The aim of this investigation is to determine the effect of free and forced convection on the distribution of heat in a fluid.
Azam Mir
31.10.2000
Heat transfer by convection
Aim
The aim of this investigation is to determine the effect of free and forced convection on the distribution of heat in a fluid.
Introduction
Heat transfer by convection in this investigation occurs as a result of heat transferred from a solid surface to a fluid by conduction and then that heat is transferred within the fluid by the movement of exited particles. ‘It is important to note that convection requires mixings of fluid elements, and is not governed by temperature differences.’
(CRCE/Vol.1/ 2000Edt. pg381).
Forced convection is generated using a magnetic stirrer and follower, which produce circulating currents within the water. The currents are formed by water from lower depth, when warmed, expand and rise due to its lower density than its surrounding environment; the empty space is replaced by colder water of higher density.
Attention may be given specifically to the force convection, since we know that when the magnetic follower rotates, it increase’s the velocity within the water, which would evenly spread the heat resulting in a more regular distribution of temperature throughout the beaker of water.
Heat balances were calculated as they indicate the theoretical amount of heat (Qw) required to raise the temperature of the water in the beaker to its final temperature, this would be subtracted from the electrical energy input from the coil heater to give the heat loss.
Method
Note: Do not operate the heating coil in air.
A 5 litre beaker was filled with approximately 4 litres of cold tap water. Then a heating coil rated at 400W/230V was placed above it. The heating coil apparatus contained 3 slots within its base in which 3 thermometers were placed. Thermometer 1 was placed 7cm below water level, thermometer 2, 10cm and thermometer 3 was 17cm respectively. The position of the thermometers and the coil below point of volume of water were also observed which in turn gave the weight (Kg). The temperatures of the 3 distances were measured at 1 minute intervals using a stop watch, until a reading of approximately 50°C was observed.