Hukum I Termodinamika
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Transcript of Hukum I Termodinamika
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Hukum I Termodinamika
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First Law of Thermodynamics
The first law of thermodynamics is the application of the conservation of energy principle to heat and thermodynamic processes:
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1. System Work
When work is done by a thermodynamic system, it is usually a gas that is doing the work.
For non-constant pressure, the work can be visualized as the area under the pressure-volume curve which represents the process taking place.
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Usaha yang dilakukan oleh gas pada tekanan konstan ( isobarik)
Usaha yang dilakukan oleh gas pada volume konstan (isokhorik)
P
V
2
1
0V
V
PdVW
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2. Tenaga Internal
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3. Kalor ( Panas )
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Specific Heat
The relationship does not apply if a phase change is encountered, because the heat added or removed during a phase change does not change the temperature.
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Transfer kalor
Konduksi
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Konveksi
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Radiasi
the net radiation loss rate takes the form
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Persamaan Perbedaan panas dan tahanan termal
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Cooling of the Human Body
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Heating of the Human Body
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Greenhouse Effect
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• Contributers to Greenhouse Effect
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Proses Adiabatik
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Saturated Vapor Pressure The process of evaporation in a closed container will proceed until there are as many molecules returning to the liquid as there are escaping. At this point the vapor is said to be saturated, and the pressure of that vapor (usually expressed in mmHg) is called the saturated vapor pressure.
Since the molecular kinetic energy is greater at higher temperature, more molecules can escape the surface and the saturated vapor pressure is correspondingly higher. If the liquid is open to the air, then the vapor pressure is seen as a partial pressure along with the other constituents of the air. The temperature at which the vapor pressure is equal to the atmospheric pressure is called the boiling point.
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Evaporation Ordinary evaporation is a surface phenomenon - some molecules have enough kinetic energy to escape. If the container is closed, an equilibrium is reached where an equal number of molecules return to the surface. The pressure of this equilibrium is called the saturation vapor pressure.
In order to evaporate, a mass of water must collect the large heat of vaporization, so evaporation is a potent cooling mechanism. Evaporation heat loss is a major climatic factor and is crucial in the cooling of the human body.
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Boiling Point
The boiling point is defined as the temperature at which the saturated vapor pressure of a liquid is equal to the surrounding atmospheric pressure. For water, the vapor pressure reaches the standard sea level atmospheric pressure of 760 mmHg at 100°C. Since the vapor pressure increases with temperature, it follows that for pressure greater than 760 mmHg (e.g., in a pressure cooker), the boiling point is above 100°C and for pressure less than 760 mmHg (e.g., at altitudes above sea level), the boiling point will be lower than 100°C. As long as a vessel of water is boiling at 760 mmHg, it will remain at 100°C until the phase change is complete. Rapidly boiling water is not at a higher temperature than slowly boiling water. The stability of the boiling point makes it a convenient calibration temperature for temperature scales.
At the boiling point,saturated vapor pressure equals atmospheric pressure.
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Evaporation vs Boiling Ordinary evaporation is a surface phenomenon - since the vapor pressure is low and since the pressure inside the liquid is equal to atmospheric pressure plus the liquid pressure, bubbles of water vapor cannot form. But at the boiling point, the saturated vapor pressure is equal to atmospheric pressure, bubbles form, and the vaporization becomes a volume phenomena.
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