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P = 4*a (a is side length) Area = p*q/2 (p=perimeter, q=diagonal
Area = Length * Width So Length = Area / Width Length = 132/1q = 132/q feet
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
If the two axes intersect at the point (p, q), then the equation is: (x -p)2/25 + (y - q)2/9 = 1
Since you know that it is a parallelogram (not parallellogram!) you already know that the opposite sides are mutually parallel. All you need to do is to establish that any pair of adjacent sides are of equal length, or equivalently, the squares of these lengths are equal. The squared length of the line AB where A = (p,q) and B = (r,s) is (p - r)^2 + (q - s)^2.
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 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.
Deep Q wave indicates old myocardial infarction.