P = 4*a (a is side length) Area = p*q/2 (p=perimeter, q=diagonal
A sphere, of radius a = 11.4 cm and charge q = 5.00 × 10 − 6 C uniformly distributed throughout its volume, is concentric with a spherical conducting shell of inner radius b = 26.2 cm and outer radius c = 28.2 cm . This shell has a net charge of -q. visit our page : grandarchinex.co.in
Area = Length * Width So Length = Area / Width Length = 132/1q = 132/q feet
If the two axes intersect at the point (p, q), then the equation is: (x -p)2/25 + (y - q)2/9 = 1
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56 cm is a length, not a volume, hence the Q is unanswerable.
Assume the two numbers are P & Q, the equation is P + Q = 53, rearranging this gives Q = 53 - P
7 x 11 = 77
A pair of parallel lines at a distance of 1 cm from the line Q.
The shortest path from P to Q along the surface of the cube will be one that goes from P, to the center point on any edge, to the opposite side, and then to Q. The length of that will be L + L/2 + L/2, or 2L, where L is the length of any side of the cube. We are told that this distance is equal to 2√2, so we can say: 2L = 2√2 cm ∴ L = √2 cm The volume of the cube will be that length, cubed, or L3, which means we can say: V = L3 ∴ V = (√2 cm)3 ∴ V = (21/2)3 cm3 ∴ V = 23/2 cm3
The mirror formula for concave mirrors is 1/f = 1/d_o + 1/d_i, where f = focal length, d_o = object distance, and d_i = image distance. Given f = 10 cm, d_i = 30 cm, we can solve for d_o: 1/10 = 1/d_o + 1/30. Solving for d_o gives d_o = 15 cm. The corresponding object is located 15 cm away from the mirror.
The answer will depend on what r, p, q, m and l are. Since none of these are defined, a sensible answer is not possible.
Q-T- Hush - 1960 The Doomsday Caper Sound of Doom 1-53 was released on: USA: 1960
Square root of 53 is simlipfied in decimal form as √53 = 7.280. Square root of 53 cannot be expressed as a fraction in the form p/q which tells us that the square root of 53 is an irrational number.
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The Darcy fluid flow equation: u = q / Ac = ( - k / µ . dp / dI ) Where: u = fluid velocity, cm/s. q = flow rate cm3/s k = permeability of the porous rock, Darcy (0.986923 µm2) Ac = cross-sectional area of the rock, cm2 µ = viscosity of the fluid, centipoises (cP) I = length of the rock sample, cm dp / dI = pressure gradient in the direction of the flow, atm/cm.
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