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WATER TREATMENT AND PURIFICATION

                      4.14                       CHAPTER FOUR

                      TABLE 4.4  Prediction of Water Tendencies by the Langelier Index

                      Langelier saturation index    Tendency of water
                             2.0                    Scale-forming and for practical purposes noncorrosive
                             0.5                    Slightly corrosive and scale-forming
                             0.0                    Balanced, but pitting corrosion possible
                            –0.5                    Slightly corrosive and nonscale-forming
                            –2.0                    Serious corrosion



                      The most accurate method for calculating pHs is to use the following formula:
                                           pHs = (9.3 + A + B) − (C + D)           (4.3)
                        The numerical values of A, B, C, and D for substitution into Eq. (4.3) are found in Table 4.5.
                      A more empirical method to find pHs is to use the chart in Fig. 4.2.

                      RYZNAR STABILITY INDEX (RI)


                      Also referred to as simply the stability index (SI), the RI is an empirical method used to
                      predict scale-forming tendencies of water. The RI is calculated from the following formula
                      using the same definitions used for the LSI:
                                                RI = 2 pHs − pH                    (4.4)

                        The RI is always positive. When it falls below 6.0, scale formation is possible and becomes
                      more probable with decreasing RI. For an interpretation of the RI, refer to Table 4.6.

                      TABLE 4.5  Numerical Values for Substitution in Eq. (4.3) to Find the pHs of Saturation of Water
                      Total solids   A      Ca as CaCO 3   C        M alkalinity    D

                        50–330     0.1        10–11       0.6         10–11        1.0
                      400–1000     0.2        12–13       0.7         12–13        1.1
                                              14–17       0.8         14–17        1.2
                      Temp, °F     B
                                              18–22       0.9         18–22        1.3
                        32–34      2.6        23–27       1.0         23–27        1.4
                        36–42      2.5        28–34       1.1         28–35        1.5
                        44–48      2.4        35–43       1.2         36–44        1.6
                        50–56      2.3        44–55       1.3         45–55        1.7
                        58–62      2.2        56–69       1.4         56–69        1.8
                        64–70      2.1        70–87       1.5         70–88        1.9
                        72–80      2.0          88–110    1.6           89–110     2.0
                        82–88      1.9       111–138      1.7        111–139       2.1
                        90–98      1.8       139–174      1.8        140–176       2.2
                      100–110      1.7       175–220      1.9        177–220       2.3
                      112–122      1.6       230–270      2.0        230–270       2.4
                      124–132      1.5       280–340      2.1        280–340       2.5
                      134–146      1.4       350–430      2.2        350–440       2.6
                      148–160      1.3       440–550      2.3        450–550       2.7
                      162–178      1.2       560–690      2.4        560–690       2.8
                      178–194      1.1       700–870      2.5        700–880       2.9
                      194–210      1.0         880–1,000   2.6         890–1,000   3.0




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