Answer:
I think option d is the answer
Complete Complete
The complete question is shown on the first uploaded image
Answer:
The moment of inertia of the bar about the center of mass is

Explanation:
The free body diagram is shown on the second uploaded image
From the diagram we see that is
The mass of each segment is



The distance from the origin to the center of the segments i.e the center of masses for the individual segments


The resultant center of mass is mathematically evaluated as

The moment of Inertia of each segment of the bar is mathematically evaluated
=
= 
=
According to parallel axis theorem the moment of inertia about the center (
) is mathematically evaluated as


Answer:
Tc = 424.85 K
Explanation:
Given that,





HEAT FLOW Q is

= 47123.88 w per unit length of rod
volumetric heat rate





= 424.85 K
The correct answers are A) determined from the amplitude recorded by a single seismometer. C) represents the amount of energy released. D) uses a logarithmic scale.
The news media often report an earthquake's magnitude on the Richter scale. The following items are characteristics of a Richter earthquake magnitude: determined from the amplitude recorded by a single seismometer, represents the amount of energy released, and uses a logarithmic scale.
When measuring the scale of the magnitude of earthquakes, the Richter scale measures the scale od moderated size earthquakes. It was invented by two United States seismologists: Charles F. Richer and Beno Gutenberg. They developed the measure in California when they were researching from 1927 through 1936, in the Seismological Laboratory of the Carnegie Institution of Washington, in Pasadena, California.
Answer:
V1 = 1.721 * V2
Explanation:
To start with, we assume that both lift forces are equal, such that
L2 = L1
1 is that of the level at 10000 m, and 2 is that of the level at sea level.
Next, we try and substitute the general formula for both forces such that
C(l).ρ1/2.V1².A = C(l).ρ2/2.V2².A
On further simplification, we have
ρ1.V1² = ρ2.V2², making V1 subject of formula, we have
V1 = √(ρ2/ρ1). V2²
Using the values of density for air at 10000 m and at sea level(source is US standard atmosphere), we have
V1 = √(1.225/0.4135) * V2
V1 = √2.9625 * V2
V1 = 1.721 * V2