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The Al-Kharj groundwaters chemical analysis revealed that the waters salinity (EC) ranged between 1.05 and 10.15 dS m−1 with an average of 3.00 dS m−1.
On the other hand, the waters salinity (EC) ranged between 1.05 and 10.15 dS m−1 with an average of 3.00 dS m−1 (Table 1, Fig. 4).
When ice melts, melts into the oceanic waters, salinity and temperature change in the larger ocean body.
Total alkalinity (TA) was computed according to: TA = 3929 - 46.156*SSS (r 2 = 0.872, p < 0.0001) where SSS is sea surface salinity, and TA is in μmol kg-1, established from 742 measurements in surface waters (salinity range 19.5 35.4) from 26 cruises carried out in the BCZ from 1996 to 2001 [[ 20, 21], Borges unpublished, Schiettecatte unpublished].
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The results also reveal that irrigation water salinity has no significant effect under shallow saline groundwater.
Water salinity has also become a vexing problem.
Soil salinity and drainage-water salinity both increased with increases in irrigation-water salinity.
The water salinity is constant in the vertical sense and tends to decrease toward the continent.
Antarctic surface-water salinity generally is below 34 parts per thousand.
Her talk will focus on patterns among plants, animals, water salinity and land in the Charles E. Wheeler Salt Marsh.
All of these indices decreased significantly as water salinity increased.
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