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Approximately 71% Of Earth’s Surface Area Is Covered By |
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The cyclical movement of water through the various reservoirs is represented by the hydrologic cycle |
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Water is transferred from one reservoir to another through these processes |
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– Evaporation – Precipitation – Ground infiltration – Surface runoff – Transpiration |
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| 86% from ocean + 14% from land = 100% |
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| 78% over ocean + 22% over land = 100% |
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| 14% evapotranspiration + 8% runoff/groundwater = 22% total ppt |
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| 78% ppt over ocean + 8% runoff/groundwater = 86% returned to ocean |
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22% of all precipitation on Earth falls over |
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22% of all precipitation on Earth falls over land: |
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– Over half is returned to the atmosphere via evapotranspiration – The remainder flows to the sea as runoff |
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| Why so high?(perciptation in NW) |
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| Why high? (percipitation in SE) |
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Evapotranspiration is the combination of evaporation and transpiration: |
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Net movement of water molecules away from a wet surface into air that is less saturated |
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Outward movement of water through small openings (stomata) in the underside of leaves |
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| Over Half Of All Precipitation On Land Is Returned |
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| To The Atmosphere Via Evapotranspiration |
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| Evapotranspiration over land accounts for |
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14% of the entire hydrologic cycle |
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Precipitation over land that is not returned to the atmosphere via evapotranspiration flows back to the sea as runoff |
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Runoff follows two basic pathways to the sea: |
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Definition
Overland flow (95%) – Subsurface flow as groundwater (5%) |
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| 95% Of All Runoff Occurs As |
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Overland Flow And Runoff To Streams |
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| 5% Of All Runoff Percolates Through |
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Definition
Underlying Soil And Bedrock To The Groundwater System |
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| The Water-Balance Equation |
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The water budget is a portrait of the hydrologic cycle at a specific site or area |
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| – Precipitation at a site is measured using rain gauge |
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| Precipitation input must be balanced |
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– Actual Evapotranspiration (ACET) is the net outward movement of water molecules away from land and plants – Potential Evapotranspiration (POTET) is the water that would evaporate and transpire under optimum moisture conditions (when enough moisture is available) |
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| WATER balance equation: precipitation = |
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| actual evapotranspiration (i.e potential evapotranspiration-deficit) + surplus +- Change in soil moisture storage |
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POTET can also be measured with a lysimeter, which employs a buried tank opened at the surface |
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Potential evaporation is easily measured using an evaporation pan: |
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– As evaporation occurs, water in measured amounts is replaced in the pan so that no shortage occurs |
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there is not enough precipitation or moisture to meet demand |
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there is an oversupply of water |
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Term
A Weighing Lysimeter For Measuring Evaporation And Transpiration |
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Definition
Precipitation falls on lysimeter
Various pathways of water are traced
Weight of water added or lost is measured by scale
Some water remains as soil moisture; some is incorporated into plant tissues
Water passing through soil drains from the bottom of the lysimeter as groundwater and collected in tank
Runoff is collected in tank and measured |
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| Water not collected or retained is credited to |
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Potential Evapotranspiration (Water Demand) Factors include |
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| Excess water can be temporarily stored as soilmoisture: |
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thin molecular layer of water tightly bound to soil particles but not available for moisture demands |
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held in soil by surface tension and hydrogen bonding and is generally accessible to plant roots |
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excess water that percolates downward from the shallower capillary zone to the deeper groundwater zone |
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is water that remains for plants after water drains from larger pore spaces in soils |
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| Soil moisture from dryest to most wet |
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| hydroscopic, capillary,gravitational |
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| Best soil for plants is in between |
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| field capacity and wilting point |
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| Moisture supply available |
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Amount of water that would evaporate and transpire under optimum moisture conditions |
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| Actual evapotranspiration |
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If precipitation exceeds the amount of water required for POTET, |
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| If ACTET is less than POTET, |
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| then a water deficit will occur |
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Not enough water available to meet demand Recent droughts around the world (e.g. Australia and southwestern US) possibly linked to global climate change |
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Meteorological drought: Agricultural drought: Hydrologic drought Socioeconomic drought |
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Lower precipitation, higher temperatures and reduction in soil moisture |
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Changes in soil moisture and weather as they affect crop yields |
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Reservoir levels drop, stream flow decreases and groundwater mining increases |
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Water rationing, wildfires, and other problems affecting the economy and society |
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| Groundwater Profile and Movement |
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Groundwater is water found in the pores of soil and sediment, plus narrow fractures in bedrock |
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About 50% of U.S. population derives a portion of its freshwater from |
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| Groundwater supplies up to |
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100% of freshwater in some rural areas |
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| pore spaces filled with water +air |
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| is under the water table. pore spaces filled with 100% water |
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upper surface of the saturated zone |
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~4 km of the Earth’s surface |
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Porosity is the percentage of open spaces within a given volume of regolith or rock |
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Permeability is a measure of how easily a rock allows fluids to pass through it |
