2017
DOI: 10.1364/oe.25.002840
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New approach to remote sensing of temperature and salinity in natural water samples

Abstract: Raman spectra for a natural water sample have been comprehensively investigated as a function of temperature and salinity, and we demonstrate that temperature and salinity can be determined from Raman spectra with RMS errors consistently below ±0.2 °C and ±0.6 PSU respectively where there is variation only in one parameter. Most significantly, we have applied multivariate methods to show that both temperature and salinity can be determined simultaneously from Raman spectra with RMS errors of ±0.7 °C and ±1.4 P… Show more

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Cited by 25 publications
(14 citation statements)
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“…Raman spectroscopy has proven to be an effective technique for determining water temperature in the laboratory with high accuracies of up to ±0.1 °C and ±0.5 °C using two-colour or depolarization markers, respectively [11,24]. The reports in [23,25,26] propose the possibility of measuring subsurface water temperature using Raman spectroscopy in combination with LIDAR methods, collecting time-resolved Raman signals in channels selected by optical filters. This is the ultimate goal of our research project.…”
Section: Introductionmentioning
confidence: 99%
“…Raman spectroscopy has proven to be an effective technique for determining water temperature in the laboratory with high accuracies of up to ±0.1 °C and ±0.5 °C using two-colour or depolarization markers, respectively [11,24]. The reports in [23,25,26] propose the possibility of measuring subsurface water temperature using Raman spectroscopy in combination with LIDAR methods, collecting time-resolved Raman signals in channels selected by optical filters. This is the ultimate goal of our research project.…”
Section: Introductionmentioning
confidence: 99%
“…Artlett and Pask have shown that both temperature and chlorinity significantly affect changes in Raman parameter dependent variables. 40 Therefore, the chlorinity calibration model should fully consider temperature and chlorinity. Accounting for the changes in chlorinity due to phase separation and water/rock reactions, 41,42 the chlorinity and temperature ranges for this study were set at 0-3.0 mol/ kg NaCl and 0-300 C, respectively, which cover the chlorinity and temperature levels of most hydrothermal fluids.…”
Section: Building the Chlorinity Calibration Modelmentioning
confidence: 99%
“…According to simulations performed by Artlett and Pask (2015) for ultrapure (Reverse-Osmosis) water, an optimum trade-off between Raman signals strength and RMSTEs would be obtained for acquisition channels with spectral widths of around 200 cm −1 . Optimum spectral positions for such channels were explored using simulations in Artlett and Pask (2017), with the "low shift" channel central position at 3,200 cm −1 and the "high shift" channel central position at 3,600 cm −1 . The availability of commercial Band Pass filters within these conditions is extremely limited, therefore the differences between spectral widths for channels collecting signals in the blue (254 and 136 cm −1 ) TABLE 3 | RMSTEs (± • C), sensitivities (% change/ • C), and absolute percentage errors in markers (%) for natural water sample analyzed by two-color and depolarisation markers.…”
Section: Considering the Relative Merits Of Spectrometers Using Blue mentioning
confidence: 99%