In
calculus, the 'mean value theorem' states, roughly, that given a section of a
smooth curve, there is a point on that section at which the
derivative (slope) of the curve is equal to the "average" derivative of the section. It is used to prove theorems that make global conclusions about a function on an interval starting from local hypotheses about derivatives at points of the interval.
This theorem can be understood concretely by applying it to motion: if a car travels one hundred miles in one hour, so that its ''average'' speed during that time was 100 miles per hour, then at some time its ''instantaneous'' speed must have been exactly 100 miles per hour.
An early version of this
theorem was first described by
Parameshvara (1370–1460) from the
Kerala school of astronomy and mathematics in his commentaries on
GovindasvÄmi and
Bhaskara II.
[1] The mean value theorem in its modern form was later stated by
Augustin Louis Cauchy (1789-1857). It is one of the most important results in
differential calculus, as well as one of the most important theorems in
mathematical analysis, and is essential in proving the
fundamental theorem of calculus. The mean value theorem can be used to prove
Taylor's theorem, of which it is a special case.
Formal statement
:Let ''f'' : [''a'', ''b''] → 'R' be a
continuous function on the closed
interval [''a'', ''b''], and
differentiable on the open interval (''a'', ''b''). Then, there exists some ''c'' in (''a'', ''b'') such that
::
The mean value theorem is a generalization of
Rolle's theorem, which assumes ''f''(''a'') = ''f''(''b''), so that the right-hand side above is zero.
The mean value theorem is still valid in a slightly more general setting, one only needs to assume that ''f'' : [''a'', ''b''] → 'R' is
continuous on [''a'', ''b''], and that for every ''x'' in (''a'', ''b'') the
limit
:
exists as a finite number or equals 屰.
Proof
An understanding of this and the
point-slope formula will make it clear that the equation of a
secant (which intersects (''a'', ''f''(''a'')) and (''b'', ''f''(''b'')) ) is:
:
The formula ( ''f''(''b'') − ''f''(''a'') ) / (''b'' − ''a'') gives the
slope of the line joining the points (''a'', ''f''(''a'')) and (''b'', ''f''(''b'')), which we call a chord of the curve, while ''f'' ' (''x'') gives the slope of the tangent to the curve at the point (''x'', ''f''(''x'') ). Thus the Mean value theorem says that given any chord of a smooth curve, we can find a point lying between the end-points of the chord such that the tangent at that point is parallel to the chord. The following proof illustrates this idea.
Define ''g''(''x'') = ''f''(''x'') + ''rx'', where ''r'' is a constant. Since ''f'' is continuous on [''a'', ''b''] and differentiable on (''a'', ''b''), the same is true of ''g''. We choose ''r'' so that ''g'' satisfies the conditions of
Rolle's theorem, which means
:
:
By Rolle's theorem, since ''g'' is continuous and ''g''(''a'') = ''g''(''b''), there is some ''c'' in (''a'', ''b'') for which ''g'' '(''c'') = 0, and it follows from ''g''(''x'') = ''f''(''x'') + ''rx'' that,
:
as required.
Cauchy's mean value theorem
'Cauchy's mean value theorem', also known as the 'extended mean value theorem', is the more general form of the mean value theorem. It states: If functions
and
are both continuous on the closed interval
, differentiable on the open interval
, and
is not zero on that open interval, then there exists some
in
, such that
:
Cauchy's mean value theorem can be used to prove
l'Hopital's rule. The mean value theorem is the special case of Cauchy's mean value when
(or more generally when
is affine and not constant, meaning
where
and
are constants and
).
Proof of Cauchy's mean value theorem
The proof of Cauchy's mean value theorem is based on the same idea as the proof of the mean value theorem.
First we define a new function ''h''(''t'') and then we aim to transform this function so that it satisfies the conditions of Rolle's theorem.
:
where ''m'' is a constant. We choose ''m'' so that
:
Since ''h'' is continuous and ''h''(''a'') = ''h''(''b''), by Rolle's theorem, there exists some ''c'' in (''a'', ''b'') such that ''h''′(''c'') = 0, i.e.
:
:
as required.
Mean value theorems for integration
The 'first mean value theorem for integration' states
:If ''G'' :
[''a'', ''b''
] → 'R' is a continuous function and φ :
[''a'', ''b''
] → 'R' is an
integrable positive function, then there exists a number ''x'' in (''a'', ''b'') such that
::
In particular for φ(''t'') = 1, there exists ''x'' in (''a'', ''b'') such that
:
The 'second mean value theorem for integration' is stated as follows
:If ''G'' :
[''a'', ''b''
] → 'R' is a
monotonically decreasing (not necessarily positive) function and φ :
[''a'', ''b''
] → 'R' is an integrable function, then there exists a number ''x'' in (''a'', ''b''
) such that
::
The latter statement was proved by
Hiroshi Okamura in 1947.
See also
★
arithmetic mean
★
Newmark-beta method
★
mean value theorem (divided differences)
References
1. J. J. O'Connor and E. F. Robertson (2000). Paramesvara, ''MacTutor History of Mathematics archive''.
External links
★
PlanetMath: Mean-Value Theorem
★
Mathworld: Mean-Value Theorem