For all Geology and geography lovers who have vast interest in Soil Science, try out this quiz. It will gauge how much knowledge you really have about soil. All the best as you challenge yourself.
Clay
Sand
Silt
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Silt
Sand
Clay
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Well structured sand
Clay
Poorly structured sand
Silt
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Silt
Clay
Sand
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Granular
Columnar
Sub-angular blocky
Prismatic
Platy
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Silt
Sand
Clay
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Parson's
Structural
Wavelength
USDA
Munsell
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Clay
Sand
Silt
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Silt
Loam
Sand
Sandy silt
Clay
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Tensiometer
Gravimetric determinations
Gypsum blocks
Neutron scattering
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The organic nature of water
The 107 degree angle in water
Hydrogen bonding
The electronegativity of hydrogen
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Iron
Silt
Humus
Clay
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Is enhanced by the symmetrical nature of the water molecule
Is independent of the matric potential in soils
Involves both adhesion and cohesion
Does not account for unsaturated water movement in soils
Is not involved in the process of water uptake from soils
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Clay
Silt
Sand
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High chromas
Low values
Low chromas
High values
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The physical suitability of a soil or plant growth
Ratio of bulk density to particle density
Micro-aggregates produced as a by-product of tillage
The moisture content at which a soil is best suited for tillage
The bearing strength of a soil under a given downward force
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7.5YR
5YR
10R
10YR
2.5YR
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Wet-dry
Freeze-thaw
Organic secretions
Sodium adsorption
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Clay
Sand
Silt
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Clouds
Soil moisture
Oceans and ice caps
Groundwater
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Tensiometer
Neutron scattering
Gypsum blocks
Gravimetric determinations
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Stabilize macro aggregates
Help to flocculate the soil colloids
Create large channels that enhance water flow and aeration
Are active in the formation of soil crusts
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True
False
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Ammonia
Carbon dioxide
Nitrogen
Methane
Oxygen
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Prismatic structure may be well developed.
The subsoil may have an organic texture.
The water table may be present in the subsoil.
Clay generally promotes free water movement.
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The tube area
The tube radius
The osmotic potential
The matrix potential
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Furrow-dike irrigation
Flood irrigation
Sprinkle irrigation
Drip irrigation
Furrow irrigation
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True
False
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Clay
Compost
Humus
Sand to the soil and mixing it well
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The interaction of clay and silt
The shape of clay particles
The interaction of polyvalent cations and clay platelets
The interaction of sodium and negatively charged clay particles
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The two H atoms are on diametrically opposite ends of the molecule
It has a positive and a negative side
It is held in soils by adhesion but not adsorption
It is attracted to surfaces with negative but not positive charges
The H to O to H angle is approximately 90 degrees.
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Light tillage of the upper centimeter or so of soil
The presence of macropores in the soil
Conventional tillage as a choice compared with conservation tillage
The production of oats rather than wheat
The use of tillage to control weeds
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Use a plastic mulch
Increase soil temperature
Remove excess water
Add organic residues
Use cover crops, especially legumes
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Mass flow
Partial pressure of N2
Dissolution in water
Respiration
Diffusion
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Nitrogen gas
Volume of macropores
Oxygen
Carbon dioxide
Redox potential
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Impossible to calculate from the data given
15mm/day
5mm/day
10mm/day
100mm/day
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-31
0
-1500
-3100
+5
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Organic matter decomposition
Diffusion of oxygen from the soil to the atmosphere
Reaction of oxygen with organic matter
Root respiration
Creation of more macropores
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55 cm
Impossible to calculate from the data given
10 cm
45 cm
50 cm
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Sandy clay
Loam
Sandy loam
Loamy sand
Sandy clay loam
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Clay
Silt loam
Sand
Poorly structured sand
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Macropores
Bulk density
Total porosity
Fineness of texture
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Higher field capacity
Higher clay content
Lower permanent wilting percentage
Larger micro pore space
Higher capacity of the OM to hold water tightly
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7.5YR2/2
2.5YR6/1
7.5YR6/2
10YR5/8
10YR8/4
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Less biota
Less organic matter content
Compaction caused by the weight of overlaying layers
Higher soil chemoentrophothy
Less aggregation
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The use of herbicides to control weeds
The use of drip irrigation for fruit trees
The use of crop residues to reduce evaporation
The use of flood irrigation for forage crops
The use of concrete-lined delivery ditches
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Not influenced appreciably by the force of gravity
Is lower in a sandy soil with 20 percent soil water than in a clay soil with same percentage of moisture
Is little affected by soil solids
Is generally higher than that of pure water outside the soil
Influenced greatly by the content of salts in the soil
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Sandy loam in upper layers with a clay band underneath
Clay texture throughout profile
Sandy loam in upper layers with a layer of coarse gravel underneath
Silt loam in upper layers underlain by a sandy layer
Uniformly textured sandy loam profile
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