hydrologic cycle. sand porosity and permeability

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Hydrologic Cycle

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Page 1: Hydrologic Cycle. Sand porosity and permeability

Hydrologic Cycle

Page 2: Hydrologic Cycle. Sand porosity and permeability
Page 3: Hydrologic Cycle. Sand porosity and permeability

Sand porosity

and permeability

Page 4: Hydrologic Cycle. Sand porosity and permeability

Fig. 19.06

W. W. Norton

Shallow aquifer

Confining bed/aquitard

Deeper aquifer

Page 5: Hydrologic Cycle. Sand porosity and permeability

Fig. 19.07 a

Unsaturated zone

Page 6: Hydrologic Cycle. Sand porosity and permeability

Fig. 19.11

W. W. Norton

HUMID CLIMATE

Important to identify recharge areas!!!! Do not pollute them!

Page 7: Hydrologic Cycle. Sand porosity and permeability

Gaining Stream

Page 8: Hydrologic Cycle. Sand porosity and permeability

Losing stream

ARID CLIMATE

Page 9: Hydrologic Cycle. Sand porosity and permeability

Fig. 19.13

W. W. Norton

Page 10: Hydrologic Cycle. Sand porosity and permeability

Determine which wayGroundwater flows

Determine location ofRecharge/discharge areas

Page 11: Hydrologic Cycle. Sand porosity and permeability

Cone of depression

Page 12: Hydrologic Cycle. Sand porosity and permeability

Fig. 19.15 a

W. W. Norton

Page 13: Hydrologic Cycle. Sand porosity and permeability

Fig. 19.15 b

W. W. Norton

Page 14: Hydrologic Cycle. Sand porosity and permeability

Fig. 19.15 c

W. W. Norton

Page 15: Hydrologic Cycle. Sand porosity and permeability
Page 16: Hydrologic Cycle. Sand porosity and permeability
Page 17: Hydrologic Cycle. Sand porosity and permeability

Fig. 19.22 a, b

W. W. Norton

Page 18: Hydrologic Cycle. Sand porosity and permeability
Page 19: Hydrologic Cycle. Sand porosity and permeability

South Florida before pumping South Florida after pumping

Page 20: Hydrologic Cycle. Sand porosity and permeability

Fig. 19.06

W. W. Norton

AQUIFER TYPES

Confining bed

Page 21: Hydrologic Cycle. Sand porosity and permeability

Confined/artesian aquifer

Note: aquiclude = confining bed!

Page 22: Hydrologic Cycle. Sand porosity and permeability
Page 23: Hydrologic Cycle. Sand porosity and permeability

Fig. 19.16 c

W. W. Norton

The potentiometric surface is a pressure surface

It’s the level to which water will rise in your well!

Page 24: Hydrologic Cycle. Sand porosity and permeability
Page 25: Hydrologic Cycle. Sand porosity and permeability

Flooding due to subsidence in Indonesia

Page 26: Hydrologic Cycle. Sand porosity and permeability

Fig. 19.09

W. W. Norton

Page 27: Hydrologic Cycle. Sand porosity and permeability
Page 28: Hydrologic Cycle. Sand porosity and permeability

Unit Conversions

Common units used to measure water are:

• cfs (cubic feet per second)• gallons• acre-foot• inches (in precip gage)

Need to be able to convert between them

Page 29: Hydrologic Cycle. Sand porosity and permeability

Acre-foot

1 acre-foot = 43,560 ft2/acre x 1 foot = 43,560 ft3

How many gallons is this???

Page 30: Hydrologic Cycle. Sand porosity and permeability

Cubic feet gallons

• 7.48 gallons = 1 ft3

• 43,560 ft3 x 7.48 gal/1 ft3 = 325,829 gal

Page 31: Hydrologic Cycle. Sand porosity and permeability

Length-Area-VolumeL vs. L2 vs. L3

1 ft2

12 inches

12 inches

12 inches x 12 inches =

144 in2

=1 ft2

Page 32: Hydrologic Cycle. Sand porosity and permeability

Length-Area-VolumeL vs. L2 vs. L3

1 ft312

inch

es

12 inches

12 inches

12 in x 12 in x 12 in = 1728 in3 = 1 ft3

Page 33: Hydrologic Cycle. Sand porosity and permeability

CRATER LAKE

Surface area = 579,348,000 ft2

Avg. ann. Precip = 68 in.

What volume of precip. is added to the lake in acre-feet each year?

1) Need to convert units to makethem consistent. It’s easiest to convert Feet to acre-feet, so let’s convert inches toFeet!68 in x 1 foot /12 inches = 68/12 feet = 5.67 ft

2) Calculate volume of precip. in ft3 by multiplying Surface area of lake x depth of precip.579,348,000 ft2 x 5.67 ft = 3,284,903,160 ft3

3) Convert ft3 to acre-ft 3,284,903,160 ft3 x 1 ac-ft/43,560 ft3 = 75,411 acre-ft/year from ppt.