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Heat Flow is a measure of the amount of heat leaving the rocks of the lithosphere, while seafloor a seabed in the bottom of the ocean. Because all the heat leaves the rocks when at the bottom of an ocean :)
No, this statement is inaccurate. The higher the R-value of insulation, the more resistant it is to heat flow. R-value measures the effectiveness of insulation in resisting heat transfer, with higher values indicating better insulation properties.
Apparently No, heat flow in oceanic crust is higher than continental crust
No, energy does not naturally flow as heat from a lower temperature to a higher temperature. Heat energy always flows from a higher temperature to a lower temperature in accordance with the second law of thermodynamics.
The specific heat of a substance affects the amount of thermal energy required to cool it. Substances with higher specific heat values require more energy to cool down compared to substances with lower specific heat values. This means that substances with higher specific heat values will cool down more slowly than substances with lower specific heat values.
In most realistic situations heat flow can be said to occur from a region of higher temperature to one of lower temperature. As the region of higher temperature loses heat and the other region gains heat their temperatures become closer and the rate of heat flow diminishes. If, however, it can be contrived to maintain the source of heat at a constant temperature and the destination of the heat also at a constant temperature, then the heat will flow between the two at a constant rate, called steady heat flow.
Yes, heat can never flow from a colder object to a hotter object, as stated by the principle that heat can never flow from a lower temperature to a higher temperature.
When both temperatures are the same, heat does NOT flow between objects.
The higher the specific heat of an object, the more energy it requires to change its temperature. Objects with higher specific heat values require more heat input to increase their temperature compared to objects with lower specific heat values.
It is heat transfer at speed higher than 0.3 Mach.
The natural flow of heat is from a higher temperature to a lower temperature. This process occurs through conduction, convection, or radiation, depending on the medium through which the heat is transferring.
True, heat will naturally flow from a higher temperature to a lower temperature. This flow of heat is governed by the second law of thermodynamics, which states that heat will always transfer from a region of higher temperature to a region of lower temperature until thermal equilibrium is reached.