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Peng Yajun, Wang Yujue, Liu Dongyan, Tang Danling. Acid treatment effects on the carbon stable isotope values of marine sediments[J]. Haiyang Xuebao, 2015, 37(12): 85-92. doi: 10.3969/j.issn.0253-4193.2015.12.009
Citation: Peng Yajun, Wang Yujue, Liu Dongyan, Tang Danling. Acid treatment effects on the carbon stable isotope values of marine sediments[J]. Haiyang Xuebao, 2015, 37(12): 85-92. doi: 10.3969/j.issn.0253-4193.2015.12.009

Acid treatment effects on the carbon stable isotope values of marine sediments

doi: 10.3969/j.issn.0253-4193.2015.12.009
  • Received Date: 2015-06-01
  • Rev Recd Date: 2015-09-09
  • Carbon stable isotope ratio(δ13C) has been regarded as an important factor tracing the organic material sources in marine ecosystem. Prior to analysis,samples have to be decarbonated. Inorganic carbon content and component are different in different marine sediments,and appropriate decarbonate methods should be chosen to get exact results. This study compared the effects of three acid treatments on δ13C values during the decarbonation of estuarial and bay sediments with different inorganic carbon content. The results showed that for the first method(rinse method),6% H2SO3 and 1 mol/L H3PO4 could not remove inorganic carbon in high inorganic carbon content samples collecting from tropical estuarial and bay completely,while 2 mol/L HCl could remove inorganic carbon in all marine sediments completely. The second method(fumigation method) is not suitable for sediment samples with high inorganic carbon content from tropical estuarial and bay,but could be used for sediments with lower inorganic carbon content,and it showed that 9 h is the best fumigate time. δ13C values obtained from the third method(non-capsule method) showed more positive values compared to the other two methods,indicated that the third method did not damage the 13C enriched materials. Also the residual acid showed not impact the δ13C values in the third method. The third method is confirmed as the most appropriate acid treatment for decarbonation of marine sediments.
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