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Evaluation of the Possibility of Developing Organic Matter Indicators in Coastal Environments: Utilization of Dissolved Organic Carbon and Fluorescent Dissolved Organic Matter

연안환경에서 유기물 지표 개발을 위한 가능성 평가: 용존유기탄소와 형광용존유기물질 활용

  • Lee, Min-Young (Faculty of Earth System and Environmental Sciences, College of Natural Sciences, Chonnam National University) ;
  • Yang, Kyungsun (Faculty of Earth System and Environmental Sciences, College of Natural Sciences, Chonnam National University) ;
  • Kim, Sunchan (Jeju Special Self-Governing Province Ocean and Fisheries Research Institute) ;
  • Kim, Tae-Hoon (Faculty of Earth System and Environmental Sciences, College of Natural Sciences, Chonnam National University)
  • 이민영 (전남대학교 자연과학대학 지구환경과학부) ;
  • 양경선 (전남대학교 자연과학대학 지구환경과학부) ;
  • 김순찬 (제주특별자치도 해양수산연구원) ;
  • 김태훈 (전남대학교 자연과학대학 지구환경과학부)
  • Received : 2021.04.21
  • Accepted : 2021.06.03
  • Published : 2021.06.30

Abstract

In order to evaluate the dissolved organic carbon (DOC) and fluorescent dissolved organic matter (FDOM), as indicators of organic matter in the coastal environments, we measured the concentrations of DOC, FDOM, and chemical oxygen demand (COD) in saline groundwater (Woljeong, Pyoseon, and Hwasun beaches) and coastal seawater (Haengwon, Gwideok, Pyoseon, and Yeongnak) in Jeju, Korea. The highest concentrations of DOC and COD in groundwater were found in Woljeong and Pyoseon, and those in coastal water were observed in Haengwon and Pyoseon, indicating that the higher concentrations of DOC and COD seem to be associated with saline groundwater-driven dissolved organic matter (DOM) and/or biogeochemical processes. According to origin and optical properties of DOM using FDOM as a tracer, proportion of humic-like FDOM, more refractory DOM, was relatively greater in the groundwater than in the coastal water. With regard to this result, there was no relationship between DOC and COD in groundwater, while DOC showed a good positive correlation (r2 = 0.66) with COD in coastal water. This result indicates that COD as an indicator of assessment of DOM has a limitation in which it is difficult to quantify refractory DOM. Although DOC is a potential alternative to COD in the coastal environments, particulate organic carbon cannot be negligible due to relatively higher concentration compared to the open ocean. Therefore, the use of total organic carbon (TOC) as a replacement of COD in the coastal ocean is important, and the evaluation criterion of the TOC is necessary in order to evaluate of organic matter indicator in the various coastal environments.

Keywords

Acknowledgement

이 논문은 2021년 해양수산부 재원으로 해양수산과학기술진흥원의 지원을 받아 수행된 연구입니다(전남씨그랜트).

References

  1. KMGL (2020) Basic environment law. http://www.law.go.kr 27 May 2021
  2. KMA (2021) Domestic climate data. http://weather.go.kr 7 Jun 2021
  3. Park KH (2013) Experience the geological splendor of Jeju Island. Jeju Research institute
  4. Song YS (2006) Evaluation of KMnO4 Spectrophotometry and KMnO4 Titration Method for the Determination of Chemical Oxygen demand. M.S. Thesis, Yonsei University
  5. MOF (2013) [Notice of Ministry of Oceans and Fisheries No. 2013-230] The Korean standards methods for Marine Environment. chapter 4 paragraph 8, pp 39-43
  6. Cho HM, Kim TH, Moon JH, Song BC, Hwang DW, Kim TJ, Im DH (2021) Estimating submarine groundwater discharge in Jeju volcanic island (Korea) during a typhoon (Kong-rey) using humic-fluorescent dissolved organic matter-Si mass balance. Sci Rep 11(1):1-10 https://doi.org/10.1038/s41598-020-79139-8
  7. Cho YB, Oh YK, Shin DC, Park CH (2014) Distribution of total organic carbon and correlations between organic matters of sewage treatment plants. J Korean Soc Environ Anal 17:207-214
  8. Choi JY, Han DH (2011) Development of water quality standard for TOC as organic matter index. Seoul STUD 12(3):173-184
  9. Coble PG (2007) Marine optical biogeochemistry: the chemistry of ocean color. Chem Rev 107(2):402-418 https://doi.org/10.1021/cr050350+
  10. Han H, Hwang J, Kim G (2021) Characterizing the origins of dissolved organic carbon in coastal seawater using stable carbon isotope and light absorption characteristics. Biogeosciences 18(5):1793-1801 https://doi.org/10.5194/bg-18-1793-2021
  11. Jung KY, Park MH, Hur J, Lee SY, Shin JK (2009) Comparison of spectroscopic characteristics and chemical oxygen demand efficiencies for dissolved organic matters from diverse sources. J Korean Soc Water Environ 25(4):589-596
  12. Kim BC, Jung SM, Jang CW, Kim JK (2007) Comparison of BOD, COD and TOC as the indicator of organic matter pollution in streams and reservoirs of Korea. J Korean Soc Environ Eng 29(6):640-643
  13. Kim G, Lee K-K, Park HS, Hwang DW, Yang HS (2003) Large submarine groundwater discharge (SGD) from a volcanic island. Geophys Res Lett 30:2098. doi:10.1029/2003GL018378
  14. Kim JH, Kim GB (2017) Inputs of humic fluorescent dissolved organicmatter via submarine groundwater discharge to coastal waters off a volcanic island (Jeju Island). Sci Rep 7(1):1-9 https://doi.org/10.1038/s41598-016-0028-x
  15. Kim SK, Choi YC, Kim JS (2008) Distribution of dissolved and particulate organic carbon in the East China Sea in summer. J Korean Soc Mar Environ 11(3):124-131
  16. Kim TH, Kim GB (2010) Distribution of dissolved organic carbon (DOC) in the southwestern east sea in summer. Ocean Polar Res 32(3):291-297 https://doi.org/10.4217/OPR.2010.32.3.291
  17. Lee SA, Kim GB (2018) Sources, fluxes, and behaviors of fluorescent dissolved organic matter (FDOM) in the Nakdong River Estuary, Korea. Biogeosciences 15(4):1115-1122 https://doi.org/10.5194/bg-15-1115-2018
  18. Oh YH, Lee YW, Kim TH (2018) In situ production of dissolved organic carbon (DOC) by phytoplankton blooms (Cochlodinium polykrikoides) in the southern sea of Korea. J Sea Res 138:19-23 https://doi.org/10.1016/j.seares.2018.05.004
  19. Son JW, Park YC, Lee HJ (2003) Characteristics of total organic carbon and chemical oxygen demand in the coastal waters of Korea. J Korean Soc Ocean 8(3):317-326