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A series of problems related to physics and geosciences concepts, focusing on velocity, density, and isostasy. Students are asked to manipulate equations to find solutions for distance, time, mass, volume, and height. Problems include calculating the depth of the ocean, time for contaminants to reach a well, volume of continental crust and outer core, and thickness of continental crust and crust below the mantle.
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Problem 1: Generally, we know the equation for velocity (a rate) to be:
Where v = velocity, d = distance and t = time.
This equation can be rearranged so that you have an equation for distance (d) and time (t).
Use the equations that you manipulated above to solve the following problems:
Problem 2: A wave traveling downward from the surface of the ocean at 1.5 km/sec takes six seconds to reflect off the ocean floor. How deep is the ocean at that site?
Problem 3: Imagine that you are working with Ms. Homeowner to understand the groundwater flow in her area. She is particularly interested in an underground tank that is located 2.6 km from her home. You have measured the velocity of the groundwater to be 0.033 km/day. About how long will it take any contaminants leaking from the tank to reach Ms. Homeowner's well?
Density plays an important role in our understanding of the physical properties of Earth materials. The equation for density is similar to that for velocity and, as such, it can be manipulated so that you can solve for any of the variables involved. The next few problems utilize the equation for density:
which can be shortened to:
Problem 1: Manipulate (rearrange) the density equation (above) to create an equation for mass.
Problem 2: Manipulate the density equation to create an equation for volume.
Use the equations that you manipulated above to solve the following problems:
Problem 3: Continental crust has a density of about 2.75 g/cm^3. What volume would 1000 g ( kg) of continental crust occupy?
Problem 4: The outer core has a density of about 10.5 g/cm^3. What volume would 1000 g (1 kg) of the outer core occupy?
Isostasy is an important concept in the geosciences that is related to density. The concept of isostasy explains why continental crust sits so much higher than oceanic crust. It involves properties of an object like height and density. It also explains why only a portion of an iceberg is visible above water. The following problems involve an equation that is important to understanding the way that continental crust/oceanic crust behave on the Earth. If you need help visualizing the problem, click on the illustration below to see a larger version.
The equation for calculating the height of an object above the "fluid" in which it is floating is:
where:
Htotal = total height of the object ρobject = density of the object of interest (e.g., iceberg, continental crust, etc.)