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Water On and Under the ground Water On and Under the ground.

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Presentation on theme: "Water On and Under the ground Water On and Under the ground."— Presentation transcript:

1 Water On and Under the ground Water On and Under the ground

2 Precipitation “rain” Precipitation “rain” Evaporation liquid converts to a vapor Evaporation liquid converts to a vapor Condensation vapor converts to a liquid Condensation vapor converts to a liquid Runoff excess water moving into rivers, lakes Runoff excess water moving into rivers, lakes Infiltration water “soaks” into the soil Infiltration water “soaks” into the soil Evapotranspiration (EvapT) evaporation + transpiration, evaporation from water bodies and off a plants Evapotranspiration (EvapT) evaporation + transpiration, evaporation from water bodies and off a plants

3 The Hydrologic Cycle Condensation water vapor cools and converts back to a “suspended” liquid Evaporation Ocean contributes 80% of total water vapor Cloud Formation Precipitation Surface Run-off Groundwater

4 II the HYDROLOGIC CYCLE I will get an A on my exams and quizzes. Discuss with a friend: 1.Draw the hydrologic cycle from memory Include the following: Include the following: precipitation evaporation condensation infiltration surface run-off groundwater 2. How do each of the above terms relate to one another? to one another?

5 Where has all the water gone ? 21%21%.03%.03%.003%.003%.62%.62% 76 % Most fresh water is locked up in ice (frozen water) Most fresh water is locked up in ice (frozen water) Fresh water %

6 How Water Affects Land Do you believe that water runs down-hill Where does it go????????????????????? Do you believe that water runs down-hill Where does it go????????????????????? Precipitation Overland flow Precipitation Overland flow Stream flow Stream Channel Stream flow Stream Channel Overland flow + Stream flow = Surface Runoff How does surface run-off affect streams and produce various land forms? How does surface run-off affect streams and produce various land forms?

7 Transportation of Sediment Load type of sediment carried by the stream Gradient the steepness of a stream channel Discharge the volume water exiting the stream (high or low) Transportation of Sediment Load type of sediment carried by the stream Gradient the steepness of a stream channel Discharge the volume water exiting the stream (high or low) The gradient, load and discharge defines the character of the stream and stream channel. how the stream flows what land features are formed The gradient, load and discharge defines the character of the stream and stream channel. how the stream flows what land features are formed

8 How does gradient influence the transportation of various types of loads? Sediment load types

9 Steeper Gradient transport of the bed load increase velocity Gentle Gradient transport of suspended and dissolved loads

10 How much “velocity” is needed (Discharge)

11 Transportation of Sediment The type and characteristics of stream can be described by its competence and capacity. Capacity: represents the maximum load of solid particles a stream can transport solid particles a stream can transport The greater the discharge, the greater capacity The greater the discharge, the greater capacity Competence: streams ability to carry various sizes Competence: streams ability to carry various sizes of sediment – not quantity of sediment – not quantity Flow velocity is the Key: a stream’s competence increases proportionately to the square of its velocity. If stream velocity doubles then, impact force is 4X greater If stream velocity doubles then, impact force is 4X greater If stream velocity triples, then impact force is 9X greater If stream velocity triples, then impact force is 9X greater If stream velocity quadruples, then impact force is ___ greater If stream velocity quadruples, then impact force is ___ greater 16X

12 II Watching the stream I will get an A on my exams and quizzes. Discuss with a friend: 1.How are gradient, discharge, and load related to stream channels? related to stream channels? 2. What are the three types of loads carried by streams? by streams? 3. Define the differences between capacity and competence of a stream. and competence of a stream.

13 Steep Gradient increase velocity increase load increase discharge Steep Gradient increase velocity increase load increase discharge Gentle Gradient decrease velocity decrease load decrease discharge Gentle Gradient decrease velocity decrease load decrease discharge Capacity? Competence? Moves large amounts of material – high volume Moves “big-stuff” and high impact force – bed load material Capacity? Moves small amounts of material –low volume Competence ? Moves small material – suspended/dissolved loads

14 Creating landforms by streams using erosion and deposition D E Deposition Erosion straight streams meandering streams braided streams

15 Straight Stream channel usually occurs over a short distance high gradient (near headwaters) takes on the classic “V” shape profile Straight Stream channel usually occurs over a short distance high gradient (near headwaters) takes on the classic “V” shape profile “V” shaped valley young stream “V” shaped valley young stream

16 Meandering stream channel low gradient erosional / depositional features Meandering stream channel low gradient erosional / depositional features Point Bars sand deposits Point Bars sand deposits Main channel Cut banks E E D D E E D D Where is the erosional and depositional parts of the river? Where is the erosional and depositional parts of the river?

