Sentence examples for a weak surface of from inspiring English sources

For the anisotropic part, two different reinforcing models are examined and it is shown that, depending on the choice of model and whether the fiber is under compression or extension, loss of ellipticity may be associated with, in particular, a weak surface of discontinuity normal to or parallel to the deformed fiber direction or at an intermediate angle.

In addition, the strength drop noticeable with small specimens which was obtained in the experiments is explained by the presence of a weak surface layer of constant thickness (caused e.g., by drying, surface damage, aggregate size limitation at the boundary, or other irregularities).

Their magnetization is consistent with a weak surface field of a few hundred to a few thousand nano-Teslas (Collinson 1997; Rochette et al. 2001).

A weak surface area of low pressure detached from a frontal system on August 8 while 1,150 miles (1,850 km) to the east of Bermuda.

By integrating arrays of such sensors on a practical testing platform using hybrid e-beam lithography and photolithography techniques, we demonstrated that these sensors were capable of detecting a weak surface temperature difference of 0.1 0.2 K at microscale, and they could be scaled up as built-in temperature sensors in many practical devices.

In such a hybrid device, these sensors remained a stable and repeatable sensitivity for sensing a weak surface temperature difference of 0.1 0.2 K over a local area of 10 100-μm scale.

The testing results showed that over an area of diameter 40 100 μm, the sensors could detect a weak surface temperature difference of 0.1 0.2 K.

Central convection decreased, and Nina became an extratropical cyclone by October 2. A weak surface low formed west of Truk on October 3, which contained little thunderstorm activity.

The combination of a weak surface trough and an upper-level low pressure system produced disorganized showers and thunderstorms from western Cuba into the eastern Gulf of Mexico.

As a tropical wave approached from the east, an inverted trough developed on the northern edge of the active region on June 2, setting the stage for the formation of a weak surface low pressure system over the southern Gulf of Mexico the next day.

A weak surface trough, located to the west of an upper-level low, developed convection to the east of the Bahamas on July 26.