Specific heat of air is 0.24 BTU/lb/degree F
the formula to find specific heat is specific heat= calories/mass X change in temperature.
Use the equation for specific heat: energy = mass x (temperature difference) x (specific heat). Replace the numbers you know, and solve for mass. Since it seems that the specific heat is specified per gram, you'll initially get the mass per gram. Converting that to kilograms is quite easy.
The Specific Heat Capacity of water is 4,184 Joules per kg per Kelvin
Specific heat is dimensionless, and dimensionless units have the same value in any system. Specific heat is the ratio between two densities - that of the substance considered, and that of water. The ratio of two quantities of the same dimension will naturally be a dimensionless number.
The amount of heat in air is measured using the specific heat capacity of air, which is about 1 kJ/kg°C. The total heat in air can be calculated by multiplying the specific heat capacity with the mass of air and the change in temperature.
Specific heat of air is 0.24 BTU/lb/degree F
The specific heat of water is greater than the specific heat of air.
The specific heat of air at 450oC as an ideal gas is: 1.081 kJ/(Kg∙K)
The value of the specific heat ratio (gamma) in air is approximately 1.4 at room temperature. It represents the ratio of specific heats, which is the ratio of the heat capacity at constant pressure to the heat capacity at constant volume.
Soil heats up faster than air because it has a higher heat capacity, meaning it can store more heat energy. This allows soil to absorb heat more rapidly from the sun compared to air. Once heated, soil can also retain heat for longer periods of time than air.
1000 J /kg-K
Because the specific heat of water is very high. In fact, water has about 1400 times more heat carrying capacity than air.
absorb or release small amounts of heat, changing its temperature dramatically.
The high specific heat of water means that it can absorb and release a large amount of heat without its temperature changing much. This helps moderate the temperature of the air near the seashore, leading to the formation of convection currents as warm air rises over the warmer water and cooler air moves inland to replace it.
Water has a high specific heat capacity compared to air, meaning it can absorb or release a lot of heat energy before its temperature changes significantly. This property allows water to maintain a relatively stable temperature compared to air, which has a lower specific heat capacity and can heat up or cool down more quickly.
For an adiabatic process, we have the equation PV^1.3 = constant, where P is the pressure and V is the volume. Specific heat at constant pressure (Cp) can be found using the relation Cp - Cv = R, where R is the gas constant. Specific heat at constant volume (Cv) is dependent on the specific gas and temperature range.