c = Q / (m(change in temperature))
Where,
c = specific heat capacity
Q = amount of heat needed
m = mass
Change in temperature = initial temperature - temperature(after)
Take note that this equation cannot be used in calculating the change in state - melting and boiling
Because temperature do not change.
We therefore use:
Q = lv x m
Where,
lv = latent heat of vapourisation (for boiling/condensation ONLY)
m = mass
Q = lf x m
Where,
lf = latent heat of fusion (for melting/freezing ONLY)
You can calculate the outlet temperature of two fluids in a heat exchanger using the energy balance equation, which equates the heat gained by one fluid to the heat lost by the other fluid. By applying this equation along with the specific heat capacities and flow rates of the fluids, you can determine the outlet temperatures. Alternatively, software tools or online calculators can be used to simplify the calculation process.
If you know the temperature and mass of an object, and the temperature, mass, and specific heat of the water, if you dunk the object in the water, and measure the temperature of the water and the object (once the object and water have the same temperature), using reasoning skills and/or equations you can figure out the specific heat of the object. Historically the specific heat was related to SH of water . Water being 1 That now is seen as archaic. The specific heat (of a substance) is the amount of heat per unit mass required to raise the temperature by one degree Celsius. This does not apply if a phase change is encountered. Every substance has to be measured separately .
To find the heat gained in a specific heat problem, you can use the formula: Q = mcΔT, where Q is the heat gained, m is the mass of the substance, c is the specific heat capacity of the substance, and ΔT is the change in temperature. Simply plug in the values for mass, specific heat capacity, and temperature change to calculate the heat gained.
To calculate the amount of heat gained by the water when the temperature changes by 15 degrees Celsius, you can use the formula: Q = mcΔT, where Q is the heat gained, m is the mass of water, c is the specific heat capacity of water (4.18 J/g°C), and ΔT is the temperature change (15°C).
To calculate the calorimeter constant, you first need to use the formula for heat transfer: q=mcΔT, where q is the heat transfer, m is the mass, c is the specific heat capacity, and ΔT is the change in temperature. Since the two water samples reached thermal equilibrium, the heat lost by the hot water is equal to the heat gained by the cold water. By rearranging the equation to find the calorimeter constant, you can solve for it using the given data.
The thermal energy equation in physics is Q mcT, where Q represents the amount of thermal energy, m is the mass of the object, c is the specific heat capacity of the material, and T is the change in temperature. This equation is used to calculate the amount of thermal energy in a system by multiplying the mass of the object by the specific heat capacity of the material and the change in temperature.
You can calculate the outlet temperature of two fluids in a heat exchanger using the energy balance equation, which equates the heat gained by one fluid to the heat lost by the other fluid. By applying this equation along with the specific heat capacities and flow rates of the fluids, you can determine the outlet temperatures. Alternatively, software tools or online calculators can be used to simplify the calculation process.
Some factors that affect heat gained or lost include the temperature difference between an object and its surroundings, the surface area of the object, the material of the object, and the thermal conductivity of the material. Additionally, factors such as the duration of thermal exposure and external forces like wind or insulation can influence heat transfer.
The constant specific heat equation is used in thermodynamics to calculate the amount of heat transferred during a process when the specific heat of a substance remains constant.
The specific heat capacity of the material the object is made of. The mass of the object. The temperature change experienced by the object.
The thermal equation used to calculate heat transfer in a system is Q mcT, where Q represents the amount of heat transferred, m is the mass of the substance, c is the specific heat capacity of the substance, and T is the change in temperature.
The key heat formulas in physics are the heat transfer equation, the specific heat capacity equation, and the thermal energy equation. These formulas are used to calculate heat transfer and temperature changes in various systems by taking into account factors such as the amount of heat transferred, the specific heat capacity of the material, and the initial and final temperatures of the system.
If you know the temperature and mass of an object, and the temperature, mass, and specific heat of the water, if you dunk the object in the water, and measure the temperature of the water and the object (once the object and water have the same temperature), using reasoning skills and/or equations you can figure out the specific heat of the object. Historically the specific heat was related to SH of water . Water being 1 That now is seen as archaic. The specific heat (of a substance) is the amount of heat per unit mass required to raise the temperature by one degree Celsius. This does not apply if a phase change is encountered. Every substance has to be measured separately .
The heat capacity equation is Q mcT, where Q represents the amount of heat energy, m is the mass of the substance, c is the specific heat capacity of the substance, and T is the change in temperature. This equation is used to calculate the amount of heat required to change the temperature of a substance by multiplying the mass, specific heat capacity, and temperature change.
To calculate the number of joules of heat gained by water, you can use the formula Q = m * c * ΔT, where Q is the heat gained, m is the mass of water in grams, c is the specific heat capacity of water (4.18 J/g°C), and ΔT is the change in temperature in degrees Celsius. Plug in the values for m, c, and ΔT to calculate the heat gained in joules.
The heat dissipation equation used to calculate the amount of heat transferred from a system to its surroundings is Q hAT, where Q represents the amount of heat transferred, h is the heat transfer coefficient, A is the surface area through which heat is transferred, and T is the temperature difference between the system and its surroundings.
When allowed to stand for long enough, the final temperature will reach room temperature.