Soils, Weathering and Ground Water
Steven Dutch, Natural and Applied Sciences,University
of Wisconsin - Green Bay
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- How can rain forests be so lush if the soil is so poor?
- They get nutrients from rain water
- The organisms have evolved to do without soil nutrients
- Human slash-and-burn agriculture returns nutrients to the soil
- The ecosystem is very effective at recycling nutrients
- Which factors enter into soil classification?
- age of the soil
- parent material
- structure of the soil
- climate and drainage
- all the above
- Why small particles weather faster than large ones:
- They have more surface area for chemical reactions
- They can be more easily eaten by soil organisms
- They are easier to break mechanically
- They are made of more soluble minerals
- Which breaks rocks down by prying the grains apart?
- freeze-thaw cycles
- growth of plant roots
- salt crystal growth along shorelines
- hydration of minerals
- all the preceding
- Which of the minerals in Bowen's reaction series is most stable
chemically?
- calcium plagioclase
- biotite
- quartz
- olivine
- pyroxene
- The layers or horizons in a soil profile result mostly from
- successive deposition of layers
- pressure of the overlying soil
- decreasing sunlight with depth
- differences in leaching and deposition with depth
- The most intense chemical weathering would be expected where?
- the Amazon Basin
- the Mojave Desert
- Northern Alaska
- Minnesota
- Manhattan
- We would expect little chemical weathering, but intense frost action here
- the Amazon Basin
- the Mojave Desert
- Northern Alaska
- Minnesota
- Manhattan
- Little chemical weathering, but episodic and violent rainfall with
rapid erosion would be most likely here:
- the Amazon Basin
- the Mojave Desert
- Northern Alaska
- Minnesota
- Manhattan
- Rapid chemical weathering because of acid rain would probably happen where?
- the Amazon Basin
- the Mojave Desert
- Northern Alaska
- Minnesota
- Manhattan
- This area would be characterized by moderate chemical weathering, and frequent but moderate rainfall and
erosion.
- the Amazon Basin
- the Mojave Desert
- Northern Alaska
- Minnesota
- Manhattan
- Most likely to weather rapidly
- granite
- gneiss
- quartzite
- basalt
- Least likely to weather rapidly
- granite
- gneiss
- quartzite
- basalt
- Why clay doesn't weather
- the grains are too large
- it's already chemically stable at
the surface
- it doesn't occur in areas prone to weathering
- it has too many ions
- Mechanical weathering is most likely to occur here:
- a steep, young mountain range
- a gentle, old mountain range
- a delta
- a coastal plain
- Rocks often shatter when they freeze because
- ice crystals are sharp
- ice expands when it freezes
- water becomes more corrosive when it's frozen
- rocks contract when they get cold
- Mechanical weathering is most likely to be dominant in an area
with:
- heat and high humidity
- a great deal of
vegetation
- much available water
-
extensive frost
wedging
- Mass wasting refers to material moved primarily by:
- wind
- running water
- ice
- gravity
- Which is not a sign of soil creep?
- trees bent near the base
- tilted posts and poles
- water seeping from the ground
- deformed rock layers near the surface
- The source of the energy that propels a landslide
- steep slopes
- strain in the rock
- water lubricating the slide
- gravity
- To prevent long-term pollution of ground water, it is most important to
protect:
- The recharge zone
- The area around the
well
- Streams and lakes
- Springs and seeps
- Most of the earth's water is:
- Lakes and rivers
- ground water
- Ocean water
- Glacial ice
- Geysers can be destroyed by:
- Minerals plugging the
conduit of the geyser
- Unusually violent
eruptions
- Both a and b.
- Neither a nor b
- Artesian wells:
- Are always pure
- Cannot be polluted
because they are sealed
- Always flow to the
surface
- None of the above
- Center-pivot irrigation:
- Has made it possible
to farm soils that cannot be conventionally irrigate
- Is causing the
depletion of many aquifers
- Is very distinctive
seen from the air
- All the above
- What percentage of the water used in the United States is provided by
groundwater?
- 50
- 40
- 30
- 20
- 10
- Rapid withdrawal of groundwater can result in:
- a cone of depression
- loss of hydrostatic
pressure
- ground subsidence
- saltwater incursion
- all of these
- What makes rainwater able to dissolve carbonate rocks?
- carbon dioxide in
solution makes the water slightly acid
- Pollutants in the
rainwater makes it alkalin
- It becomes alkaline
in percolating through the soil.
- Dissolved nitrogen
forms diluted nitric acid
- Most of the liquid fresh water on Earth is in
- ground water
- streams
- rivers
- On a geological time scale, lakes are
- very long-lasting
- short-lived
- The water table in a swamp
- is far below the
surface
- is just at the
surface
- is well above the
surface
- has nothing to do
with the swamp
- A well which flows naturally because the water is under pressure:
- aquifer
- artesian
- alkaline
- mineralized
- Excessive pumping of well water can:
- suck salt water into
coastal wells
- cause subsidence
- lower the water table
- all the above
- A landscape which forms as a result of solution of limestone by ground
water:
- karst landscape
- basin-and-range
topography
- stoss-lee topography
- Most likely to produce the deepest lake
- forming a cutoff
meander
- flooding a graben
- a delta blocking a
bay
- a ice block melting
to form a kettle pond
- A few lakes have bottoms which are below sea level. Which kind of lake
is least likely to be in that category?
- an oxbow or cutoff
meander
- a glacially-scoured
lake
- a graben lake
- a caldera or crater
lake
- Which kind of lake is likely to last longest?
- a kettle lake
- a sinkhole lake
- a cutoff meander or
oxbow lake
- a graben lake
- An aquifer is:
- a permeable layer
that transmits water
- a man-made conduit
through which water is carried to places of habitation.
- the place where water
tables intersect the earth's surface
- the zone of the water
table which transmits aerated water
- none of these
- The primary force which is responsible for the downward migration of
groundwater is:
- surface tension
- air pressure
- gravity
- precipitation
- none of these
- Porosity may be defined as:
- the rate of forward
flow of groundwater
- the amount of space
in a body of rock or soil which is filled by mineral grains
- the volume of
interconnecting open areas in a rock body
- This technique has recently made it possible to irrigate and farm land
that formerly could not be irrigated:
- no-till agriculture
- aerial spraying
- gravity-feed
dispersal
- center-pivot-irrigation
- none of these
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Created 29 Dec 1996; Last Update 26 September 2003
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