Heat and Heat Transfer Notes
Heat & Temperature Scales
- Temperature and heat are distinct concepts.
- Temperature determines the direction of heat flow when objects are in thermal contact; heat flows from high to low temperature.
Temperature Scales
- SI Scale: Kelvin (K)
- Common Scale: Celsius (°C), widely used, including in clinical settings.
- Celsius Scale:
- 0°C: Freezing point of water at Standard Temperature and Pressure (STP)
- 100°C: Boiling point of water at STP
- Conversions:
- Celsius to Kelvin: K=°C+273.15
- Celsius to Fahrenheit: °F=(°C×59)+32
- Fahrenheit to Celsius: °C=(°F−32)×95
Fahrenheit Scale Usage
- Used in:
- U.S.
- Marshall Islands
- Liberia
- Jamaica
- Belize
Absolute Zero
- Charles’ Law: Volume of an ideal gas is directly proportional to absolute temperature at constant pressure.
- Extrapolation to -273.15°C on a volume vs. temperature graph.
- Absolute Zero: -273.15°C, the starting point of the Kelvin scale.
Temperature Measurement
Thermometers
- Used to measure temperature.
- Calibrated to a reference material via its thermometric property.
- Example: Mercury thermometer uses thermal expansion of mercury.
- Change in mercury column height indicates temperature change.
Calorimeters
Thermometric Property
- Physical property of a substance that changes uniformly (not necessarily linearly) and predictably with temperature.
- Examples:
- Volume
- Color
- Electrical resistance or voltage
- Pressure
Types of Thermometers
- Mercury/Alcohol thermometer
- Thermocouple: Measures resistance of two different metals
- Gas-filled bulb thermometer
- Liquid crystal thermometer: Measures color change of crystals
Thermometer Function
- Mercury or alcohol expands when heated.
- Expansion is linear within a specific temperature range.
- After calibration, the thermometer can accurately measure temperature.
Human Body Temperature
- Core body temperature: Approximately 37°C (98.6°F).
- Temperature varies at extremities.
Body Temperature Variation
- Oral cavity: 0.4°C lower than core temperature.
- Rectum: 0.3°C higher than core temperature.
- Armpit (axilla): 0.9°C lower than core temperature.
Factors Affecting Body Temperature
- Hard exercise
- Hard work
- Emotion
- Age
- Time of day
- Smoking
- Hot/cold drinks
- Hormones
- Menstrual cycle: Used in the Rhythm Method of birth control
Changes in Temperature
- Heat energy must be added or removed to change an object's temperature.
- The rise in temperature (ΔT) depends on:
- Quantity of heat added (Q)
- Mass (m)
- Specific heat capacity (c)
Specific Heat Capacity (SHC)
- Amount of heat energy required to raise the temperature of 1 kg of a substance by 1 Kelvin.
- Units: J kg⁻¹ K⁻¹
- Formula: Q=mcΔT
Water's High SHC
- Water has a very high SHC value.
- The human body has a high water content, resulting in high thermal inertia (resistance to temperature change).
- Example Specific Heat Capacity:
Example Calculation
- Problem: How much heat energy is required to raise the temperature of 3L of water from 20 to 80°C? (SHC of water = 4200 J/kg.K)
- Solution:
- m = 3 kg (1L of water = 1 kg)
- ΔT=80−20=60°C
- Q=3×4200×60=7.56×105J
Heat Transfer
- Heat flows from one object to another via three methods:
- Radiation: Does not require a medium
- Convection: Occurs in liquids and gases
- Conduction: Occurs in solids
Conduction
- Heat transfer by direct contact.
- Formula: Hcd=LkAΔT
- Hcd: Rate of heat transfer by conduction
- k: Thermal conductivity of the material (W/m.K)
- A: Cross-sectional area (m²)
- ΔT: Temperature difference (K)
- L: Length of the material (m)
Thermal Conductivity Examples
- Air vs. Water:
- Air feels colder than water at 0°C due to differences in thermal conductivity.
- kair=0.023Js−1m−1K−1
- kwater=0.56Js−1m−1K−1
- Water is 24 times better at conducting heat than air.
- Air is a good insulator.
Insulation Examples
- Arctic Fox: Winter coat has a larger volume for better insulation.
- Reindeer (Caribou): Hair follicles are hollow, trapping insulating air.
- String Vests: Air in the holes provides insulation; air is a better insulator than cotton.
Convection
- Heat transfer in fluids (liquids or gases).
- Heated fluid becomes less dense and rises.
- Cooler, denser fluid sinks to replace it, creating convection cells.
Convection Examples
- Solar Surface: Convection cells are visible.
- Tectonic Plates: Geo-thermal convection drives their movement.
Rate of Convective Heat Flow
- Formula: q=hAΔT
- q: Rate of convective heat flow
- h: Convective heat transfer constant (depends on shape, orientation, surface; for humans, approximately 7.1 W m⁻² K⁻¹)
- A: Surface area
- ΔT: Temperature difference
Wind-Chill
- Convection causes wind-chill: moving cold air cools you down.
Fan Oven Effect
- Moving hot air will cause the food/substance/person to heat up more quickly.
- If T > 37°C, and there is no air conditioning, fans can cause fatalities in heatwaves by increasing convection.
Radiation
- Heat transfer that does not require a medium.
- Relies on photons, so it can occur across a vacuum.
- Formula: P=eσA(T4−T04)
- P: Net radiated power
- e: Emissivity (0 = bad, 1 = perfect)
- σ: Stefan’s constant = 5.7 x 10⁻⁸ W m⁻² K⁻⁴
- A: Surface area
- T: Temperature of the object in Kelvin
- T0: Temperature of the surroundings in Kelvin