nycgirl212
Which of the following most logically completes the argument below?
Within the earth's core, which is iron, pressure increases with depth. Because the temperature at which iron melts increases with pressure, the inner core is solid and the outer core is molten. Physicists can determine the melting temperature of iron at any given pressure and the pressure for any given depth in the earth. Therefore, the actual temperature at the boundary of the earth's outer and inner cores—the melting temperature of iron there—can be determined, since_______.
(A) the depth beneath the earth's surface of the boundary between the outer and inner cores is known
(B) some of the heat from the earth's core flows to the surface of the earth
(C) pressures within the earth's outer core are much greater than pressures above the outer core
(D) nowhere in the earth's core can the temperature be measured directly
(E) the temperatures within the earth's inner core are higher than in the outer core
Take some simplistic numbers.
Earth's core is made of iron.
- Pressure increases with depth so say at the surface of the core, the pressure is 1 pascal, then as you go inside at 10 m depth, pressure increases to 2 pascal and so on.
- Temperature at which iron melts increases with pressure. If pressure is higher, melting point is higher. So say at 1 pascal, melting point of iron is 100 degree C and at 1 pascal, the melting point is 110 degree Celsius. If the temperature of the entire core is same say 105 degree celsius, then iron at the surface will be melted while iron at 10 m depth will be solid.
- So the inner core is solid and the outer core is molten (Earth's core has two regions - inner and outer core. Because pressure at the inner core is higher, the melting point of iron is higher there. That temperature is not reached and hence the inner core is solid. The outer core has lower pressure and hence melting point is lower there. That temperature is reached and hence iron is in molten form there)
- We know the pressures at different depths and all melting points of iron.
So we can determine the actual temperature at the boundary of the earth's outer and inner cores .. (Here they are talking about the boundary of the two regions where outer core ends and inner core begins. At that point, there would be some temperature. That is the transition pressure - as it reduces toward outer core, iron melts at that temperature. As pressure increases toward inner core, iron does not melt)
How can we determine the temperature at that boundary? The temperature there is the melting point of iron at the pressure there. If we know the pressure there, we can find what temperature is there.
How can we find the pressure there? We know the pressures at various depths. So if we know the depth of the boundary of inner and outer core, then we can find the pressure there. Based on the pressure there, we know the melting point of iron. So temperature there would be the melting point of iron at that pressure.
That is why option (A) is correct.
We can determine the actual temperature at the boundary if we know the depth of the boundary.
None of the other options even talk about the boundary.