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+273.15K = °C + 273.15
    • Celsius to Fahrenheit: °F=(°C×95)+32°F = (°C \times \frac{9}{5}) + 32
    • Fahrenheit to Celsius: °C=(°F32)×59°C = (°F - 32) \times \frac{5}{9}

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

  • Used to measure heat.

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
    • Reliability: ~75%

Changes in Temperature

  • Heat energy must be added or removed to change an object's temperature.
  • The rise in temperature (ΔT\Delta T) 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=mcΔTQ = mc\Delta T

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:
    • Steel: 0.45

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=8020=60°C\Delta T = 80 - 20 = 60°C
    • Q=3×4200×60=7.56×105JQ = 3 \times 4200 \times 60 = 7.56 \times 10^5 J

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=kAΔTLH_{cd} = \frac{kA\Delta T}{L}
    • HcdH_{cd}: Rate of heat transfer by conduction
    • kk: Thermal conductivity of the material (W/m.K)
    • AA: Cross-sectional area (m²)
    • ΔT\Delta T: Temperature difference (K)
    • LL: 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=0.023Js1m1K1k_{air} = 0.023 J s^{-1} m^{-1} K^{-1}
    • kwater=0.56Js1m1K1k_{water} = 0.56 J s^{-1} m^{-1} K^{-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=hAΔTq = hA\Delta T
    • qq: Rate of convective heat flow
    • hh: Convective heat transfer constant (depends on shape, orientation, surface; for humans, approximately 7.1 W m⁻² K⁻¹)
    • AA: Surface area
    • ΔT\Delta T: 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(T4T04)P = e\sigma A(T^4 - T_0^4)
    • PP: Net radiated power
    • ee: Emissivity (0 = bad, 1 = perfect)
    • σ\sigma: Stefan’s constant = 5.7 x 10⁻⁸ W m⁻² K⁻⁴
    • AA: Surface area
    • TT: Temperature of the object in Kelvin
    • T0T_0: Temperature of the surroundings in Kelvin