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EEOS 350 – Quantitative Hydrogeology

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EEOS 350 – Quantitative Hydrogeology. Syllabus  an (optimistic) approximation of what we will cover. Text: Fundamentals of Ground Water, Schwartz and Zhang, 2003. http://www.wiley.com/WileyCDA/WileyTitle/productCd-0471137855.html - PowerPoint PPT Presentation
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September 4, 2007 EEOS 350 – Quantitative EEOS 350 – Quantitative Hydrogeology Hydrogeology Syllabus Syllabus an (optimistic) an (optimistic) approximation of what we will approximation of what we will cover. cover. Text: Fundamentals of Ground Text: Fundamentals of Ground Water, Schwartz and Zhang, 2003. Water, Schwartz and Zhang, 2003. http://www.wiley.com/WileyCDA/Wi http://www.wiley.com/WileyCDA/Wi leyTitle/productCd-0471137855.ht leyTitle/productCd-0471137855.ht ml ml ERRATA!! Need to go through and ERRATA!! Need to go through and highlight the errors in your highlight the errors in your text! text!
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Page 1: EEOS 350 – Quantitative Hydrogeology

September 4, 2007 1

EEOS 350 – Quantitative EEOS 350 – Quantitative HydrogeologyHydrogeology

Syllabus Syllabus an (optimistic) an (optimistic) approximation of what we will approximation of what we will cover.cover.

Text: Fundamentals of Ground Text: Fundamentals of Ground Water, Schwartz and Zhang, 2003. Water, Schwartz and Zhang, 2003. http://www.wiley.com/WileyCDA/Wihttp://www.wiley.com/WileyCDA/WileyTitle/productCd-0471137855.htleyTitle/productCd-0471137855.htmlml

ERRATA!! Need to go through and ERRATA!! Need to go through and highlight the errors in your text!highlight the errors in your text!

Page 2: EEOS 350 – Quantitative Hydrogeology

September 4, 2007 2

EEOS 350 – Quantitative EEOS 350 – Quantitative HydrogeologyHydrogeology

Field trip at Nantucket Field siteField trip at Nantucket Field site

http://www.umb.edu/nantucket/http://www.umb.edu/nantucket/

– Water level mapWater level map– Slug testsSlug tests– Install transducersInstall transducers– Run pumping testRun pumping test

Page 3: EEOS 350 – Quantitative Hydrogeology

September 4, 2007 3

Water FactsWater Facts Requirements:Requirements:

– A person requires 3 liters/day (3.2 qts/day) of water A person requires 3 liters/day (3.2 qts/day) of water for drinking (minimum survival requirement)for drinking (minimum survival requirement)

– 50 liters/day (13.2 gal/day) for drinking, sanitation 50 liters/day (13.2 gal/day) for drinking, sanitation and hygiene.and hygiene.

– 1300 m1300 m33/yr (940 gal/day) when food production is /yr (940 gal/day) when food production is included. included.

Uses:Uses:– Average US citizen uses 80 to 100 gal/day. During Average US citizen uses 80 to 100 gal/day. During

medieval times, a person only used 5 gal/day (didn’t medieval times, a person only used 5 gal/day (didn’t shower much, I guess).shower much, I guess).

– A single flush of a toilet requires 2-7 gal (same as A single flush of a toilet requires 2-7 gal (same as King Arthur used in a whole day!)King Arthur used in a whole day!)

– 2 gal to brush teeth, 25-50 gal for shower2 gal to brush teeth, 25-50 gal for shower– It takes 1 gal of water to process a quarter pound of It takes 1 gal of water to process a quarter pound of

hamburger.hamburger.– It takes 2072 gal to make 4 tires.It takes 2072 gal to make 4 tires.

Page 4: EEOS 350 – Quantitative Hydrogeology

September 4, 2007 4

How much water stored (in How much water stored (in %)?%)?

