equipotential surface sentence in Hindi
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- TPMS have been observed as biological membranes, as block copolymers, equipotential surfaces in crystals etc . They have also been of interest in architecture, design and art.
- Since the Sea Level Datum of 1929 was a hybrid model, it was not a pure model of mean sea level, the geoid, or any other equipotential surface.
- In a state of rest or absence of external forces, the mean sea level would coincide with this geoid surface, being an equipotential surface of the Earth's gravitational field.
- The formulas for calculating the normal gravity is based on the assumption of an imagined rotationally symmetrical ellipsoid model of the earth, the surface of which is identical to an equipotential surface.
- In electrostatics, the work done to move a charge from any point on the equipotential surface to any other point on the equipotential surface is zero since they are at the same potential.
- In electrostatics, the work done to move a charge from any point on the equipotential surface to any other point on the equipotential surface is zero since they are at the same potential.
- Taylor's derivation is based on two assumptions : ( 1 ) that the surface of the cone is an equipotential surface and ( 2 ) that the cone exists in a steady state equilibrium.
- Additional tidal bench mark elevations were not used due to the demonstrated variations in sea surface topography, i . e ., that mean sea level is not the same equipotential surface at all tidal bench marks.
- A geopotential field U is constructed, being the sum of a gravitational potential \ Psi and the known centrifugal potential \ Phi, that " has the GRS80 reference ellipsoid as one of its equipotential surfaces ".
- In 2001, Mars Orbiter Laser Altimeter data led to a new convention of zero elevation defined as the equipotential surface ( gravitational plus rotational ) whose average value at the equator is equal to the mean radius of the planet.
- The reference surface that normal heights are measured from is called the quasi-geoid, a representation of " mean sea level " similar to the geoid and close to it, but lacking the physical interpretation of an equipotential surface.
- In 1919, the renowned physicist, Albert A . Michelson, noted that the most favorable arrangement to obtain high sensitivity and immunity from temperature perturbations is to use the equipotential surface defined by water in a buried half-filled water pipe.
- The gradient of the scalar potential ( and hence also its opposite, as in the case of a vector field with an associated potential field ) is everywhere perpendicular to the equipotential surface, and zero inside a three-dimensional equipotential region.
- Specifically, the geoid is the equipotential surface that would coincide with the mean ocean surface of Earth if the oceans and atmosphere were in equilibrium, at rest relative to the rotating Earth, and extended through the continents ( such as with very narrow canals ).
- Gravity is perpendicular to the equipotential surfaces of the gravity potential, and in electrostatics and in the case of steady currents the electric field ( and hence the electric current, if any ) is perpendicular to the equipotential surfaces of the electric potential ( voltage ).
- Gravity is perpendicular to the equipotential surfaces of the gravity potential, and in electrostatics and in the case of steady currents the electric field ( and hence the electric current, if any ) is perpendicular to the equipotential surfaces of the electric potential ( voltage ).
- One can construct a simple model geopotential U that has as one of its equipotential surfaces this reference ellipsoid, with the same model potential U _ 0 as the true potential W _ 0 of the geoid; this model is called a " normal potential ".
- Once a clean, smooth geopotential field U has been constructed matching the known GRS80 reference ellipsoid with an equipotential surface ( we call such a field a " normal potential " ) we can subtract it from the true ( measured ) potential W of the real Earth.
- The actual shape of the equipotential surface is called the geoid and it is not quite ellipsoidal, because of the unequal distribution of mass of the continents, etc . And even more accurately than the equipotential surface, you really have to describe every single point, to account for every rock, hill, bump on the ground, etc . talk ) 17 : 41, 15 April 2010 ( UTC)
- The actual shape of the equipotential surface is called the geoid and it is not quite ellipsoidal, because of the unequal distribution of mass of the continents, etc . And even more accurately than the equipotential surface, you really have to describe every single point, to account for every rock, hill, bump on the ground, etc . talk ) 17 : 41, 15 April 2010 ( UTC)
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