The zero-field conductivities (σ) of the polycrystaline title
materials, are governed by inter-grain transport. In the majority of cases
their σ(T) can be described by the "fluctuation induced tunneling"
model. Analysis of the results in terms of this model reveals two remarkable
features: 1. For \emph{all} Sr2FeMoO6 samples of various microstructures,
the tunneling constant (barrier width × inverse decay-length of the
wave-function) is ∼ 2, indicating the existence of an intrinsic insulating
boundary layer with a well defined electronic (and magnetic) structure. 2. The
tunneling constant for \emph{all} cold-pressed samples decreases linearly with
increasing magnetic-moment/formula-unit.Comment: 10 pages, 2 tables, 3 figure