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Raman spectrum of CCl 4 after extraction after conventional experimental setup. 

Raman spectrum of CCl 4 after extraction after conventional experimental setup. 

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The levels of dissolved sulfate and methane are crucial indicators in the geochemical analysis of pore water. Compositional analysis of pore water samples obtained from sea trials was conducted using Raman spectroscopy. It was found that the concentration of SO42- in pore water samples decreases as the depth increases, while the expected Raman sign...

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... 4 is immiscible with water. Thus, the trace CH 4 dissolved in water is enriched into CCl 4 after the extraction. Then, the CCl 4 after extraction is taken as samples for Raman spectrum acquisition. The molecular density of CH 4 ( C in Equation (1)) in CCl 4 is much bigger than that in H 2 O. Finally, the Raman spectrum of CCl 4 after the extraction acquired by the conventional experimental setup with an integration time of 0.1 s, which is an average result of ten measurements, is shown in Figure 9. The Raman peak of methane is located at 2907 cm and can be clearly observed in Figure 9. This indicates that, after the extraction, the methane dissolved in water is enriched into the CCl 4 . The preliminary result shows that the methane dissolved in water with concentration below 1.14 mmol/L could be indirectly detected assisted by CCl 4 extraction. There are still many opportunities for optimizing this approach, and there is a long way to go in order to achieve a quantitative analysis of methane dissolved in water. For the compositional analysis of pore water, Raman spectra of the pore water samples obtained from the sea trials were acquired. According to the linear function obtained from the calibration curve, the concentration of SO 42 − in pore water is inversely calculated according to the linear function obtained from the calibration curve. It is found that the concentration of SO 42 − in pore water samples decreases as the depth increases. However, methane cannot be detected using Raman spectroscopy because of its low concentration. Two approaches are proposed and used for a better analysis of pore water samples. One approach uses a LCOF as a sample container to enlarge the optical path length for detection of SO 42 − . The other approach is an enrichment process for methane with CCl 4 extraction. With the assistance of a LCOF whose physical length is 50 cm, the LOD of Raman spectroscopy is significantly improved, and the Raman signal of SO 42 − is amplified over 10 times compared to that obtained with a conventional Raman experimental setup. By the means of extraction, the trace methane dissolved in water is enriched into CCl 4 because the solubility of methane in water and CCl 4 differs immensely. Hence ...
Context 2
... 4 is immiscible with water. Thus, the trace CH 4 dissolved in water is enriched into CCl 4 after the extraction. Then, the CCl 4 after extraction is taken as samples for Raman spectrum acquisition. The molecular density of CH 4 ( C in Equation (1)) in CCl 4 is much bigger than that in H 2 O. Finally, the Raman spectrum of CCl 4 after the extraction acquired by the conventional experimental setup with an integration time of 0.1 s, which is an average result of ten measurements, is shown in Figure 9. The Raman peak of methane is located at 2907 cm and can be clearly observed in Figure 9. This indicates that, after the extraction, the methane dissolved in water is enriched into the CCl 4 . The preliminary result shows that the methane dissolved in water with concentration below 1.14 mmol/L could be indirectly detected assisted by CCl 4 extraction. There are still many opportunities for optimizing this approach, and there is a long way to go in order to achieve a quantitative analysis of methane dissolved in water. For the compositional analysis of pore water, Raman spectra of the pore water samples obtained from the sea trials were acquired. According to the linear function obtained from the calibration curve, the concentration of SO 42 − in pore water is inversely calculated according to the linear function obtained from the calibration curve. It is found that the concentration of SO 42 − in pore water samples decreases as the depth increases. However, methane cannot be detected using Raman spectroscopy because of its low concentration. Two approaches are proposed and used for a better analysis of pore water samples. One approach uses a LCOF as a sample container to enlarge the optical path length for detection of SO 42 − . The other approach is an enrichment process for methane with CCl 4 extraction. With the assistance of a LCOF whose physical length is 50 cm, the LOD of Raman spectroscopy is significantly improved, and the Raman signal of SO 42 − is amplified over 10 times compared to that obtained with a conventional Raman experimental setup. By the means of extraction, the trace methane dissolved in water is enriched into CCl 4 because the solubility of methane in water and CCl 4 differs immensely. Hence ...

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... In the aerobic sedimentary environment, the Permian Chihsian Formation in South China has deposited a wide range of carbonate and bioclastic, in which aragonite and organic matter accounted for a significant proportion (Sandberg, 1983;Yan and Wu, 2006). A large amount of sulfate, the main sulfur compound in seawater, could be preserved in pore water with no reduction (Du et al., 2015). Dissolved oxygen oxidized organic matter and led to the release of CO 2 (R1) (Fig. 9a). ...
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