Figure 4 | Scientific Reports

Figure 4

From: Brillouin spectroscopy of fluid inclusions proposed as a paleothermometer for subsurface rocks

Figure 4

Determination of TX with Brillouin spectroscopy for salt bearing FIs.

(a) Comparison of Raman spectra at 20 °C (all normalized to unit area). The blue curve shows the OH stretching band of pure water. The spectrum from FI4 (red) exhibits a decrease at low shift and increase at high shift, typical of dissolved salt. A standard procedure37 yields an equivalent NaCl molality mRaman = 1.25 ± 0.05 mol kg−1. The spectrum from a bulk aqueous solution of 1.25 molal NaCl is also shown (black) for direct comparison. (b) Brillouin shift ΔfB as a function of temperature for reference NaCl solutions. The curves designated by the solution molality m (in mol kg−1) were calculated from literature data (see Methods). They agree well with the corresponding experimental data (symbols). (c) ΔfB(T) for FI4, with (open symbols) or without (closed symbols) bubble. The thin black curve is the calculated for a NaCl solution with molality 1.20 mol kg−1. The thick red curve is the result of the linear fitting procedure on ; it intersects at TX. (d) Uncertainty δTX (± 1 standard deviation) on TX determined with Brillouin spectroscopy, as a function of TX. The solid curves were calculated with equation (4) (see Methods) for pure water and NaCl solutions with designated molalities (in mol kg−1). The marker shows the error on TX from the linear fitting procedure for FI3, as given in Table 1.

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