How long does a moun live during a measurement

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In summary, a muon with a kinetic energy of 200 ± 0.05 MeV is produced in a linear accelerator. Its rest mass is 106 MeV/c2. The speed of the muon is 0.938c and its linear momentum is 287 MeV/c. The lifetime of the muon is 6.58e-21 seconds and the distance it travels in the laboratory before disappearing is 2e4 meters. Based on measurements of energy, it is better to identify a muon rather than based on measurements of distance because the energy remains constant while the distance can vary depending on the reference frame. The equation that may have caused confusion is the uncertainty principle, which states that the uncertainty in energy
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DODGEVIPER13
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Homework Statement


A muon with a kinetic energy of 200 ± 0.05 MeV
is produced in a linear accelerator. The rest
mass of the muon is 106 MeV/c2.
(a) Calculate the speed of the muon (in units of c),
(b) Calculate the linear momentum (in units of eV/c),
(c) How long does it live during the measurement?
(d) Find the lifetime of the muon.
(e) What is the distance traveled by muon in laboratory
before it disappears (use c = 3 x 108 m/s)? Could
this distance be measured?
(f) For identifying a muon what method do you think
that is better: (1) based on measurements of energy
or (2) based on measurements of distance? Why?

I am having trouble with part c


Homework Equations


(1 stands for naught)
E = E1 + K
deltaE dot deltaT = h (I don't understand this equation)
deltaT = h/deltaE


The Attempt at a Solution


I found this and the solution online I understand part a and b then answers are respectivley v=.938c and p=287MeV/c. It is part c that I am struggling with this is what my instructor does he says deltaE dot deltaT = h which isn't on my equation sheet so I am not sure about this. Then he states E = K + E1 remains constant, then sets deltaE=deltaK = .1MeV I think I understand where he got the equality part and I think I get how he got .1 I assume he did this .05-(-.05) = .1 = deltaK = deltaE. But I am not sure as to why he did this. Then deltaT = h/deltaE = (6.58e-16 eV.s)/(1e5 eV) = 6.58e-21s. How the heck did he obtain 6.58e-16 I am confused?
 
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  • #2
Ouch! no replies yet very weird I guess maybe I was confusing or something.
 
  • #3
The equation you don't understand seems to be the uncertainty principle for energy and time.
 
  • #4
lol after looking up the uncertainty principle I agree that's what it is but I really need to know where the .1 and 6.58e-16 came from?
 
  • #5
.1 comes from the uncertainty of energy. 6.58e-16 is Planck's constant in eV.s.
 

FAQ: How long does a moun live during a measurement

How long does a mountain live during a measurement?

The lifespan of a mountain is not measured in terms of time like living organisms. Instead, mountains are considered to be constantly changing and evolving geological features, influenced by factors such as weathering and erosion. Therefore, it is not possible to accurately determine a specific duration for the "life" of a mountain during a measurement.

Can a mountain die during a measurement?

In terms of traditional definitions of life and death, a mountain cannot die. However, it can be significantly altered or destroyed due to natural disasters or human activities. Thus, the concept of "death" is not applicable to mountains.

How do scientists measure the lifespan of a mountain?

Scientists use various methods to study the formation, growth, and erosion of mountains. This includes analyzing the rock layers and structures, studying the movement of tectonic plates, and using geochronological techniques to determine the age of a mountain.

Can the lifespan of a mountain be extended?

Technically, the lifespan of a mountain can be extended through geological processes such as uplift and volcanic activity. However, these changes occur over millions of years, making it difficult to measure any significant extension in the lifespan during a measurement.

Do all mountains have the same lifespan?

No, the lifespan of a mountain can vary greatly depending on its location and geological history. For example, some mountains are formed by volcanic activity and may have shorter lifespans, while others are the result of tectonic collisions and can exist for millions of years.

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