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The early Holocene was then characterised by increasing development of Nothofagus open canopy forest.
The surface was then characterised using techniques of SEM, XRD and microhardness testing.
The system was then characterised in terms of its fluid dynamics under pressure and voltage driven conditions and its functionality was demonstrated in a preliminary experiment.
A copolymer of anti-5,15-bis([2′,2″:5″,2″′-terthiophene]-3″-yl -2,8,12,18-tetra-n-butyl-3,7,13,17-tetramethylporphyrin (1) with 2,2′:5″,2″′-terthiophene]-3″-yl -2,8,12,18-tetra-n-butyl-3,7,13,17-tetramethylporphyrined by cyclic voltammetry, UV-Vis spectroscopy, four-point probe conductivity measurement, and scanning electron microscopy.
The quality of each DST was then characterised by the average of the weighted mean scores from the two raters, adjusted by the model to take account of their personal propensity to give higher or lower scores.
This 'most important' reaction was then characterised experimentally, or through literature data.
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The crystalline products were then characterised by FTIR, FESEM, EDX, TGA, DSC and XRD.
These modified membranes were then characterised with the use of different techniques.
The region from -5 to 80 m is then characterised by the presence of strong echoes.
The evolution of the fluid's chemical composition is then characterised after passage through the fracture.
In-situ chl-a data for each region were then characterised by runoff and salinity groups using box plots.
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