OceansOceans 96.596.5 Ice caps/glaciers/snowIce caps/glaciers/snow 1.74 1.74 GroundwaterGroundwater 1.7 1.7

– FreshFresh (0.76%)(0.76%)– Saline (0.94%)Saline (0.94%)

Freshwater lakesFreshwater lakes 0.007 0.007 Inland seas/salt lakesInland seas/salt lakes 0.008 0.008 Soil moistureSoil moisture 0.001 0.001 AtmosphereAtmosphere 0.001 0.001 All RiversAll Rivers 0.0002 0.0002 Biological waterBiological water 0.0001 0.0001

Page 5: EEOS 350 – Quantitative Hydrogeology

September 4, 2007 5

The Hydrologic Cycle

Source: www.cet.nau.edu/Projects/ SWRA/research.html

Fluxes (flows)Stocks (storage)

Page 6: EEOS 350 – Quantitative Hydrogeology

September 4, 2007 6

Components of the water Components of the water cyclecycle

Fluxes (flows)Fluxes (flows)– Units = volume/time or Units = volume/time or

depth/time(in/yr, depth/time(in/yr, mm/hr)mm/hr)

– These are the These are the “renewable” “renewable” componentscomponents

PrecipitationPrecipitation EvaporationEvaporation TranspirationTranspiration InfiltrationInfiltration RechargeRecharge RunoffRunoff StreamflowStreamflow Groundwater flowGroundwater flow

Storage (stocks)Storage (stocks)– Units = Volume (ftUnits = Volume (ft33, m, m33))– These are the These are the

components that are components that are emptied or filled by the emptied or filled by the fluxesfluxes

Soil moisture storage Soil moisture storage (unsaturated zone)(unsaturated zone)

Surface storage Surface storage (lakes, ponds, (lakes, ponds, puddles)puddles)

Atmospheric storage Atmospheric storage (water vapor)(water vapor)

Aquifer storage Aquifer storage (saturated zone)(saturated zone)

Page 7: EEOS 350 – Quantitative Hydrogeology

September 4, 2007 7

Source: Jackson et al, 2001

Page 8: EEOS 350 – Quantitative Hydrogeology

September 4, 2007 8

Global renewable water resourcesGlobal renewable water resources~ ~ 40,000 billion cubic meters 40,000 billion cubic meters

(BCM)(BCM) Accessible in both space & timeAccessible in both space & time

~ ~ 20,000 BCM20,000 BCM Minimum human freshwater Minimum human freshwater

requirements = 1,300 mrequirements = 1,300 m33/yr per person/yr per person ~ ~ 7,800 BCM7,800 BCM

Human requirementsHuman requirements

~ ~ 39% of total supply and yet…39% of total supply and yet…

Page 9: EEOS 350 – Quantitative Hydrogeology

September 4, 2007 9

……in the year 2000:in the year 2000:– 1 billion people lacked access to 1 billion people lacked access to

improved drinking waterimproved drinking water»2 out of 5 Africans2 out of 5 Africans

– 2.4 billion lacked access to 2.4 billion lacked access to improved sanitationimproved sanitation»fewer than half of all Asiansfewer than half of all Asians

Source: Global Water Supply and Sanitation Assessment 2000 Report, WHO

Page 10: EEOS 350 – Quantitative Hydrogeology

September 4, 2007 10

…because freshwater is not evenly distributed.

Page 11: EEOS 350 – Quantitative Hydrogeology

September 4, 2007 11

What makes water so What makes water so unique?unique?

Water is the only substance found Water is the only substance found in all three states (phases) at in all three states (phases) at ambient temperatures.ambient temperatures.– Water has unusually high melting and Water has unusually high melting and

boiling points.boiling points.

Page 12: EEOS 350 – Quantitative Hydrogeology

September 4, 2007 12

What makes water so What makes water so unique?unique?

Water expands when both heated Water expands when both heated or cooled from 4or cooled from 4°C.°C.– This makes fish VERY happy, but This makes fish VERY happy, but

sometimes not water fowl!sometimes not water fowl!

