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SWS 3022 Exam 2 Questions with Answers

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  • Course
  • SWS 3022
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  • SWS 3022

SWS 3022 Exam 2 Questions with Answers Know that primary minerals dominate the sand and silt fractions, while secondary minerals dominate the clay fraction. Also, know the basic difference in reactivity of primary vs. secondary minerals. - Answer-Primary= less reactive Know how texture generall...

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  • August 6, 2024
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  • 2024/2025
  • Exam (elaborations)
  • Questions & answers
  • SWS 3022
  • SWS 3022
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SWS 3022 Exam 2 Questions with
Answers

Know that primary minerals dominate the sand and silt fractions, while secondary
minerals dominate the clay fraction. Also, know the basic difference in reactivity of
primary vs. secondary minerals. - Answer-Primary= less reactive

Know how texture generally affects overall porosity and pore size distribution. - Answer-
Larger particles-> large pores, low porosity
Clay- high water retention

Know generally how texture affects water and gas movement in soils. - Answer-Course
texture- easier path, less contact time
Fine texture- more convoluted path, more contact time

Be able to use the soil textural triangle. Know the number of textural classes,
Understand the general trends in the triangle. - Answer-12 textural classes
Clay at top takes up most, sand to left, silt to right

Understand the relationship between soil texture and specific surface area; why is it
important? - Answer-Finer soils have higher specific surface area
Sand SSA- 444
Silt- 100,000
Clat- 7,000,000

Understand what Stokes' Law indicates and how it is used in the hydrometer method to
assess soil texture. - Answer-Stokes law allows determination of the
time required for different particle size
separates to settle from a suspension

Understand the hydrometer method and how to calculate % sand, silt, and clay given
appropriate measurements. - Answer-Hydrometer measures in g/L

Know the numerical value for soil particle density. - Answer-2.65 g/cm cubed

Know how to compute soil bulk density and what it is. - Answer-Mass oven dried soil
divided by volume of soil
Density of soil including the
particles and the pore spaces

, Know the range in bulk densities for a typical mineral soil containing approximately 1-
5% organic matter. - Answer-1-1.6 g/cm cubed

Know how organic matter, aggregation, compaction, and depth in profile affect porosity
and bulk density. - Answer-Organic soils have a lower bulk density, high porosity
Aggregation- low bulk density, increases porosity
Compaction- decreases porosity, increases bulk density
Depth- compacted, low organic matter, fewer roots, high bulk density, decrease porosity

Know the conceptual and quantitative relationship between BD and porosity. - Answer-
When porosity declines, BD increases because there is a greater mass of soil particles
for a given volume.
Quantitative- Porosity= 1-BD/PD= Volume of pores/Volume of soils

Understand the difference between total porosity and pore size distribution. - Answer-
Total porosity indicates the maximum volume
of water and gases a soil can hold
Pore size distribution- diameters of pore
macro pores- >/08 mm
Meso pores- .08-.03mm
Micropores -.03-.005 mm

Understand basically how differences in density and texture impact water and gas
movement and chemical properties of soils. - Answer-Lower diameter, slower water
movement

Know what soil structure is and how it affects soil porosity and pore size distribution. -
Answer-Arrangement of grouping of individual soil particles into secondary units.
(aggregates)
Interaggregate- porosity btwn aggregates, larger diameters, drains rapidly
Intraaggregate- within aggregate, small diameters, strong capillary forces, retain water
well

Know the boiling and freezing point of water. - Answer-100 degrees Celsius and 0
degrees Celsius

Know the dimensions of the earth. - Answer-Diameter: 8,000 mi
Circumference: 25,000 mi

Understand that definitions of soil depend strongly on the concerns of those making the
definitions - Answer-

Know the parameters related to soil composition for an idealized surface soil. - Answer-
Reactive and porous
45% mineral particles
5% organic matter

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