Sea water's density can be calculated as a function of the compressibility, b, where p = po exp[(p - patm)/b]. calculate the pressure and density 10,000 m below the surface of the sea. assume ß = 200 mega pa.

The pressure 10,000 m below the surface of the sea is 137.14 MPa.

The density 10,000 m below the surface of the sea is 2039 kg/m3

Explanation:

P0 and ρ0 are the pressure and density at the sea level (atmosferic condition). As the depth of the sea increases, both the pressure and the density increase.

We can relate presure and density as:

Rearranging

With this equation, we can calculate P at 10,000 m below the surface:

The density at 10,000 m below the surface of the sea is

here is table 2-2:

country

percent of eligible voters that voted

rank

united states

44.9%

138

canada

60.1%

107

costa rica

84.6%

14

hungary

66.9%

82

japan

57.0%

118

egypt

27.7%

159

south africa

85.5%

10

ans is no, the data set cannot be plotted as a single circle graph