Blaga P. Lectures on the differential geometry of - tiera.ru
Blaga P. Lectures on the differential geometry of - tiera.ru
Blaga P. Lectures on the differential geometry of - tiera.ru
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4.19. Geodesics 177<br />
will denote it by kg and we will call it geodesic or tangential curvature <strong>of</strong> <strong>the</strong> curve 7 . To<br />
find <strong>the</strong> quantity d, we start from <strong>the</strong> relati<strong>on</strong><br />
N = sin θ · ν − cos θ · β.<br />
By differentiating with respect to <strong>the</strong> arclength <strong>of</strong> <strong>the</strong> curve, we get, using <strong>the</strong> last two<br />
<strong>of</strong> <strong>the</strong> Frenet’s formulae:<br />
N ′ = θ ′ · sin θ · ν − sin θ(−k · τ + χ · β) + θ ′ sin θ · β + χ · cos θ · ν =<br />
= −k · sin θ · τ + (θ ′ + χ) · (cos θ · ν + sin θ · β) =<br />
= −k · sin θ · τ + (θ ′ + χ) · n,<br />
and, comparing with <strong>the</strong> sec<strong>on</strong>d equati<strong>on</strong> from (4.19.2), we get<br />
d = θ ′ + χ.<br />
This functi<strong>on</strong> is denoted by χg and it s called <strong>the</strong> geodesic torsi<strong>on</strong>. His geometric meaning<br />
will be made clear later. Clearly, we cannot claim, as we did with <strong>the</strong> geodesic<br />
curvature, that <strong>the</strong> geodesic torsi<strong>on</strong> is <strong>the</strong> torsi<strong>on</strong> <strong>of</strong> <strong>the</strong> projecti<strong>on</strong> <strong>of</strong> <strong>the</strong> curve <strong>on</strong> <strong>the</strong><br />
tangent plane, as <strong>the</strong> torsi<strong>on</strong> <strong>of</strong> that curve is always zero, while <strong>the</strong> geodesic torsi<strong>on</strong> <strong>of</strong><br />
<strong>the</strong> given curve is not, usually.<br />
The geodesic curvature plays a much more important role in <strong>the</strong> <strong>differential</strong> <strong>geometry</strong><br />
<strong>of</strong> surfaces than <strong>the</strong> geodesic torsi<strong>on</strong> does, so we start by focusing <strong>on</strong> it. We notice, to<br />
begin with, that<br />
kg = τ ′ · N = −τ · N ′ . (4.19.4)<br />
Since, as we saw earlier, N = n × τ, <strong>on</strong>e obtains for kg <strong>the</strong> expressi<strong>on</strong><br />
i.e.<br />
kg = τ ′ · N = τ ′ · (n × τ),<br />
kg = (τ, τ ′ , n). (4.19.5)<br />
This formula holds for naturally parameterized curves. Let us c<strong>on</strong>sider, now, an arbitrary<br />
regular parameterized curve <strong>on</strong> S , given by <strong>the</strong> local equati<strong>on</strong>s u = u(t), v = v(t). We<br />
have, <strong>the</strong>refore, r = r(u(t), v(t)). If we denote by a dot <strong>the</strong> differentiati<strong>on</strong> with respect to<br />
<strong>the</strong> parameter t al<strong>on</strong>g <strong>the</strong> curve, we get<br />
τ ≡ dr<br />
ds<br />
dr dt 1<br />
= = · ˙r,<br />
dt ds ˙s<br />
7 Here <strong>the</strong> term “tangential” refers to <strong>the</strong> tangent plane <strong>of</strong> <strong>the</strong> surface, not to <strong>the</strong> tangent line <strong>of</strong> <strong>the</strong> curve.<br />
In fact, it can be shown that <strong>the</strong> geodesic curvature at a point <strong>of</strong> a curve lying <strong>on</strong> a surface is <strong>the</strong> signed<br />
curvature <strong>of</strong> <strong>the</strong> projecti<strong>on</strong> <strong>of</strong> <strong>the</strong> curve <strong>on</strong> <strong>the</strong> tangent plane to <strong>the</strong> surface at that particular point.