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  2. Equipotential - Wikipedia

    en.wikipedia.org/wiki/Equipotential

    An equipotential of a scalar potential function in n-dimensional space is typically an (n − 1)-dimensional space. The del operator illustrates the relationship between a vector field and its associated scalar potential field. An equipotential region might be referred as being 'of equipotential' or simply be called 'an equipotential'.

  3. Geoid - Wikipedia

    en.wikipedia.org/wiki/Geoid

    Being an equipotential surface, the geoid is, by definition, a surface upon which the force of gravity is perpendicular everywhere, apart from temporary tidal fluctuations. This means that when traveling by ship, one does not notice the undulation of the geoid ; neglecting tides, the local vertical (plumb line) is always perpendicular to the ...

  4. Geopotential - Wikipedia

    en.wikipedia.org/wiki/Geopotential

    The surfaces of constant geopotential or isosurfaces of the geopotential are called equigeopotential surfaces (sometimes abbreviated as geop), [1] also known as geopotential level surfaces, equipotential surfaces, or simply level surfaces. [2] Global mean sea surface is close to one equigeopotential called the geoid. [3]

  5. Electrical bonding - Wikipedia

    en.wikipedia.org/wiki/Electrical_bonding

    Equipotential bonding involves electrically connecting metalwork so that it is at the same voltage everywhere. Exact rules for electrical installations vary by country, locality, or supplying power company. [2] Equipotential bonding is done from where the distribution wiring enters the building to incoming water and gas services.

  6. Flow net - Wikipedia

    en.wikipedia.org/wiki/Flow_net

    The method consists of filling the flow area with stream and equipotential lines, which are everywhere perpendicular to each other, making a curvilinear grid.Typically there are two surfaces (boundaries) which are at constant values of potential or hydraulic head (upstream and downstream ends), and the other surfaces are no-flow boundaries (i.e., impermeable; for example the bottom of the dam ...

  7. Potential flow - Wikipedia

    en.wikipedia.org/wiki/Potential_flow

    where in fact is the volume flux per unit length across a surface enclosing the source or sink. The velocity field in polar coordinates are The velocity field in polar coordinates are u r = Q 2 π r , u θ = 0 {\displaystyle u_{r}={\frac {Q}{2\pi r}},\quad u_{\theta }=0}

  8. Roche lobe - Wikipedia

    en.wikipedia.org/wiki/Roche_lobe

    A critical equipotential intersects itself at the L 1 Lagrangian point of the system, forming a two-lobed figure-of-eight with one of the two stars at the center of each lobe. This critical equipotential defines the Roche lobes. [2] Where matter moves relative to the co-rotating frame it will seem to be acted upon by a Coriolis force.

  9. Confocal conic sections - Wikipedia

    en.wikipedia.org/wiki/Confocal_conic_sections

    Considering the pencils of confocal ellipses and hyperbolas (see lead diagram) one gets from the geometrical properties of the normal and tangent at a point (the normal of an ellipse and the tangent of a hyperbola bisect the angle between the lines to the foci). Any ellipse of the pencil intersects any hyperbola orthogonally (see diagram).