water level in the hole is the same as the level of the ocean.

  10. Pumping can affect the level of the water table:

  11. Groundwater and global water distribution • Groundwater occurs only close to the Earth's surface. • There must be space between the rock particles for ground water to occur • Water in aquifers below the oceans is generally saline • Water below the land surfaces (where freshwater, which fell as precipitation, infiltrates into the ground) is generally freshwater.

  12. Lotic and Lentic Systems • There are two main types of surface freshwater ecosystems • Lentic • Stillwater • Lakes • Ponds • Lotic • Moving Water • Rivers • Streams

  13. Springs • A spring is a water resource formed when the side of a hill, a valley bottom or other excavation intersects a flowing body of ground water at or below the local water table • A spring is the result of an aquifer being filled to the point that the water overflows onto the land surface

  14. Is Spring Water fit to drink? • The quality of the water in the local ground-water system will generally determine the quality of spring water. • The quality of water discharged by springs can vary greatly because of factors such as the quality of the water that recharges the aquifer and the type of rocks with which the ground water is in contact. • rate of flow and the length of the flowpath through the aquifer affects the amount of time the water is in contact with the rock, and thus, the amount of minerals that the water can dissolve. • The quality of the water also can be affected by the mixing of freshwater with pockets of ancient seawater in the aquifer or with modern seawater along an ocean coast. (FYI)

  15. Rivers • A river is nothing more than surface water finding its way over land from a higher altitude to a lower altitude, all due to gravity.

  16. Parts of a River (draw this) Drainage Divide (separates one watershed from another) Source (snowpack, glaciers, springs, headwater streams) Tributary (small creek or river that runs into a larger one) Mouth (empties into lake or ocean; often forms a delta with extensive wetlands)

  17. Parts of a River • A river is confined to a channel bordered by banks. • When the river floods, it erodes a wider channel outside of its normal banks. This is a floodplain.

  18. Rivers • Rivers are invaluable to not only people, but to life everywhere! • People use river water for drinking-water supplies and irrigation water, to produce electricity, to flush away wastes (hopefully, treated wastes), to transport merchandise, and to obtain food. • Rivers even help keep the aquifers underground full of water by discharging water downward through their streambeds.

  19. Watersheds and Rivers • A watershed is the area of land where all of the water that falls in it and drains off of it goes to the same place. • It’s not just the rivers…

  20. What is a Watershed? • It is also known as a Drainage Basin • EPA: “A watershed is the area of land where all of the water that is under it or drains off of it goes into the same place.” • Wikipedia: an extent of land where water …drains downhill into a body of water (river, lake, estuary, wetland, sea or ocean.) The drainage basin includes both the streams and rivers that convey the water as well as the land surfaces from which water drains into those channels, and is separated from adjacent basins by a drainage divide.

  21. Addicks Reservoir Watershed

  22. Watersheds and Rivers • the main influence on stream flow is precipitation runoff in the watershed • The size of a river is highly dependent on the size of its watershed. Large rivers have watersheds with lots of surface area; small rivers have smaller watersheds.

  23. Rivers are always moving • Natural mechanisms • Runoff from rainfall and snowmelt • Evaporation from soil and surface-water bodies • Transpiration by vegetation • Ground-water discharge from aquifers • Ground-water recharge from surface-water bodies • Sedimentation of lakes and wetlands • Formation or dissipation of glaciers, snowfields, and permafrost

  24. Rivers are always moving • Human-induced mechanisms • Surface-water withdrawals and transbasin diversions • River-flow regulation for hydropower and navigation • Construction, removal, and sedimentation of reservoirs and stormwater detention ponds • Stream channelization and levee construction • Drainage or restoration of wetlands • Land-use changes such as urbanization that alter rates of erosion, infiltration, overland flow, or evapotranspiration • Wastewater outfalls • Irrigation wastewater return flow

  25. Lakes • A lake is where surface-water runoff (and maybe some ground-water seepage) have accumulated in a low spot, relative to the surrounding countryside. • It's not that the water that forms lakes get trapped, but that the water entering a lake comes in faster than it can escape, either via outflow in a river, seepage into the ground, or by evaporation.

  26. Lakes and Reservoirs • A reservoir is a manmade lake that is created when a dam is built on a river. River water backs up behind the dam creating a reservoir. • Lakes formed by the erosive force of ancient glaciers, such as the Great Lakes, can be thousands of feet deep. Some very large lakes may be only a few dozen feet deep

  27. Limnology - The study of lakes • The condition of a lake at a given time is the result of the interaction of many factors—its watershed, climate, geology, human influence, and characteristics of the lake itself • Each lake system is unique, and its dynamics can be understood only to a limited degree based on information from other lakes

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