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DIAGRAM's large sample ensures reasonable power; for the lowest RAF of all eight SNPs, the DIAGRAM sample had greater than 80% power to detect an OR of at least 1.07, and therefore non-association may be due to substantially different LD structures or lower effect sizes in white Europeans because of ethnic specific gene environment or gene gene interactions.
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Open image in new window Fig. 3 US salinity diagram: samples are in low-sodium category and in different salinity category.
Open image in new window Figure 2 X-ray diagram samples of RGO reduced with (a) sodium hypophosphite and (b) sodium sulfite.
Samples 20 and 21 show exception which are collected from the upcoming urban agglomerate Open image in new window Fig. 4 Wilcox diagram: samples are in very good to good category except samples 20 and 21 Open image in new window Fig. 5 Hill Piper diagram: Samples spread in almost all types with sodium chloride type dominating.
In the CM diagram samples from the tsunami unit and the reference samples from the beach are located in high-energy depositional area, while the marshland samples are located in low-energy zones (Fig. 9).
On conventional trilinear diagrams, sample values for three cations (calcium, magnesium and alkali metals-sodium and potassium) and three anions (bicarbonate, chloride and sulfate) are plotted relative to one another.
During the post-monsoon season, most of the samples were plotted in Na Cl type field in the piper diagram, except sample number S8. Sample number S8 showed the Ca Na HCO3 type of water.
Plotted on temperature salinity diagrams, samples from a single water mass tend to cluster in unique groups or elongate zones.
In these diagrams, samples falling in the centre of the curve are derived from rock water interaction.
According to Gibbs diagrams samples fall in the rock dominance field and the chemical quality of groundwater is related to the lithology of the area.
In the chondrite-normalized rare-earth element (REE) diagrams, samples FZ01 to FZ08 are clearly enriched in light REE (LREE), with weak to moderate negative Eu anomalies (Figure 8a).
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