The use of ultra-violet setting glue for microelectrode fabrication
Abstract The characteristics of glues which set in ultra-violet light are described with respect to their advantages for microelectrode assembly.
The electrophysiology of dopamine (D2) receptors: A study of the actions of dopamine on corticostriatal transmission
Electrophysiological recordings from the cells of the neostriatum in rats anaesthetised with halothane revealed only inhibitory actions of dopamine applied iontophoretically close to the cells. Inhibition of cortical driving seemed to have a slightly higher threshold in most cells but dopamine inhibited spontaneous action potentials, glutamate-induced responses, and cortical driving in the cells studied. Fluphenazine applied iontophoretically blocked the actions of dopamine but was itself without effect on the neuronal responses. Sulpiride, in contrast, was without effect on the spontaneous activity of the cells and was ineffective in blocking the action of applied dopamine. Sulpiride, nevertheless, increased the response to cortical stimulation though it had no action on the response to applied glutamate. These results suggest that the sub-class of dopamine receptors on the terminals of the corticostriatal pathway may be inhibitory on glutamate release and preferentially sensitive to blockade by sulpiride.
Observations of nearshore infragravity waves: Seaward and shoreward propagating components
[1] The variation of seaward and shoreward infragravity energy fluxes across the shoaling and surf zones of a gently sloping sandy beach is estimated from field observations and related to forcing by groups of sea and swell, dissipation, and shoreline reflection. Data from collocated pressure and velocity sensors deployed between 1 and 6 m water depth are combined, using the assumption of cross-shore propagation, to decompose the infragravity wave field into shoreward and seaward propagating components. Seaward of the surf zone, shoreward propagating infragravity waves are amplified by nonlinear interactions with groups of sea and swell, and the shoreward infragravity energy flux increases in the onshore direction. In the surf zone, nonlinear phase coupling between infragravity waves and groups of sea and swell decreases, as does the shoreward infragravity energy flux, consistent with the cessation of nonlinear forcing and the increased importance of infragravity wave dissipation. Seaward propagating infragravity waves are not phase coupled to incident wave groups, and their energy levels suggest strong infragravity wave reflection near the shoreline. The cross-shore variation of the seaward energy flux is weaker than that of the shoreward flux, resulting in cross-shore variation of the squared infragravity reflection coefficient (ratio of seaward to shoreward energy flux) between about 0.4 and 1.5.