The factor of volume of air got increased when it is taken from earth’s surface to the stratosphere has to be calculated Concept Introduction: Combined Gas Law : Boyle’s law: V α 1 P (at constant T) P f V f = P i V i (at constant T) Charles’s law: V α T (at constant P) V f T f = V i T i (at constant P) The boyle’s law and charles’s law is combined and stated as “the volume (V) of a given gas is directly proportional to temperature (T) and inversely proportional to pressure (P)” V α T P For a sample of gas supposing a change in temperature, volume and pressure, the combined gas law can be written as P f V f T f = P i V i T i On rearranging, we get V f = V i × P i P f × T f T i Where, T i a n d T f are initial temperature and final temperature respectively V i a n d V f are initial volume and final volume respectively P i a n d P f are initial pressure and final pressure respectively
The factor of volume of air got increased when it is taken from earth’s surface to the stratosphere has to be calculated Concept Introduction: Combined Gas Law : Boyle’s law: V α 1 P (at constant T) P f V f = P i V i (at constant T) Charles’s law: V α T (at constant P) V f T f = V i T i (at constant P) The boyle’s law and charles’s law is combined and stated as “the volume (V) of a given gas is directly proportional to temperature (T) and inversely proportional to pressure (P)” V α T P For a sample of gas supposing a change in temperature, volume and pressure, the combined gas law can be written as P f V f T f = P i V i T i On rearranging, we get V f = V i × P i P f × T f T i Where, T i a n d T f are initial temperature and final temperature respectively V i a n d V f are initial volume and final volume respectively P i a n d P f are initial pressure and final pressure respectively
Solution Summary: The author explains that the factor of volume of air got increased when it is taken from earth’s surface to the stratosphere has to be calculated.
Author: Steven D. Gammon, Ebbing, Darrell Ebbing, Steven D., Darrell; Gammon, Darrell Ebbing; Steven D. Gammon, Darrell D.; Gammon, Ebbing; Steven D. Gammon; Darrell
Definition Definition Any of various laws that describe the ways in which volume, temperature, pressure, and other conditions correlate when matter is in a gaseous state. At a constant temperature, the pressure of a particular amount of gas is inversely proportional with its volume (Boyle's Law) In a closed system with constant pressure, the volume of an ideal gas is in direct relation with its temperature (Charles's Law) At a constant volume, the pressure of a gas is in direct relation to its temperature (Gay-Lussac's Law) If the volume of all gases are equal and under the a similar temperature and pressure, then they contain an equal number of molecules (Avogadro's Law) The state of a particular amount of gas can be determined by its pressure, volume and temperature (Ideal Gas law)
Chapter 5, Problem 5.110QP
Interpretation Introduction
Interpretation:
The factor of volume of air got increased when it is taken from earth’s surface to the stratosphere has to be calculated
Concept Introduction:
Combined Gas Law:
Boyle’s law:
Vα1P (at constant T)
PfVf=PiVi (at constant T)
Charles’s law:
Vα T (at constant P)
VfTf=ViTi (at constant P)
The boyle’s law and charles’s law is combined and stated as “the volume (V) of a given gas is directly proportional to temperature (T) and inversely proportional to pressure (P)”
VαTP
For a sample of gas supposing a change in temperature, volume and pressure, the combined gas law can be written as
PfVfTf=PiViTi
On rearranging, we get
Vf=Vi×PiPf×TfTi
Where,
Tiand Tf are initial temperature and final temperature respectively
Viand Vf are initial volume and final volume respectively
Piand Pf are initial pressure and final pressure respectively
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