Page 108 - Soil and water contamination, 2nd edition
P. 108

Major dissolved phase constituents                                     95
                    1                                   6
                    Na+K                            Cl  Na+K                            Cl
                     Ca                             HCO3  Ca                            HCO3
                     Mg                             SO4  Mg                             SO4
                     Fe                             NO3  Fe                             NO3
                      25  20  15  10  5  0  5  10  15  20  25 meq/l  50  40  30  20  10  0  10  20  30  40  50 meq/l
                                                  25
                    2                                   7
                    Na+K                            Cl  Na+K                            Cl
                     Ca                             HCO3  Ca                            HCO3
                     Mg                             SO4  Mg                             SO4
                     Fe                             NO3  Fe                             NO3
                      1.0  0.8  0.6  0.4  0.2  0.0  0.2  0.4  0.6  0.8 1.0 meq/l  10  8  6  4  2  0  2  4  6  8  10 meq/l
                    3                                   8
                    Na+K                            Cl  Na+K                            Cl
                     Ca                             HCO3  Ca                            HCO3
                     Mg                             SO4  Mg                             SO4
                     Fe                             NO3  Fe                             NO3
                     100  80  60  40  20  0  20  40  60  80  100 meq/l  250 200 150 100  50  0  50  100 150 200 250meq/l
                    4                                   9
                    Na+K                            Cl Cl  Na+K                         Cl
                    Na+K
                                                    HCO3
                     Ca                             HC O 3  Ca                          HCO3
                     Mg                             SO4 4  Mg                           SO4
                                                    SO
                     Fe                             NO3  Fe                             NO3
                                                    NO3
                                                    meq/l
                      25  20  15  10  5  0  5  10  15  20  25 meq/l  2.5  2.0  1.5  1.0  0.5 0.0  0.5  1.0  1.5  2.0  2.5 meq/l
                    5                                   10
                    Na+K                            Cl  Na+K                            Cl
                     Ca                             HCO3  Ca                            HCO3
                     Mg                             SO4  Mg                             SO4
                     Fe                             NO3  Fe                             NO3
                     6642  6642  6642  5  4  3  2  1  0  1  2  3  4  5 meq/l  1.0  0.8  0.6  0.4  0.2 0.0  0.2  0.4  0.6  0.8 1.0 meq/l

                   Figure 5.3  Stiff diagrams  of ten bottled mineral waters from Europe (see Table 5.2) (source: Van der Perk and De
                   Groot, 2013).
                   is particularly important for maintaining osmotic pressure in the cells. It is essential for
                   the exchange of water between the cells and the intercellular medium. Although Na is an
                   essential element, it is toxic in large concentrations or amounts. In animals and humans,
                   chronic excess intake of Na leads to high blood pressure, which can result in serious health
                   issues in the long term. The tolerance of different organisms to Na displays a broad range,
                   but the tolerance of individual species may be limited. This implies that a structural increase
                   in Na concentrations will bring about changes in species composition. Drinking water
                                                                          -1
                   containing elevated Na concentrations of more than about 200 mg l  has an objectionable
                   salty taste.
                      Sodium is derived from weathering  of Na-bearing feldspars  present in igneous rocks
                   (e.g. albite, NaAlSi O ) or dissolution  of evaporite  sediments. In addition, in coastal areas,
                                  3  8
                   seawater and brackish water may particularly be a significant source of Na, either via direct
                   input as a result of flooding or via atmospheric input (salt spray). Because the major Na









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