2 research outputs found
Optimization of a Solution-Processed SiO<sub>2</sub> Gate Insulator by Plasma Treatment for Zinc Oxide Thin Film Transistors
We report on the optimization of
the plasma treatment conditions
for a solution-processed silicon dioxide gate insulator for application
in zinc oxide thin film transistors (TFTs). The SiO<sub>2</sub> layer
was formed by spin coating a perhydropolysilazane (PHPS) precursor.
This thin film was subsequently thermally annealed, followed by exposure
to an oxygen plasma, to form an insulating (leakage current density
of ∼10<sup>−7</sup> A/cm<sup>2</sup>) SiO<sub>2</sub> layer. Optimized ZnO TFTs (40 W plasma treatment of the gate insulator
for 10 s) possessed a carrier mobility of 3.2 cm<sup>2</sup>/(V s),
an on/off ratio of ∼10<sup>7</sup>, a threshold voltage of
−1.3 V, and a subthreshold swing of 0.2 V/decade. In addition,
long-term exposure (150 min) of the pre-annealed PHPS to the oxygen
plasma enabled the maximum processing temperature to be reduced from
180 to 150 °C. The resulting ZnO TFT exhibited a carrier mobility
of 1.3 cm<sup>2</sup>/(V s) and on/off ratio of ∼10<sup>7</sup>
New Zealand GPS velocity field: 1995–2013
<p>We collate nearly two decades of campaign GPS data gathered at over 900 sites throughout New Zealand to release a New Zealand nationwide GPS velocity field. The data span the entire North and South islands of New Zealand with a typical spacing of 10–20 km and a denser network (c. 2–8 km spacing) in the Wellington region, central Taupo Volcanic Zone and parts of the Arthur's Pass area. The dataset provides the most comprehensive-to-date view of crustal deformation within the Australia–Pacific plate boundary zone in the New Zealand region. We discuss the data acquisition, processing and derivation of the velocities and uncertainties. We also undertake corrections for earthquake displacements to obtain a velocity field that is largely representative of interseismic deformation between 1995 and 2013.</p