Abstract
Naturally-occurring thorium isotopes and corresponding Ra-Th disequilibrium in aquatic system are good tracers for particle dynamic processes. Here we reported a case study on the occurrence of 228Thex-228Ra disequilibrium in sediments of a shallow estuary-coastal bay system (Zhangjiang Estuary-Dongshan Bay). 228Ra activity concentration in saline water and 228Ra and 228Th activities in the surface sediments were measured and we found 228Ra’s non-conservative behavior in saline water and the existence of excess 228Th (228Thex = 228Th-228Ra) in surficial sediments at all the stations. Spatially, 228Thex gradually decreased from the Zhangjiang Estuary (16 Bq/kg) to the inner Dongshan Bay (8–11 Bq/kg), which is consistent with the variation trend of 228Ra activity concentration in seawater. This consistency explained the reason for the occurrence of 228Ra-228Th disequilibrium (or called “228Thex occurrence”) in the surface sediments. Because 228Ra activity concentration is very high in estuarine water, and 228Th continues to decay from 228Ra, and the newly formed 228Th is quickly cleared by suspended particles in the water and subsequently settles down to the seabed sediments. Based on a constructed simple irreversible scavenging model, the residence time of 228Thex was constrained to be 15–30 days in the estuary and to be 5–11 days in the inner bay. These results show that Th and other similarly particle-reactive trace metals will be scavenged rapidly from the water column of shallow estuary-bay systems.
Graphical abstract
Similar content being viewed by others
References
Marsan D, Rigaud S, Church T (2014) Natural radionuclides 210Po and 210Pb in the Delaware and Chesapeake estuaries: modeling scavenging rates and residence times. J Environ Radioact 138:447–455
Roy-Barman M, Chen JH, Wasserburg GJ (1996) 230Th-232Th systematics in the Central Pacific Ocean: the sources and the fates of thorium. Earth Planet Sci Lett 139:351–363
Zhang L, Chen M, Yang WF, Xing N, Li YP, Qiu YS, Huang YP (2005) Size-fractionated thorium isotopes (228Th, 230Th, 232Th) in surface waters in the Jiulong River estuary, China. J Environ Radioact 78:199–216
Yang W, Chen M, Zhang X, Guo Z, Li G, Ma Q, Yang J, Huang Y (2013) Thorium isotopes (228Th, 230Th, 232Th) and applications in reconstructing the Yangtze and Yellow River floods. Int J Sediment Res 28(4):588–595
Turekian KK, Cochran JK, Nozaki Y, Thompson I, Jones DS (1982) Determination of shell deposition rates of arctica islandica from the new york bight using natural 228Ra and 228Th and bomb-produced 14C. Limnol Oceanogr 27(4):737–741
Lin W, Yu K, Wang Y, Liu X, Xu S, He B, Ning Q, Li Y, Deng F, Wang J, Ma H (2021) Assessing the feasibility of the 228Th/228Ra dating method for young corals (<10 a) by gamma spectrometry. Quat Geochronol 61:101125
Hancock GJ, Hunter JR (1999) Use of excess 210Pb and 228Th to estimate rates of sediment accumulation and bioturbation in Port Phillip Bay, Australia. Mar Freshwater Res 50:533–545
Cochran JK, Buesseler KO, Bacon MP, Wang HW, Hirschberg DJ, Ball L, Andrews J, Crossin G, Fleer A (2000) Short-lived thorium isotopes (234Th, 228Th) as indicators of POC export and particle cycling in the Ross Sea, Southern Ocean. Deep Sea Res Part II 47:3451–3490
Tamborski J, Cai P, Eagle M, Henderson P, Charette M (2022) Revisiting 228Th as a tool for determining sedimentation and mass accumulation rates. Chem Geol 607:121006
Moore WS, Sarmiento JL, Key RM (2008) Submarine groundwater discharge revealed by 228Ra distribution in the upper Atlantic Ocean. Nat Geosci 1(5):309–311
Rodellas V, Garcia-Orellana J, Trezzi G, Masque P, Stieglitz TC, Bokuniewicz H, Cochran JK, Berdalet E (2017) Using the radium quartet to quantify submarine groundwater discharge and porewater exchange. Geochim Cosmochim Acta 196:58–73
