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The turbidity maximum zone was located downstream of the study site since thick slackwater mud drapes that characterize the seaward part of the fluvial to tidal transition zone are not present; only a few thin mud drapes are found at the study locality.
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The estuary turbidity maximum (ETM) zone was about 10 km longer during the wet season than the dry season.
The maximum coupled zone was in the frequency range between 1 and 7 Hz for the vertical oscillations affecting the Scintrex CG-3 M#9310234 and between 1 and 11 Hz for the vertical oscillations affecting the LaCoste & Romberg D 185.
The isolate having maximum clearance zone was selected for further studies.
When those mixing units were combined, it showed the maximum because the recirculation zone was significantly developed.
We detected a seismic swarm at 13 to 20 km depth beneath the main Marmara fault (MMF), and the maximum depth of seismogenic zone was 25 km within the OBS observation area.
The maximum hardness value for this zone was observed near the interface and gradually decreased towards the substrate.
The maximum diameter of the inhibition zone was observed.
The maximum height of the caving zone was 9.0 m, which was 7.5 times of the mining height.
Those who consented were interviewed with the aid of self-administered semi-structured questionnaire until the maximum sample size for each zone was reached.
As result, the maximum zone area is 18.37 km2, with mean 1.34 and median 0.72 km2.
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CEO of Professional Science Editing for Scientists @ prosciediting.com