Gallery of Surfaces.
Virtual Math Museum.
Classic
Curves and Surfaces. "National Curve Bank" of Gustavo Gordillo.
Wikipedia : Surfaces
The most explicit way to specify a surface is to give the 3 cartesian coordinates of an arbitrary point as functions of 2 parameters, traditionally denoted u and v. The equation of a surface is the relation satisfied by the coordinates of every point.
When (a,b,c) is not (0,0,0) the plane's cartesian equation is:
a x + b y + c z = a2 + b2 + c2
Otherwise, we're dealing with a plane going through the origin and shall use any nonzero vector (a,b,g) orthogonal to the plane:
a x + b y + g z = 0
This can be construed as a limiting case of the previous equation.
[画像: Helicoid ] The cartesian parametric equations are:
The equation in cylindrical coordinates is just:
z = k q
For a right-handed helicoid (as depicted above) the constant k is positive. It's negative for a left-handed one. The plane is an helicoid (with k = 0).
The constant k is homogeneous to a length per unit of angle. It's related to the wavelength a (the constant signed vertical displacement between two consecutive sheets) by the following relation, if angles are in radians:
a = 2 p k
An 1842 theorem due to Catalan (1814-1894) states that helicoids (planes included) are the only ruled minimal surfaces. [ Proof ]
A generalized helicoid is generated by helical rotation of an abitrary curve of equation z = f (x). Its cartesian parametric equations are:
The cylindrical equation is: z = f (r) + k q
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Jean-Baptiste Meusnier (1754-1793)
Wikipedia :
Helicoid
|
Generalized helicoid
MathWorld :
Circular helicoid
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Catalan surfaces | Eugène Catalan (1814-1894; X1833)
The term torse is considered archaic.
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Gaussian curvature (K) | Wikipedia : Developable surface (torse)
At a given point on a surface, the normal curvature is extreme along the two perpendicular directions of the lines of curvature.
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Pappus of Alexandria (c. AD 290-350) | Paul Guldin (1577-1643)
Because the plane of a meridian is orthogonal to the surface, the normal curvature of the meridian is equal to its curvature given by the formula:
An unduloid is a surface of revolution whose meridian is traced by the focus of a conic section which rolls on the axis.
With a parabola, a catenoid is obtained. The mean curvature is zero.
When it's an hyperbola, the surface has negative mean curvature, which corresponds to a soap film surrounding a region of lower pressure.
A rolling ellipse corresponds to a positive mean curvature and/or a higher inner pressure. We obtain the undulatory shape shown below, which has given its name to the whole family.
Mean curvature | Wikipedia : CMC surface (constant mean curvature) | Wente torus (1984): video.
Dupin's theorem | Charles Dupin (1784-1873; X1801)