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  1. Heat • The temperature difference determines the direction of heat transfer. • Bodies don’t “contain” heat; heat always refers to energy in transit from one body to another. • We can change the temperature of a body by adding heat to it.

  2. The Higher Heating Value (HHV), also known as the Gross Calorific Value or Higher Calorific Value, is determined when the water of combustion is entirely condensed and that the heat contained in the water vapor is recovered.

  3. In the next 3 weeks, we’ll talk about the heat equation, which is a close cousin of Laplace’s equation. In fact, both of them share very similar properties Heat Equation: u t= u 1. Derivation of the Heat Equation Reading: Physical Interpretation of the heat equation (page 44) The derivation of the heat equation is very similar to the ...

  4. LECTURE 7: HEAT EQUATION AND ENERGY METHODS Readings: Section 2.3.4: Energy Methods Convexity (see notes) Section 2.3.3a: Strong Maximum Principle (pages 57-59) This week we’ll discuss more properties of the heat equation, in partic-ular how to apply energy methods to the heat equation. In fact, let’s start with energy methods, since they ...

  5. The rate of heat transfer [J/s] through a thin slab of homogeneous material of thicknes xand area Awith one face held at a constant temperature T and the other at a somewhat higher constant temperature T+ Tis:

  6. Thermodynamics is the study of how heat moves around in ‘macroscopic’ objects.

  7. This short note aims to define and clarify the different uses of four most commonly used heating value terms, which are high heating value (HHV) or gross calorific value (GCV), low heating value (LHV), gross heating value (GHV) and net calorific value or net heating value (NCV or NHV), in the context of biomass fuels.

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