SOIL AND THE HYDROLOGIC CYCLEww2.odu.edu/~jrule/geo508/Geol_408-Ch_6web.pdf · -major component of...
Transcript of SOIL AND THE HYDROLOGIC CYCLEww2.odu.edu/~jrule/geo508/Geol_408-Ch_6web.pdf · -major component of...
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CHAPTER 6
Brady & Weil, Rev. 14th ed.
GEOLOGY 408/508
SOIL AND THEHYDROLOGIC CYCLE
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(FIGURE 6.2)
THE HYDROLOGIC CYCLE
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Watershed - an area of land drained by a single stream system and is separated from adjacent areas by ridges
• An important ecological concept; activities inone area may affect entire watershed
• Water-balance equation:P = ET + SS + D
P = precipitationET - evapotranspirationSS - soil storageD - discharge
WATER BALANCE EQUATION
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• Interception - catchment of precipitation by canopy vegetation- may prevent 30-50% rainfall from
reaching soil
• Water impacting soil:- infiltration
- soil storage- drainage from profile
- surface runoff- may cause erosion
FATE OF PRECIPITATION & IRRIGATION WATER
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Effects of Vegetation & Soil Properties on Infiltration
• Type of vegetation- grasslands - dense vs sparse cover- forests - dense vs sparse cover
• Stem flow- slows and captures rainfall - varies with vegetation type
• Soil management- enhance surface retention in cultivated fields- cover crops
• Soil porosity- loose & open vs. tightly packed
FATE OF PRECIPITATION & IRRIGATION WATER
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Two methods of increasing infiltration and slowing runoff in urbanized watersheds
Permeable pavers Inlet to a small rain garden
FIGURE 6.11a,b
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(SPAC)
(FIGURE 6.14)
Water movement through various media
SOIL-PLANT-ATMOSPHERE CONTINUUM
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SPAC = Soil - Plant - Atmosphere Continuum-major component of hydrologic cycle
Water movement - two major points of resistance:- root-soil water interface- leaf cell - atmosphere interface
Component Moisture potential
Atmosphere -20,000 kPaLeaf surface -500 kPaUpper plant (internal) -85 kPaLower plant (internal) -75 kPaSoil water -50 kPa
WATER BALANCE
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• Evaporation (E) - loss of water from soil surface
• Transpiration (T) - loss of water from plant leaves
• Evapotranspiration (ET) - combined loss of water - most commonly measured
• Potential evapotranspiration (PET) - useful info
• Water deficit = (PET) - (ET)
• ET losses vary greatly with plant type
SOIL-PLANT-ATMOSPHERE CONTINUUM
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In most areas, it is desirable to limit ET:
• limit nutrient supply to plants to limit growth
• decrease plant density (partially effective) limits leaf area index
• eliminate undesirable plants (weeds)
• fallow cropping (use in semiarid lands)
CONTROL OF EVAPOTRANSPIRATION
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Partitioning of liquid water losses (discharge) and vapor losses (evaporation and Transpiration) in regions varying from low (arid) to high (humid) levels of annual precipitation. (FIGURE 6.20)
LIQUID AND
VAPOR LOSSES
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• Vegetative mulches:sawdust, manure, leaves, straw, crop residue
• Paper & plastic mulches:- generally use specially prepared material- can use newspapers, etc
• Crop residues & conservation tillage:- leaves a high percentage of previous crop- leaves stubble mulch- plants next crop without tillage
CONTROL OF SURFACE EVAPORATION
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Percolation & leaching:
• Loss of water/chemicals to the groundwater
• Study with tile drains or lysimeters
• High percolation rates give a high potential for leaching losses
• Percolation losses influenced by: amount & distribution of rainfall
LIQUID LOSSES OF WATER FROM THE SOIL
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(FIGURE 6.25)
Generalized curves for precipitation & evapotranspiration for three temperate zone regions
Max. supply is not generally during max. need
LIQUID LOSSES OF WATER FROM THE SOIL
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Groundwater resources:
• Significant water source for domestic, industrial & agricultural uses
• About 50% of people use some groundwater
• Local versus regional aquifers - Ogallala aquifer
• Supply versus withdrawl
• Overpumping aids contaminant influx
• Coastal areas: potential saltwater intrusion
PERCOLATION AND GROUNDWATERS
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Relationship of the water table and groundwater to water movement into and out of the soil. (FIGURE 6.27)
SUBSURFACE WATER
MOVEMENT
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Shallow groundwater:
• most dynamic portion of groundwater
• may supply growing plants via capillary fringe
Chemicals in drainage water:
• chemicals may leach into groundwater- nutrients
- loss from plant use (lost $$)- cause eutrophication (NO3
-)- contaminants
- pesticides- pathogens
PERCOLATION AND GROUNDWATERS
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Chemical movement through macropores:
• Preferential or bypass flow - chemicals merely applied to surface do not contact bulk of soil
• High intensity rain or irrigation increases bypass flow
• Need to control irrigation rates and manage soil properties (macropore properties)
PERCOLATION AND GROUNDWATERS
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Preferential or bypass flow in macropores transports soluble chemicals downward through a soil profile.