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porosity: very high permeability: very high |
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| coarse to medium grained sand |
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porosity: high permeability: high |
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| fine grained sand and salt |
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porosity: moderate permeability: moderate to low |
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| sandstone, moderately cemented |
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porosity: moderate to low permeability: low |
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| fractured shale or metamorphic rocks |
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porosity: low permeability: very low |
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porosity: very low permeability: very low |
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Characteristics of Groundwater Table |
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– Intersects the land surface at lakes, marshes, springs, and streams – Somewhat imitates the overlying land surface – May drop during dry seasons – Rises after heavy rainfalls |
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| the water table falls, reducing stream flow and drying up some wells |
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| Recharge of groundwater occurs in |
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areas where precipitation seeps downward to the saturation zone: Groundwater then flows to discharge areas |
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In areas of abundant rainfall, the recharge area may encompass the |
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entire landscape beyond stream channels |
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recharge occurs beneath an influent stream |
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Stream is site of groundwater discharge |
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Stream is site of groundwater recharge |
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The time water takes to move through the ground from recharge to discharge depends on: |
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– Permeability of material – Travel distance – Path of flow
Can range from days to thousands of years |
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| A Well Supplies Water When It |
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Definition
Penetrates the Water Table and Enters the Zone of Saturation |
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| A Cone Of Depression Forms When |
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The Rate Of Water Withdrawal Exceeds The Rate Of Local Groundwater Flow |
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is a body of rock such as shale that does not conduct water in usable amounts |
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is a highly permeable rock such as sandstone or porous limestone within the zone of saturation |
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Unconfined (not bound by aquicludes) – Confined (bounded above and below by aquicludes |
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| Hydrostatic Pressure Is The |
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Definition
Weight That An Overlying Column Of Water Would Exert At A Particular Depth |
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| Water under hydrostatic pressure seeks |
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to rise to the same height as its pressure (potentiometric) surface |
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Artesian system occurs where groundwater under pressure rises above the level of an aquifer |
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| Two conditions are necessary: |
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– Aquifer is inclined with one end receiving water (recharge area) – Aquifer is confined with aquicludes above and below |
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In artesian wells, water rises on its own without pumping |
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| Two types of artesian wells |
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Nonflowing occurs when pressure surface is below ground and water does not reach surface – Pressure surface above ground creates a flowing artesian well |
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Changes in the Water Table With Time |
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In regions where withdrawal of water exceeds recharge, the water table will gradually drop |
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High Plains Aquifer 170,000 wells irrigate |
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Groundwater can be contaminated by: |
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– Drainage from septic tanks, broken sewers and barnyards – Agricultural poisons – Highway salts – Buried hazardous wastes – Invading seawater along coastal areas |
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Water supply in the United States comes from surface and groundwater sources |
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BGD: Billions of gallons a day Of the average 4200 BGD precipitation received by the U.S., 71% ends up as ACTET while 29% is surplus |
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of vegetation; all water as ACTET is returned to the atmosphere |
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runoff available for withdrawal, consumption, and various instream (navigation, wildlife, hydroelectric power, etc.) uses |
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Surplus water that is not consumed eventually ends up |
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All the precipitation received is eventually returned |
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Definition
to the atmosphere and ocean |
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Desalination of seawater can augment diminishing groundwater supplies |
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| For the following illustration of the Hydrologic Cycle, what do the yellow arrows represent? |
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| Most runoff on land occurs in the subsurface as groundwater. |
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| What percentage of water evaporated over land and water eventually ends up as precipitation? |
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| What is potential evapotranspiration? |
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| Amount of water that would evaporate and transpire under optimum (saturated) moisture conditions |
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| In the water balance equation, actual evapotranspiration (ACTET) is equal to... |
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| Potential evapotranspiration (POTET) minus deficit (DEFIC) |
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| or the following figure of the water budget for Saskatoon, Saskatchewan, the blue curve represents precipitation, the orange curve potential evapotranspiration (POTET), and the green curve actual evapotranspiration (ACTET). During what time of year is the moisture deficit the greatest? |
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| With regard to soil-moisture storage, what happens to excess moisture (known as gravitational water) that cannot be held in the soil? |
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| Excess moisture percolates downward to the deeper groundwater zone |
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| Which of the following statements about groundwater is FALSE? |
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| Groundwater only consists of subsurface water that occurs above the water table |
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| Which of the following statements about groundwater is TRUE? |
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| Groundwater flows from areas of recharge to discharge |
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| __________ is a measure of how readily groundwater flows through soil, sediment, and bedrock |
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| Which of the following has the highest porosity and would therefore make the best aquifer? |
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| In order for an aquifer to be an artesian system and supply well-water to the surface without pumping, the aquifer must be _________ and ______________. |
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| Inclined/bounded above and below by aquicludes |
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| If groundwater was excessively pumped by wells over a long period of time, which of the following would most likely result? |
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