After reading the above Part B and making sure you understand Figure 17.4: Question: 1 Briefly summarize the three ways that material is moved by wind and include the percentage of each mode of transportation. Apply What You Learned: Air reacts in a very similar way to the way a fluid reacts. Compare how material moves along a river to how material moves in wind and identify at two or more similarities.

Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
Problem 1LR
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Question

 After reading the above Part B and making sure you understand Figure 17.4:

Question: 1 

  1. Briefly summarize the three ways that material is moved by wind and include the percentage of each mode of transportation.
  2. Apply What You Learned: Air reacts in a very similar way to the way a fluid reacts. Compare how material moves along a river to how material moves in wind and identify at two or more similarities.

 

Sand generally begins to move when the wind achieves a velocity of about 4.5 meters per
second (m/sec), which is equivalent to about 10 miles per hour. At first, sand exhibits a rolling
motion called traction or surface creep. Approximately 25% of total sand transport during
sandstorms occurs by traction. As wind speed increases, grains are lifted into the air by wind
gusts.
Once airborne, sand grains travel downwind and then drop back to the surface several
centimeters from their point of origin. Finer dust particles are lifted from the surface and
suspended in the air at much greater heights than heavier sand grains. With strong winds and
turbulence, sand grains can be lifted as high as 2 meters (~6.5 feet) and travel 10 meters (~32
feet) or more. About 25% of the total sand transport during these events are caused by this
suspension process.
When a settling sand grain impacts the surface, it sends another grain of sand into the air to
travel in the downwind direction in a process called saltation. Watching this process in action
makes sand appear to be bouncing along the surface (Figure 17.4). Saltation accounts for about
50% of sand transport over dunes. Once saltation begins, transport can continue under
somewhat lower wind speeds.
Wind Direction
….
Note that after the impact, sediments are
dislodged and put into motion.
fim.
Transcribed Image Text:Sand generally begins to move when the wind achieves a velocity of about 4.5 meters per second (m/sec), which is equivalent to about 10 miles per hour. At first, sand exhibits a rolling motion called traction or surface creep. Approximately 25% of total sand transport during sandstorms occurs by traction. As wind speed increases, grains are lifted into the air by wind gusts. Once airborne, sand grains travel downwind and then drop back to the surface several centimeters from their point of origin. Finer dust particles are lifted from the surface and suspended in the air at much greater heights than heavier sand grains. With strong winds and turbulence, sand grains can be lifted as high as 2 meters (~6.5 feet) and travel 10 meters (~32 feet) or more. About 25% of the total sand transport during these events are caused by this suspension process. When a settling sand grain impacts the surface, it sends another grain of sand into the air to travel in the downwind direction in a process called saltation. Watching this process in action makes sand appear to be bouncing along the surface (Figure 17.4). Saltation accounts for about 50% of sand transport over dunes. Once saltation begins, transport can continue under somewhat lower wind speeds. Wind Direction …. Note that after the impact, sediments are dislodged and put into motion. fim.
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