where ε = 0.622 (unitless) and yields w in g/kg. This reveals that w is partially dependent on atmospheric pressure, p. What does this formula suggest about the effect of pressure on the actual moisture content at higher elevations?

Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
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where ε = 0.622 (unitless) and yields w in g/kg. This reveals that w is partially dependent on atmospheric pressure, p. What does this formula suggest about the effect of pressure on the actual moisture content at higher elevations?

In the equation presented:

\[ w = \varepsilon \times \frac{e}{p} \]

- \(w\) represents a variable or a rated quantity.
- \(\varepsilon\) (epsilon) is another variable or a parameter in the equation.
- \(e\) is the numerator of the fraction.
- \(p\) is the denominator of the fraction.
- The fraction \(\frac{e}{p}\) indicates division of \(e\) by \(p\).
- The symbol \(\times\) denotes multiplication.

This equation might be used in a context such as physics, engineering, or economics where \(w\) could be a result of some combination of \(\varepsilon\) and the ratio of \(e\) to \(p\).
Transcribed Image Text:In the equation presented: \[ w = \varepsilon \times \frac{e}{p} \] - \(w\) represents a variable or a rated quantity. - \(\varepsilon\) (epsilon) is another variable or a parameter in the equation. - \(e\) is the numerator of the fraction. - \(p\) is the denominator of the fraction. - The fraction \(\frac{e}{p}\) indicates division of \(e\) by \(p\). - The symbol \(\times\) denotes multiplication. This equation might be used in a context such as physics, engineering, or economics where \(w\) could be a result of some combination of \(\varepsilon\) and the ratio of \(e\) to \(p\).
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