Research Article

Understanding the Compositional Variability of the Major Components of Hydrothermal Plumes in the Okinawa Trough

Table 2

Major component ratios of hydrothermal plume water columns in the middle and southern Okinawa Trough.

Iheya NorthClamYonaguni Knoll IVTangyinAverage seawater
AverageRangeAverageRangeAverageRangeAverageRange

Sr2+/Ca2+0.008 ()0.007–0.0110.008 ()0.008–0.0090.009 ()0.008–0.0100.009 ()0.008–0.0090.009
Mg2+/Cl-0.095 ()0.091–0.0990.094 ()0.090–0.0970.093 ()0.091–0.0950.092 ()0.087–0.0960.097
Mn2+/Cl-2.97 × 10−8 ()1.89 × 10−9–1.13 × 10−7
Mg2+/Ca2+5.40 ()4.97–5.825.28 ()5.01–5.685.32 ()5.08–5.565.38 ()5.19–5.565.17
B3+/Ca2+0.038 ()0.033–0.0500.037 ()0.034–0.0400.048 ()0.043–0.0540.039 ()0.036–0.0410.040
Ca2+/Cl-0.018 ()0.016–0.0190.018 ()0.017–0.0190.017 ()0.016–0.0190.017 ()0.016–0.0180.019
Ca2+/salinity0.291 ()0.263–0.3200.298 ()0.283–0.3160.291 ()0.278–0.3070.287 ()0.275–0.3060.293
Mg2+/salinity1.57 ()1.48–1.691.57 ()1.51–1.621.55 ()1.51–1.581.54 ()1.49–1.621.52
/salinity0.793 ()0.760–0.8600.801 ()0.775–0.8200.796 ()0.779–0.8100.800 ()0.772–0.8160.807
Mn2+/salinity2.07 × 10−4 ()2.81 × 10−5–10.8 × 10−44.92 × 10−4 ()3.18 × 10−5–1.88 × 10−32.08 × 10−4
B3+/salinity0.011 ()0.010–0.0130.011 ()0.010–0.0150.014 ()0.013–0.0150.011 ()0.011–0.0120.012
Na+/salinity14.4 ()13.2–16.014.5 ()13.4–15.514.5 ()13.5–15.214.2 ()13.3–15.113.4
Total S/salinity0.831 ()0.783–0.8890.838 ()0.807–0.8790.816 ()0.785–0.8550.804 ()0.788–0.8340.806
K+/salinity0.301 ()0.282–0.3260.303 ()0.288–0.3160.307 ()0.295–0.3270.305 ()0.284–0.3210.286
Sr2+/salinity2.47 ()2.13–2.892.51 ()2.29–2.842.60 ()2.44–2.752.52 ()2.44–2.652.64
Cl-/salinity16.6 ()15.9–17.816.7 ()16.3–17.016.7 ()16.5–17.016.8 ()16.4–17.215.6
F-/salinity0.021 ()0.019–0.0240.020 ()0.017–0.0220.019 ()0.018–0.0250.020 ()0.018–0.0230.020
Potential density/salinity0.775 ()0.681–0.7930.784 ()0.697–0.7940.785 ()0.677–0.7940.784 ()0.672–0.794

“–”: no data. Average seawater data from Turekian [50] and Millero [4].