If you have a discontinuity and you can cancel factors in the numerator and the denominator, then it is removable. If you can't cancel those factors to get rid of the discontinuity it is nonremovable. Here is an example that shows both kinds.
f(x) = (x - 2)(x + 3) /[(x - 2) (x - 4)
There is a discontinuity at x=2 but we can cancel out(x-2) from the top and bottom.
That makes it removable. However, at x=4 there also a discontinuity and there is no way to remove that one.
"Removable discontinuity" means the function is not defined at that point (it has a "hole"), but by changing the function definition at that single point, defining it to be certain value, it becomes continuous. "Irremovable discontinuity" means the function makes a sudden jump at that point. There are infinitely many functions like that; for example, you can set the function to be: f(x) is undefined at x = -2 f(x) = 0 for x < 2 (except for x = -2) f(x) = 1 for x > 2
Don't hand that holier than thou line to me
Limitations of Regular falsi method: Investigate the result of applying the Regula Falsi method over an interval where there is a discontinuity. Apply the Regula Falsi method for a function using an interval where there are distinct roots. Apply the Regula Falsi method over a "large" interval.
Well, honey, a point of discontinuity is not the same as a critical point in calculus. A critical point is where the derivative is either zero or undefined, while a point of discontinuity is where a function is not continuous. So, in short, they may both be important in their own ways, but they're not the same thing.
Yes, a Fourier series can represent a function that is discontinuous. While the series converges to the function at points of continuity, at points of discontinuity, it converges to the average of the left-hand and right-hand limits. This phenomenon is known as the Gibbs phenomenon, where the series may exhibit oscillations near the discontinuities. Despite these oscillations, the Fourier series still provides a useful approximation of the function.
It is the word removable with the prefix 'un' meaning not. unremovable = not removable
your system's BIOS is stored on an unremovable chip on your computer's motherboard. your system's BIOS is stored on an unremovable chip on your computer's motherboard. your system's BIOS is stored on an unremovable chip on your computer's motherboard. your system's BIOS is stored on an unremovable chip on your computer's motherboard. your system's BIOS is stored on an unremovable chip on your computer's motherboard. your system's BIOS is stored on an unremovable chip on your computer's motherboard. it is permanently stored on one or two ROM ICs installed on the system board
The Discontinuity Guide was created in 1995.
The Discontinuity Guide has 357 pages.
The Mohorovičić Discontinuity, also called the Moho Discontinuity, was named for Andrija Mohorovičić, the Croatian seismologist who first identified it in 1909.
The unscrambled word is discontinuity.
The ISBN of The Discontinuity Guide is 0-426-20442-5.
The two layers of discontinuity in Earth's interior are the Mohorovičić discontinuity (Moho) that separates the Earth's crust from the underlying mantle, and the Gutenberg discontinuity that marks the boundary between the mantle and the outer core. These discontinuities are characterized by changes in seismic wave velocity and composition.
No, the Lehmann discontinuity is believed to be located between 220 km and 260 km beneath the Earth's surface. The Gutenberg discontinuity, on the other hand, sits at a depth of around 2,900 km.
The seismic discontinuity at the base of the crust is known as the Mohorovičić discontinuity, or Moho for short. It marks the boundary between the Earth's crust and the underlying mantle, where seismic waves experience a sudden change in velocity.
No. The Moho (more correctly the Mohorovičić discontinuity) is the name given to a seismic discontinuity between the Earth's crust and mantle. The seismic discontinuity between the Earth's mantle and liquid core is known as the Gutenberg discontinuity or the CMB - Core Mantle Boundary.
interface between the crust and the upper mantle