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No significant seasonal variations of MMD and GSD were observed in most of samples.
The piper diagram shows that most of samples are bicarbonate and calcic facies.
At 120°C, solutions were saturated with repect to niter, sylvite, and halite between most of samples between 0.15 ≤ XNa ≥ 0.30.
The result shows that the value for log PCO2 is low for most of samples, i.e., all selected samples are under saturated with respect to it.
The graph of Ca2+ + Mg2+ versus SO4 2− + HCO3 − (Fig. 4f) shows that most of samples fall above the 1 1 ratio line and show a deficiency of Ca2+ + Mg2+ relative to SO4 2− + HCO3 −.
This figure shows that most of samples plot around the fresh water evaporation line, emphasizing that evaporation plays a major role in deciding the chemical composition of groundwater in this area.
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I would never contest the idea that hip-hop made the most of sampling but it is not the square one of sampling for everyone.
The melting thermograms of most types of samples exhibited single peaks with melting range increasing with exposure time.
For most kinds of samples, ashing can be completed within half an hour.
The avidity indices of most of the samples varied considerably depending on the sample dilution.
Most of the samples from Well X have similar distribution patterns except some samples (Fig. 4).
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com