17 Braided Stream channel very low gradient large load (lots of sediment) – causing the stream to “move” around the sediment and becoming “choked” Braided Stream channel very low gradient large load (lots of sediment) – causing the stream to “move” around the sediment and becoming “choked”

18 II watching the stream I will get an A on my exams and quizzes. Discuss with a friend: 1.List at least 2-characteristics that define a straight, meandering and braided stream channel system. stream channel system. Characteristics such as: load capacity, gradient and discharge

19 Stream deposits – what happens to the sediment when the stream looses energy – or decreases “gradient” Stream deposits – what happens to the sediment when the stream looses energy – or decreases “gradient” Types of stream deposits floodplains oxbow lakes alluvial fans delta deposits Types of stream deposits floodplains oxbow lakes alluvial fans delta deposits High Energy Low Energy

20 Floodplain “flat” area adjacent to a river which is invaded by high river discharge (flooding) Floodplain “flat” area adjacent to a river which is invaded by high river discharge (flooding) floodplain

21 Oxbow lake Oxbow lake Oxbow Lakes

22 Alluvial Fans – fan shaped sediment deposit Alluvial Fans – fan shaped sediment deposit Steep gradient carrying large sediment load enters an area that is flat Steep gradient carrying large sediment load enters an area that is flat

23 Where’s Bakersfield built on an alluvial fan Where’s Bakersfield built on an alluvial fan Bakersfield

24 Delta stream deposit stream deposits sediment into a large body of water (ocean) Cross-bedded deltaic deposits

25 Nile River in Egypt deposits sediment into the Mediterranean sea Delta means in Greek Nile River in Egypt deposits sediment into the Mediterranean sea Delta means in Greek

26 Flood Meandering streams Alluvial fans Alluvial fans Typical stream channel components Typical stream channel components

27 II Watching the stream deposits I will get an A on my exams and quizzes Discuss with a friend Define the four types of stream deposits 1. Define the four types of stream deposits 2. Give at least 2 characteristics of each stream deposit type stream deposit type 3. Describe how an oxbow lake forms

28 Surface Water as a hazard Floods Floods are NORMAL – only when people live in the area they become a hazard Floods can be predicted using a hydrograph Floods Floods are NORMAL – only when people live in the area they become a hazard Floods can be predicted using a hydrograph Time Scientists can predict the time of the water surge or when the crest will appear (water wave) Start

29 Predicting a flood

30 2 2 4 4 8 8 12 16 22 What if the Isabella Dam breaks? Will Bakersfield flood???? What if the Isabella Dam breaks? Will Bakersfield flood???? Alluvial fan

31 II Watching a flood I will get an A on my exams and quizzes Discuss with a friend 1.What is a hydrograph 2. How do scientist predict a flood for a particular area? a particular area? 3.How would you explain the flood map for the Bakersfield area the Bakersfield area

32 Groundwater distribution and Movement

33 Factors that influence the storage and movement of groundwater Factors that influence the storage and movement of groundwater Porosity: the amount of void spaces available to spaces available to store water store water Expressed as a % Porosity: the amount of void spaces available to spaces available to store water store water Expressed as a % 10% -20% 30%-50% Permeability: the ability for water to move (transmit) through the media (transmit) through the mediaPermeability: the ability for water to move (transmit) through the media (transmit) through the media

34 Distribution and Movement of groundwater Saturated Zone – pore spaces completely “full” Unsaturated Zone – pore spaces “not” full top of water table

35 II Drinking ground-water I will get an A on my exams and quizzes Discuss with a friend 1.Describe the differences between porosity and permeability and permeability 2. What does mean? (the symbol) 3. Define the following: 1.Unsaturated zone 2.Saturated zone 3.Perched aquifer

36 High Porosity - Permeability AquiferAquifer Low Porosity - Permeability AquitardAquitard Clay Aquifer under pressure (confined) Aquifer under pressure (confined) Porosity and Permeability

37 Movement of Groundwater Areas of high pressure Areas of Low pressure

38 II Groundwater characteristics I will get an A on my exams and quizzes Discuss with a friend 1.Describe the differences between an unconfined and confined aquifers unconfined and confined aquifers 2.What is an aquitard? 3. Describe the general flow of groundwater

39 DrawdownDrawdown Water Wells Producing a cone of depression AA BB Residential uses – small cone of depression (A) Industrial uses – large cone of depression (B)

40 “Pressure Surface Above pressure surface NOT - Artesian Below the pressure surface - Artesian Artesian well : flowing water from a well not being pumped being pumped confined conditions (1) pressure forces water up(2) Confined aquifer (1) Aquitard (2)

41 II Watching the stream I will get an A on my exams and quizzes Discuss with a friend 1.How would you describe a “cone of depression? depression? 2. How can groundwater wells influence other people living in an area? people living in an area? 3. What conditions are necessary to produce an artesian well? an artesian well?

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43 Groundwater Contamination Cecil Ave Muffler / Glass shop U-Save GAS Santa Monica Example:


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