Note that if the pore is not open to the surface, the bypass flow will NOT occur. (FIGURE 6.29)
BYPASS FLOW IN
MACROPORES
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Reasons for enhancing drainage:• engineering problems: soil stability for
roadbeds, building foundations • plant Production: tillage restrictions, oxygen
limitations, low temps in springtime, limited rooting depth in springtime
Surface drainage systems:- drainage ditches- land forming
ENHANCING SOIL DRAINAGE
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Subsurface (internal) drainage:
• deep open-ditch drainage- best for coarse textured soils- barriers for eqiopment
• buried perforated pipes (drain tiles)- can last for many years- do not disrupt surface operations
• building foundation drains- Figure 6.32c
• mole drainage- inexpensive; use in clay soils
ENHANCING SOIL DRAINAGE
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(FIGURE 6.30)
REGIONAL AND PERCHED WATER TABLES
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Illustration of water levels of undrained and tile-drained land in the spring and summer. (FIGURE 6.31)
tile
UNDRAINED AND TILE-
DRAINED LAND
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(FIGURE 6.32a,b)
OPEN DITCH & TILE DRAINS IN FIELDS
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(FIGURE 6.32c)
FOOTER DRAIN AROUND FOUNDATION
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(Figure 6.38)
Wastewater stimulation of lawn grass from poorly functioning system
Standard system
Utility of perc test
SEPTIC TANK AND DRAIN FIELD
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Importance of irrigation today:
• landscaping- use is increasing- used to grow non-native species- large amounts used in semi-arid regions
• food production- agriculture is largest consumptive user- large amounts used in semi-arid regions
• future prospects- demand increasing, supplies decreasing- will become global crisis
IRRIGATION PRINCIPLES & PRACTICES-1
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Water-use efficiency:
• application efficiency- applied vs amount used by plants- inefficient, 30-50% used by plants- loss from ditches, evaporation
• field water efficiency- (transp by crop) ÷ (applied to field) × 100- values low, 50-60%- much lost via runoff, percolation, evap’n
IRRIGATION PRINCIPLES & PRACTICES-2
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Surface irrigation:- use supply ditches & furrows - application control difficult- precise slope control needed- inexpensive system to install
Sprinkler systems:- additional losses from evaporation- plants are cooled by application of water- plant foliage may stay wet - fungal probs- more expensive than surface systems- generally uniform application
IRRIGATION PRINCIPLES & PRACTICES-3
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CENTER PIVOT IRRIGATION SYSTEMS
(Figure 6.46)
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CENTER PIVOT IRRIGATION IN ARID AN CLIMATE
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Concrete-lined irrigation ditches and standard sized siphon pipes
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TYPICAL IRRIGATION SCENE IN EARLY SPRING IN THE WESTERN US
Delivery of water to a coarse-textured soil under surface irrigation from gated pipe
Water is siphoned from the ditch into miniponds
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UNEVEN PENETRATION OF WATER FROM THE USE OF A GATED PIPE
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Microirrigation:- most efficient systems used today- drip (trickle), spitters, bubblers- precise placement and amounts- may add soluble fertilizer(fertigation)- capital costs are relatively high- decreases salinity/waterlogged soils probs- useful for residential lawns, decks, etc.
Irrigation water management:- major problem is salinity of soils/water used- need for increasing water-use efficiency- need to use water/landscaping more wisely- reduction of water cost subsidies
IRRIGATION PRINCIPLES & PRACTICES-4
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DRIP OR TRICKLE IRRIGATION WITH A SINGLE EMITTER FOR EACH SEEDLING
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A MICROSPRAYER OR SPITTER IRRIGATING AN INDIVIDUAL TREE IN A HOME GARDEN