Page 13: EEOS 350 – Quantitative Hydrogeology

September 4, 2007 13

What makes water so What makes water so unique?unique?

Water is a “universal solvent”.Water is a “universal solvent”.– High dielectric constant because of it’s High dielectric constant because of it’s

polar structurepolar structure– Strong hydrogen bondsStrong hydrogen bonds

Page 14: EEOS 350 – Quantitative Hydrogeology

September 4, 2007 14

What makes water so What makes water so unique?unique?

Water has a:Water has a:– Extremely low compressibility (water is Extremely low compressibility (water is

considered essentially incompressible).considered essentially incompressible).– high thermal conductivity (that’s why we high thermal conductivity (that’s why we

get cold even when the pool is heated)get cold even when the pool is heated)– Low electrical conductivityLow electrical conductivity– High viscosity (relative to other liquids)High viscosity (relative to other liquids)– High surface tension (making water High surface tension (making water

skippers happy, too!). Surfactants reduce skippers happy, too!). Surfactants reduce surface tension.surface tension.

Page 15: EEOS 350 – Quantitative Hydrogeology

September 4, 2007 15

Physical properties of Physical properties of waterwater

Density, Density, : : – 1,000 kg/m1,000 kg/m33 at at

44°C°C– 1.94 slugs/ft1.94 slugs/ft33 at 40°F at 40°F

Specific weight:Specific weight:

Specific gravity:Specific gravity:

g

w

fSG

Page 16: EEOS 350 – Quantitative Hydrogeology

September 4, 2007 16

Hydrologic CycleHydrologic Cycle

Water BalanceWater BalanceInflow - Outflow = change in storageInflow - Outflow = change in storage

*assumes conservation of mass *assumes conservation of mass mass mass (in this case, water) is neither created (in this case, water) is neither created nor destroyed within the control nor destroyed within the control volume)volume)

Page 17: EEOS 350 – Quantitative Hydrogeology

September 4, 2007 17

Water balanceWater balance

For a water balance (or any mass For a water balance (or any mass balance), you need:balance), you need:– Control volumeControl volume the boundaries of your the boundaries of your

analysisanalysis– Water balance termsWater balance terms inputs and inputs and

outputs across the CV, storage within CVoutputs across the CV, storage within CV– Time stepTime step time frame over which your time frame over which your

water balance terms are estimated.water balance terms are estimated.

Page 18: EEOS 350 – Quantitative Hydrogeology

September 4, 2007 18

Control VolumeControl Volume

For mass (or water) balance For mass (or water) balance analysis, need to establish the size analysis, need to establish the size (scale) of the problem.(scale) of the problem.

For a surface water balance, the For a surface water balance, the control volume is the watershed. control volume is the watershed. (Control volume is much harder to (Control volume is much harder to establish in groundwater balance).establish in groundwater balance).

What is a watershed?What is a watershed?

Page 19: EEOS 350 – Quantitative Hydrogeology

September 4, 2007 19

Page 20: EEOS 350 – Quantitative Hydrogeology

September 4, 2007 20

Delineating a watershed Delineating a watershed boundaryboundary

Pick a point of interest on the streamPick a point of interest on the stream Start on right or left bank, draw a line away Start on right or left bank, draw a line away

from that point, always maintaining the line from that point, always maintaining the line perpendicular to contoursperpendicular to contours

continue line until it is going opposite of continue line until it is going opposite of starting direction (in general).starting direction (in general).

WS boundaries tend to follow ridge lines.WS boundaries tend to follow ridge lines. Always ask “If I was a drop of water, which Always ask “If I was a drop of water, which

way would I fall”way would I fall” A WATERSHED BOUNDARY NEVER CROSSES A A WATERSHED BOUNDARY NEVER CROSSES A

STREAM CHANNEL.STREAM CHANNEL. Start on opposite bank and do the same for Start on opposite bank and do the same for

other side of watershed.other side of watershed.


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