  
      
        - Carefully observe the x-axis of the above graph, “Concentration
          of Atomic Oxygen in the Thermosphere”– notice the exponents.
          These numbers are an abbreviated format used for scientific notation.
          An example would be: 102 = 1 x 102 = 10 x 10 = 100. In the table below,
        indicate the actual number represented by the scientific notation.
 
       
      
        
          Scientific 
            Notation 
           | 
          102  | 
          104  | 
          106  | 
          108  | 
          1010  | 
         
        
          Actual 
          Number | 
          100  | 
             | 
             | 
             | 
             | 
         
             
      
        - Study the actual numbers along the x-axis.
 
          Do they
          increase in equal intervals? __________ 
          Is there a pattern to how
          the x-axis numbers increase? ___________ 
          Explain the pattern that you
          observe. 
       
        
        
      
        - The x-axis is a logarithmic scale, which means that each number is
        ten times greater than the one before it. An example would be:
 
	   
        
		
          
            1 x 10 = 10 (101)  
10 x 10 = 100 (102) 
100 x 10 = 1000 (103)  
1000 x 10 = 10000 (104) | 
           
                 
         
        
        
          Logarithmic scales do NOT display equal intervals, as do non-logarithmic
          scales. Carefully observe the diagram below displaying a logarithmic
        scale along the x-axis. 
         
          
        
        The small marks between the numbers 10 and 100 are 20, 30, 40, 50,
        60, 70, 80, and 90 respectively. Notice that they are not evenly spaced.  
        The small marks between the numbers 100 and 1000 are 200, 300, 400,
          500, 600, 700, 800, and 900 respectively.  
        The uneven spacing is because you are working with the logarithmic
      function of these actual numbers not the numbers themselves. For example: 
        
          
            |   | 
            log (10) = 1.00 
            log (20) = 1.30 
            log (30) = 1.48 
            log (40) = 1.60 
            log (50) = 1.70 | 
            	 	 	 
 | 
            log (60) = 1.78 
            log (70) = 1.85 
            log (80) = 1.90 
            log (90) = 1.95 | 
              | 
           
               These numbers would all be placed along the x-axis between
        101 and 102. 
      
        
          |   | 
          log (100) = 2.00 
      log (200) = 2.30 
      log (300) = 2.48 
      log (400) = 2.60 
      log (500) = 2.70 | 
            
               
               
           | 
          log (600) = 2.78 
      log (700) = 2.85 
      log (800) = 2.90 
      log (900) = 2.95 | 
            | 
         
             
      These numbers would all be placed along the x-axis between
        102 and 103. 
        (Notice that numbers after the decimal point display a consistent
      pattern. For example 1.78, 2.78, 3.78, 4.78, etc. will all have a ‘6’ as
      the first digit – 60, 600, 6000, and 60,000 respectively. The number
      before the decimal indicates how many places are present after the first
      digit. For example, 1.78 would start with a ‘6’ and be followed
      by one place = 60. Or 3.78 would start with a ‘6’ and be followed
      by three places = 6000.) 
      
        - Now you try it. For the following logarithm functions of actual numbers,
          give the logarithm number. Try it first WITHOUT using a calculator, and
        then check your work using a calculator.
 
       
      
        
          |   | 
          log (1000) =  | 
           | 
          
           | 
          log (6000) =  | 
           | 
            | 
         
        
          |   | 
          log (2000) =  | 
           | 
            | 
          log (7000) =  | 
           | 
            | 
         
        
          |   | 
          log (3000) = 
            | 
           | 
            | 
          log (8000) = 
            | 
           | 
            | 
         
        
          |   | 
          log (4000) =  | 
           | 
            | 
          log (9000) =  | 
           | 
            | 
         
        
          |   | 
          log (5000) =  | 
           | 
            | 
            | 
            | 
            | 
         
             
      
            
      
        - On the axis below, complete the scale by placing the scientific notation
          numbers in the top boxes and the actual numbers in the bottom boxes.
 
       
        
        
        
     | 
  
  
    
      - Refer to the graph, “Concentration of Atomic Oxygen in
        the Thermosphere” as you complete the following data table.
 
         
    
      
        Height (km) / 
        (% Concentration) 
         | 
        Particle Density (cm-3) of 
        Atomic Oxygen (green line) 
         | 
       
      
        100 / ( 4%) 
         | 
          | 
       
      
        200 / (55%)  
         | 
          | 
       
      
        300 / (79%) 
         | 
          | 
       
      
        400 / (91%)  
         | 
          | 
       
      
        500 / (96%)  
         | 
          | 
       
     
      
        - Using the above data, describe in some detail how the concentration
          of atomic oxygen in the Earth’s thermosphere changes with height.
          Be sure to include actual and/or logarithmic numbers in your description.
 
       
        
        
        
        
        
        
      
        - Consider this: As you go higher in the thermosphere from 100 km to
          500 km, the percentage of atomic oxygen increases from 4% to 96%, but
          the concentration of particle density per cubic centimeter decreases.
          Why do you think this happens?
 
       
        
        
        
        
      You will need to keep this spacing of a logarithmic scale in mind as
        you complete data tables in two other lessons: "Graphs and the Composition
        of  Earth’s Thermosphere" and "Graphs and the Composition
        of  Earth’s Ionosphere". 
         |