Page 305 Q 1-4 .. On looseleaf with heading

Water cycle :

Water cycle :

Impermeable

Impermeable

Impermeable

Zone of Saturation

Impermeable

Zone of Saturation

GROUNDWATER

Impermeable

Zone of Aeration

Zone of Saturation

GROUNDWATER

Impermeable

Zone of Aeration

Zone of Saturation

GROUNDWATER

Impermeable

Zone of Aeration

Zone of Saturation

Zone of Capillarity

GROUNDWATER

Impermeable

Zone of Aeration

Zone of Saturation

Zone of Capillarity

capillary water:• Adhesion: attraction between different objects

• Cohesion: attraction between like objects

• As pore size increases, capillary___________________

Do water on table and straw demo….

Notes page 2 relationship

10.________________________________________

11.________________________________________

12.________________________________________

13.________________________________________

14.________________________________________

15.

16. Pore space / total space x 100 = ____________

Notes page 4

1. size...

2. Affect porosity

a.

b.

c.

3

21

Notes page 4

3.

a.

b.

c.

Groundwater factors:• 1. Porosity

– – –

• 2. Permeability– – –

Factors of Groundwater:

• (a) porosity:

• sandy soil

• clay soil

Factors of Porosity

• Particle shape

• packing

• particle size

• sorting

FACTORS OF PERMEABILITY:

• 1.

• 2.

• 3.

• 4.

40.0 cm

40.0 cm

Fine grain size = 4.0 mm

Sediment: 500.0 ml

Shape: spherical sediment

Water to fill pores: 260.6 ml

Time for water to pass: 32.2 sec

Water passing through:182.4 ml

Water movement distance = 40.0 cm

Medium grain size = 7.0 mm

Sediment: 500.0 ml

Shape: spherical sediment

Water to fill pores: 260.0 ml

Time for water to pass: 12.6 sec

Water passing through: 218.3 ml

Water movement distance = 40.0 cm

Coarse grain size = 12.0 mm

Sediment: 500.0 ml

Shape: spherical sediment

Water to fill pores: 260.3ml

Time for water to pass: 9.9 sec

Water passing through: 232.1 ml

Water movement distance = 40.0 cm

Mixed Grain size = 12.0, 7.0, 4.0 mm

Sediment: 500.0 ml

Shape: spherical sediment

Water to fill pores: ___________

Time for water to pass: _______

Water passing through: _______

Water movement distance = 40.0 cm

Fine grain size = 4.0 mm

Sediment: 500.0 ml spherical sediment

Fine grain size = 4.0 mm

Sediment: 500.0 ml spherical sediment

Water to fill pores: 260.6 ml

Time for water to pass: 32.2 sec

Water passing through: 182.4 ml

Water movement distance = 40.0 cm

Medium grain size = 7.0 mm

Sediment: 500.0 ml spherical sediment

Medium grain size = 7.0 mm

Sediment: 500.0 ml spherical sediment

Water to fill pores: 260.0 ml

Time for water to pass: 12.6 sec

Water passing through: 218.3 ml

Water movement distance = 40.0 cm

Coarse grain size = 12.0 mm

Sediment: 500.0 ml spherical sediment

Coarse grain size = 12.0 mm

Sediment: 500.0 ml spherical sediment

Water to fill pores: 260.3ml

Time for water to pass: 9.9 sec

Water passing through: 232.1 ml

Water movement distance = 40.0 cm

Mixed Grain size = 12.0, 7.0, 4.0 mm

Sediment: 500.0 ml spherical sediment

Water to fill pores: ___________

Time for water to pass: _______

Water passing through: _______

Water movement distance = 40.0 cm

Lab • Porosity = Pore space (water to fill pores)

total space (500.0 ml) x 100

• Capillary Water =

Water to fill pores - Water passing through

As size increases, porosity ________

As size increases, permeability _____

As size increases, capillary ________

Copy on back of notes page 3…

Greenhouse effect

Copy on back of notes page 3…

Page 5 Binder notes…

WATER ENTERS THE ATMOSPHERE AND LEAVES

THE GROUND BY:

Evapotranspiration

(Ep or PE)

WATER ENTERS THE ATMOSPHERE AND LEAVES THE GROUND BY:

Evapotranspiration

WATER Leaves THE ATMOSPHERE AND Enters

THE GROUND BY:

Precipitation(P)

Tucson, AZ

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J F M A M J J A S O N D

mm

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P and Ep

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J F M A M J J A S O N D

mm

Tucson, AZP and Ep

Climate P/Ep or P/PE

Humid > 1.2

Subhumid 0.8 to 1.2

Semiarid 0.4 to 0.8

Arid < 0.4

Climate Classification

New Orleans

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J F M A M J J A S O N D

mm

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P and Ep

New Orleans

0

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J F M A M J J A S O N D

mm

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P and Ep

Key:

Blue = ppt

Red - Ep DO NOW

: Lab

Groups

Pages

7 an

d 8

Key:

Blue = ppt

Red - Ep

Climate Factors

• 1. Latitude

• 2. Altitude

• 3.Orographic effect

• 4. Closest to large body water

• 5. Currentsa. windb. ocean

COLOR CODE ESRT 4

Converge

Diverge

Converge

Converge

Diverge

LOW

HIGH

Converge LOW

Converge

Diverge

LOW

HIGH

Cold ocean

Cold ocean

Converge LOW

Warm Ocean

Warm Ocean

Converge

Diverge

LOW

HIGH

Cold ocean

Cold ocean

Converge LOW

Warm Ocean

Warm Ocean

Climate P/Ep or P/PE

Humid > 1.2

Subhumid 0.8 to 1.2

Semiarid 0.4 to 0.8

Arid < 0.4

Greenhouse effect

INSOLATION• INcoming

• SOLar

• radiATION• INSOLATION strength variables

• Angle of insolation

greatest=

• Duration of insolation

greatest=

Upwelling

the process by which warm, less-dense surface water is drawn away from along a shore by offshore currents and replaced by cold, denser water brought up from the subsurface.

El Nino Lab

http://www.bom.gov.au/lam/Students_Teachers/elnanim/elani.shtml

http://esminfo.prenhall.com/science/geoanimations/animations/26_NinoNina.html animation

April 2010: Airlines Face Continued Disruptions From Ash Clouds From

Iceland Volcano