The boiling point of water can change significantly with altitude, as the following table shows. -What is the atmospheric pressure, in pascals, at the top of Mt. Everest on a day when water boils there at a temperature of 70.0°C?

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The boiling point of water can change significantly with altitude, as the following table shows.

-What is the atmospheric pressure, in pascals, at the top of Mt. Everest on a day when water boils there at a temperature of 70.0°C? 

### Temperature, Vapor Pressure, and Saturation Vapor Density

The table below provides values of temperature in degrees Celsius (°C), vapor pressure in Pascals (Pa), and saturation vapor density in grams per cubic meter (g/m³). These measurements are important for understanding the relationship between temperature and the amount of water vapor the air can hold.

| Temperature (°C) | Vapor Pressure (Pa) | Saturation Vapor Density (g/m³) |
|------------------|---------------------|--------------------------------|
| 60               | 1.99 x 10⁴          | 130                            |
| 70               | 3.12 x 10⁴          | 197                            |
| 80               | 4.73 x 10⁴          | 294                            |
| 90               | 7.01 x 10⁴          | 418                            |
| 95               | 8.59 x 10⁴          | 505                            |
| 100              | 1.01 x 10⁵          | 598                            |
| 120              | 1.99 x 10⁵          | 1095                           |
| 150              | 4.76 x 10⁵          | 2430                           |
| 200              | 1.55 x 10⁶          | 7090                           |
| 220              | 2.32 x 10⁶          | 10200                          |

**Explanation:**

- **Temperature (°C):** The degree of heat present in a substance or object.
- **Vapor Pressure (Pa):** The pressure exerted by a vapor in thermodynamic equilibrium with its condensed phases at a given temperature in a closed system.
- **Saturation Vapor Density (g/m³):** The maximum density of water vapor the air can hold at a given temperature.

This data helps in the prediction and understanding of weather patterns, atmospheric pressure changes, and is crucial in HVAC technologies, meteorology, and environmental sciences. As temperature increases, both vapor pressure and saturation vapor density tend to increase significantly.
Transcribed Image Text:### Temperature, Vapor Pressure, and Saturation Vapor Density The table below provides values of temperature in degrees Celsius (°C), vapor pressure in Pascals (Pa), and saturation vapor density in grams per cubic meter (g/m³). These measurements are important for understanding the relationship between temperature and the amount of water vapor the air can hold. | Temperature (°C) | Vapor Pressure (Pa) | Saturation Vapor Density (g/m³) | |------------------|---------------------|--------------------------------| | 60 | 1.99 x 10⁴ | 130 | | 70 | 3.12 x 10⁴ | 197 | | 80 | 4.73 x 10⁴ | 294 | | 90 | 7.01 x 10⁴ | 418 | | 95 | 8.59 x 10⁴ | 505 | | 100 | 1.01 x 10⁵ | 598 | | 120 | 1.99 x 10⁵ | 1095 | | 150 | 4.76 x 10⁵ | 2430 | | 200 | 1.55 x 10⁶ | 7090 | | 220 | 2.32 x 10⁶ | 10200 | **Explanation:** - **Temperature (°C):** The degree of heat present in a substance or object. - **Vapor Pressure (Pa):** The pressure exerted by a vapor in thermodynamic equilibrium with its condensed phases at a given temperature in a closed system. - **Saturation Vapor Density (g/m³):** The maximum density of water vapor the air can hold at a given temperature. This data helps in the prediction and understanding of weather patterns, atmospheric pressure changes, and is crucial in HVAC technologies, meteorology, and environmental sciences. As temperature increases, both vapor pressure and saturation vapor density tend to increase significantly.
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