An extremal quasi-conformal mapping f of a domain D is said to be of non-landslide type if the set Ef(δ):= {z∈D:|μf(z)|≤||μ|| ∞ -δ} has no interior points for any δ 】 0. In this paper,we construct a quasi-con...An extremal quasi-conformal mapping f of a domain D is said to be of non-landslide type if the set Ef(δ):= {z∈D:|μf(z)|≤||μ|| ∞ -δ} has no interior points for any δ 】 0. In this paper,we construct a quasi-conformal mapping f of the unit disc D such that its Teichmu¨ller equivalence class [f] contains infinitely many extremal mappings of non-landslide type. The relation between extremal mappings of non-landslide type and locally extremal mappings is also discussed.展开更多
本文证明:如果f(z)是拓广复平面到自身使得f(0)=0,f(1)=1和f(∞)=∞的一个Q拟共形映照。则对任何r,|z|≤r |f(z)|≤r,成立|f(z)-z|≤4/π rK(1/1+r)K(r/1+r)·logQ,其中K(t)=integral from n=0 to 1(dx/((1-x^2)(1-tx^2))^(1/2)。...本文证明:如果f(z)是拓广复平面到自身使得f(0)=0,f(1)=1和f(∞)=∞的一个Q拟共形映照。则对任何r,|z|≤r |f(z)|≤r,成立|f(z)-z|≤4/π rK(1/1+r)K(r/1+r)·logQ,其中K(t)=integral from n=0 to 1(dx/((1-x^2)(1-tx^2))^(1/2)。它是夏道行的一个定理的拓广。展开更多
基金supported by National Natural Science Foundation of China (Grant No.10771153)
文摘An extremal quasi-conformal mapping f of a domain D is said to be of non-landslide type if the set Ef(δ):= {z∈D:|μf(z)|≤||μ|| ∞ -δ} has no interior points for any δ 】 0. In this paper,we construct a quasi-conformal mapping f of the unit disc D such that its Teichmu¨ller equivalence class [f] contains infinitely many extremal mappings of non-landslide type. The relation between extremal mappings of non-landslide type and locally extremal mappings is also discussed.
文摘本文证明:如果f(z)是拓广复平面到自身使得f(0)=0,f(1)=1和f(∞)=∞的一个Q拟共形映照。则对任何r,|z|≤r |f(z)|≤r,成立|f(z)-z|≤4/π rK(1/1+r)K(r/1+r)·logQ,其中K(t)=integral from n=0 to 1(dx/((1-x^2)(1-tx^2))^(1/2)。它是夏道行的一个定理的拓广。
