Summary
A functionE:I } I → ℝ is called aquasideviation on the open interval \(I \subseteq \mathbb{R}_{\dot + } \) if
-
(E1)
sgnE(x, y) = sgn(x − y) forx, y ∈ I;
-
(E2)
y → E(x, y) is a continuous function onI for each fixedx ∈ I;
-
(E3)
y → E(x, y)/E(x′, y) is a strictly decreasing function on ]x, x′[ forx < x′ inI.
Ifx 1,⋯, x n ∈ I then the equation
E(x 1,y) + ⋯ + E(x n ,y) = 0 has a unique solutiony = y 0 which is between\(\mathop {min}\limits_{1 \leqslant i \leqslant n} \) x i and\(\mathop {max}\limits_{1 \leqslant i \leqslant n} \) x i (see [6]). This valuey 0 is called theE-quasideviation mean ofx 1,⋯, x n and is denoted by\(\mathfrak{M}_E (x_1 ,...,x_n )\).
TheE-quasideviation mean\(\mathfrak{M}_E \) is calledhomogeneous if
is satisfied for alln ∈ ℕ,x 1,⋯, x n ∈ I withtx 1,⋯, tx n ∈ I.
One of the main results of the paper is the following
Theorem.If I/I = {x/y ∣ x, y ∈ I} = ℝ+ and E:I } I → ℝ is an arbitrary function, then E is a quasideviation and \(\mathfrak{M}_E \) is a homogeneous mean if and only if there exist three functions a: I → ℝ +;f: ℝ + → ℝ, m:ℝ + → ℝ + so that
-
(i)
a is continuous and positive;
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(ii)
f is continuous and increasing on ℝ +,further it is strictly monotonic on ]0, 1[ or on ]1, ∞[ and sgn f(x) = sgn(x − 1),x > 0;
-
(iii)
m is multiplicative, i.e. m(xy) = m(x)m(y) for x, y > 0;
-
(iv)
E(x, y) = a(y)m(x)f(x/y) for x, y ∈ I.
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Páles, Z. On homogeneous quasideviation means. Aeq. Math. 36, 132–152 (1988). https://doi.org/10.1007/BF01836086
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DOI: https://doi.org/10.1007/BF01836086