Sentence examples for dissolution gap from inspiring English sources

The oxygen-rich layer at the WOx/W TE interface with a thickness of 3.5 nm was observed at LRS, and the dissolution gap in the CF ruptured region was approximately 7.5 nm.

By adjusting the P/E operation conditions, the filament length or maintaining dissolution gap is also important where the resistance ratio could be decreased because HRS value will be lower.

The oxygen ion migration under external bias, oxygen-rich layer formation at the WOx/W TE interface during set, and larger dissolution gap during reset show the resistive switching characteristics.

Basically, oxygen ion migration under external bias controls the interfacial oxygen-rich layer and dissolution gap as well as the lower and higher barrier heights which lead to LRS and HRS switching, as shown in energy band diagram under bias (Fig. 7).

Due to oxygen-rich layer formation at LRS, the F-N tunneling is observed, and after reset at the maximum value of negative voltage (−5, −6, and −4 V for the S1, S2, and S3 devices, respectively), the electrons had enough energy to F-N tunnel through the dissolution gap.

The dissolution gap in reset for the devices showed that the device annealed at 500 °C had the smallest gap among the three devices, which was responsible for the lowest set/reset voltage and Φ B value. Figure 6c shows the E (=dψ/dx) distributions for the S1, S2, and S3 devices after set (or at LRS).

The etching process was found to consist of two compensating partial currents, corresponding to the anodic dissolution of GaP and to the cathodic reduction of Fe CN 3−6via hole injection respectively.

The micropores in the shale observed by the SEM are dominated by intergranular (dissolution) mineral pores, intergranular gaps, intragranular pores, the organic matter micropores, and micro-fractures.

There are various kinds of secondary pores and gaps containing dissolution pores in particles and cements (Fig. 6k, l), moldic pores (Fig. 6i), intergranular micropores of kaolinite (Fig. 6m, n, o and p), microfractures and diagenetic contraction fractures.

The fixed-term parliaments bill could widen the gap by making dissolution more difficult and enabling parties to change coalition partners without having to appeal to the voters.

There was a long gap after the dissolution but the tradition was revived by Sir Thomas May in 1701 when he became the owner of the Priory.