the natural environment
DESCRIPTION
The Natural Environment. The Hydrologic Cycle . Hydrologic Processes. Hydrologic Budget. Change in storage = inflow – outflow ∆S = P – R – G – E – T Where: P = Precipitation R = Surface Runoff G = Groundwater E = Evapotranspiration T = Transpiration - PowerPoint PPT PresentationTRANSCRIPT
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The Natural Environment
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The Hydrologic Cycle
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Hydrologic Processes
Precipitation Evapotranspiration Infiltration
Overland Flow Groundwater Flow
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Hydrologic Budget• Change in storage = inflow – outflow
• ∆S = P – R – G – E – T–Where:• P = Precipitation• R = Surface Runoff• G = Groundwater• E = Evapotranspiration• T = Transpiration• ∆S = Change in storage over specified
time
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Aral Sea1989 2008
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Watersheds
• Area of land which drains to a single outlet point
• Characterized by– Size, slope, shape, soil
type, storage capacity, land use, channel morphology
• Basin– Large watershed– i.e. Mississippi river basin
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Hydrology and Infrastructure• Design infrastructure to
withstand precipitation of specific reoccurrence interval
• 100yr = 1% chance• 10yr = 10% chance• Expense increases as you
design to a less frequent return period
• Location specific IDF curves relate rainfall intensity and duration to probability
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Rivers and Infrastructure• flood probabilities not directly related to storm
probabilities– 100yr storm does not necessarily equate to 100yr flood
• Floodplain– The land along a stream or river that is inundated when
the stream overtops its banks• FEMA determines 100yr floodplain and updates it
accordingly with increasing development– More impermeable surfaces = more runoff– Most building codes prohibit construction in the 100yr
floodplain
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The Woodlands
•Designed to handle 100yr flood by not altering the natural floodplain
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Geological Formations• Soil
– Uppermost layer of unconsolidated material that lies above the uppermost layer of rock (consolidated material)
• Soil type and location of bedrock have huge influence in construction– Borings used to design
building foundation– Location of consolidated
material varies even over a short distances
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Vertisols and Houston
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Groundwater• Water which fills
pores and fractures of unconsolidated material
• Aquifer– Geologic formation
that stores water• Supply in jeopardy
as demand increases
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Aquifer
Source: National Groundwater Association
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Porosity, Head and GW Flow RatesDarcy’s Law (1856) relates change in head and hydraulic conductivity to groundwater flow rates:
dLdhK
AQV
Seepage velocity (actual flow) is Darcy’s velocity divided by the porosity of the groundwater medium:
)(ndLdhK
nAQVs n = porosity
Porosity = vol void / total vol
dh/dL = change in headK = hydraulic conductivity = 10-2 cm/s (Sand) = 10-4 cm/s (Silt) = 10-7 cm/s (clay)
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Climate ChangeGreenhouse Gases:• Trap heat radiating outward from Earth• Increase Earth’s temperature to support life• 30oC cooler w/o
• Increasing concentrations amplify such warming
•Five main greenhouse gases:• Water Vapor (H2O) .004 – 4% (40–40000ppm)• Carbon Dioxide (CO2) .0391% (391ppm)• Methane (CH4) .00017% (1.7ppm)• Nitrous Oxide (N2O) .000033% (.33ppm)• Ozone (O3) .000005%
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IPCC and Climate Change•Intergovernmental panel on climate change• International body for the
assessment of climate change• Found that climate change is most likely anthropogenic•Kyoto protocol created as a result• Calls for 5% global reduction
in greenhouse gas emissions• US assigned 7% reduction• US has not signed
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Kyoto Countries
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Climate Change Consequences• Increased drought and water
shortages• Extinction• Coral reef loss• Alterations to carbon cycle• Loss of habitat• Changes in locations of
agricultural regions• Increased flooding• Increased malnutrition and
disease• Increased frequency and
severity of storms
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Climate Change Consequences
Downtown Boston 100 year floodplains: current (solid)After “high level” greenhouse gas emission scenario (dashed)
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Dealing With Climate Change
Above: IPCC projected global mean temperature change with different emission scenarios
Below: Global temperature profile with different GHG emission scenarios
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Engineering for Climate Change
• Problem:– Predicting the extent of
climate change is challenging
– Two options:• 1. design for current
day conditions and risk failure• 2. design for worst
case scenario and risk extra expenditure
• Solution:– Adaptive management
• Incorporate future uncertainties into design plan so that if changes do occur, strategy is in place to handle them • E.g. Design levee to be
readily modified to accommodate seawater increase
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Conclusion
• Infrastructure has impact on the environment and the environment impacts infrastructure
• Relationship must be understood for future sustainable development