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  2. Prism correction - Wikipedia

    en.wikipedia.org/wiki/Prism_correction

    Thus a prism of 1 Δ would produce 1 cm visible displacement at 100 cm, or 1 meter. This can be represented mathematically as: = ⁡ where is the amount of prism correction in prism dioptres, and is the angle of deviation of the light.

  3. Vertex distance - Wikipedia

    en.wikipedia.org/wiki/Vertex_distance

    After simplifying the final equation is found: F F c = 1 − x F ⇒ F c = F 1 − x F = 1 1 F − x ⇒ F = 1 1 F c + x {\displaystyle {\begin{aligned}&&{\frac {F}{F_{\text{c}}}}&=1-xF\\&\Rightarrow &F_{\text{c}}&={\frac {F}{1-xF}}={\frac {1}{{\frac {1}{F}}-x}}\\&\Rightarrow &F&={\frac {1}{{\frac {1}{F_{\text{c}}}}+x}}\end{aligned}}}

  4. Schrödinger equation - Wikipedia

    en.wikipedia.org/wiki/Schrödinger_equation

    Linearity. The Schrödinger equation is a linear differential equation, meaning that if two state vectors and are solutions, then so is any linear combination. of the two state vectors where a and b are any complex numbers. [13] : 25 Moreover, the sum can be extended for any number of state vectors.

  5. Aberration (astronomy) - Wikipedia

    en.wikipedia.org/wiki/Aberration_(astronomy)

    This gives an angular correction ⁡ = / ≈ 0.000099364 rad = 20.49539 sec, which can be solved to give = / = ≈ 0.000099365 rad = 20.49559 sec, very nearly the same as the aberrational correction (here is in radian and not in arcsecond).

  6. Stratonovich integral - Wikipedia

    en.wikipedia.org/wiki/Stratonovich_integral

    In stochastic processes, the Stratonovich integral or Fisk–Stratonovich integral (developed simultaneously by Ruslan Stratonovich and Donald Fisk) is a stochastic integral, the most common alternative to the Itô integral. Although the Itô integral is the usual choice in applied mathematics, the Stratonovich integral is frequently used in ...

  7. Ramanujan's master theorem - Wikipedia

    en.wikipedia.org/wiki/Ramanujan's_master_theorem

    Equivalently, if the spherical Bessel function is preferred, the formula becomes 2 ν − 2 s π ( 1 − 2 s + 2 ν ) cos ⁡ ( π ( s − ν ) ) ∫ 0 ∞ z s − 1 − ν / 2 j ν ( z ) d z = Γ ( s ) Γ ( 1 2 + s − ν ) {\displaystyle {\frac {2^{ u -2s}{\sqrt {\pi }}(1-2s+2 u )}{\cos {(\pi (s- u ))}}}\int _{0}^{\infty }z^{s-1- u /2}j ...

  8. Goldman equation - Wikipedia

    en.wikipedia.org/wiki/Goldman_equation

    The Goldman–Hodgkin–Katz voltage equation, sometimes called the Goldman equation, is used in cell membrane physiology to determine the Resting potential across a cell's membrane, taking into account all of the ions that are permeant through that membrane. The discoverers of this are David E. Goldman of Columbia University, and the Medicine ...

  9. Free-air gravity anomaly - Wikipedia

    en.wikipedia.org/wiki/Free-air_gravity_anomaly

    Calculation. The free-air gravity anomaly is given by the equation: = (+) Here, is observed gravity, is the free-air correction, and is theoretical gravity.

  10. Maxwell's equations - Wikipedia

    en.wikipedia.org/wiki/Maxwell's_equations

    Maxwell's equations can be formulated with possibly time-dependent surfaces and volumes by using the differential version and using Gauss and Stokes formula appropriately. ∫ ∂ Ω {\displaystyle {\vphantom {\int }}_{\scriptstyle \partial \Omega }} is a surface integral over the boundary surface ∂Ω , with the loop indicating the surface is ...

  11. Dirac equation - Wikipedia

    en.wikipedia.org/wiki/Dirac_equation

    The Dirac equation is superficially similar to the Schrödinger equation for a massive free particle: − ℏ 2 2 m ∇ 2 ϕ = i ℏ ∂ ∂ t ϕ . {\displaystyle -{\frac {\hbar ^{2}}{2m}} abla ^{2}\phi =i\hbar {\frac {\partial }{\partial t}}\phi ~.}