Rodellas V, Garcia-Orellana J, Tovar-Sánchez A, Basterretxea G, López-Garcia JM, Sánchez-Quiles D, Garcia-Solsona E, Masqué P (2014) Submarine groundwater discharge as a source of nutrients and trace metals in a Mediterranean bay (Palma Beach, Balearic Islands). Mar Chem 160:56–66
Hong Q, Cai P, Walter G, Cao Z, Ingrid S, Liu L, Li Q (2018) Benthic fluxes of metals into the Pearl River Estuary based on 224Ra/228Th disequilibrium: from alkaline earth (Ba) to redox sensitive elements (U, Mn, Fe). Geochim Cosmochim Acta 237:223–239
Koide M, Bruland KW, Goldberg ED (1973) Th-228/Th-232 and Pb-210 geochronologies in marine and lake sediments. Geochim Cosmochim Acta 37:1171–1187
Huh CA, Zahnle DL, Small LF, Noshkin VE (1987) Budgets and behaviours of uranium and thorium series isotopes in Santa Monica Basin sediments. Geochim Cosmochim Acta 51:1743–1754
Wang Q, Sha Z, Wang J, Zhong Q, Du J (2020) Vertical distribution of radionuclides in Lake Qinghai, Qinghai-Tibet Plateau, and its environmental implications. Chemosphere 259:127489
Santschi PH, Li YH, Bell J (1979) Natural radionuclides in the water of Narrangansett Bay. Earth Planet Sci Lett 45:201–213
McKee BA, DeMaster DJ, Nittrouer CA (1986) Temporal variability in the partitioning of thorium between dissolved and particulate phases on the Amazon Shelf: implications for the scavenging of particle reactive species. Cont Shelf Res 6(1/2):87–106
Chen Y, Li Y, Cai T, Thompson C, Li Y (2016) A comparison of biohydrodynamic interaction within mangrove and saltmarsh boundaries. Earth Surf Processes Landforms 41(13):1967–1979
Yu X, Liu J, Chen X, Huang D, Yu T, Peng T, Du J (2022) Submarine groundwater-derived inorganic and organic nutrients vs. mariculture discharge and river contributions in a typical mariculture bay. J Hydrol 613:128342
Men W, Jiang Y, Liu G, Wang F, Zhang Y (2016) Study of water mixing in the coastal waters of the western Taiwan Strait based on radium isotopes. J Environ Radioact 152:16–22
Liu J, Yu X, Chen X, Du J, Zhang F (2021) Utility of radium quartet for evaluating porewater-derived carbon to a saltmarsh nearshore water: implications for blue carbon export. Sci Total Environ 764:144238
Moore WS (1976) Sampling 228Ra in the deep ocean. Deep-Sea Res Oceanogr Abstr 23:647–651
Charette MA, Buesseler KO, Andrews JE (2001) Utility of radium isotopes for evaluating the input and transport of groundwater-derived nitrogen to a Cape Cod estuary. Limnol Oceanogr 46(2):465–470
Krest JM, Moore WS, Rama, (1999) 226Ra and 228Ra in the mixing zones of the Mississippi and Atchafalaya Rivers: indicators of groundwater input. Mar Chem 64:129–152
Liu J, Su N, Wang X, Du J (2017) Submarine groundwater discharge and associated nutrient fluxes into the Southern Yellow Sea: A case study for semi-enclosed and oligotrophic seas-implication for green tide bloom. J Geophys Res Oceans 122:139–152
Key RM, Stallard RF, Moore WS, Sarmiento JL (1985) Distribution and flux of 226Ra and 228Ra in the Amazon River estuary. J Geophys Res Oceans 90(C4):6995–7004
Webster IT, Hancock GJ, Murray AS (1995) Modelling the effect of salinity on radium desorption from sediments. Geochim Cosmochim Acta 59(12):2469–2476
Luo H, Li L, Wang J, Zhong Q, Du J (2019) The desorption of radium isotopes in river sediments in Qinzhou Bay. J Ocean Univ 41(4):27–41
Li L, Zhong Q, Du J (2021) Radium desorption behavior of riverine suspended sediment: theoretical and experimental. J Environ Radioact 234(7):106644
Su W, Ma Y, Wang Q, Yan Q, Lu X, Ma Z, Yi L, Liu X, Chen F, Han F, Xu Z (2022) Effects of salinity and particle size on radium desorption from river sediments in the Qinghai-Tibet Plateau. J Environ Radioact 241:106771
Zhong Q, Wang H, Wang Q, Chen S, Lin J, Huang D, Yu T (2023) Study of Ra desorption processes in an estuary system with high-turbidity at the Southeast China. J Environ Radioact 259–260:107108
Wang J, Du J, Baskaran M, Zhang J (2016) Mobile mud dynamics in the East China Sea elucidated using 210Pb, 137Cs, 7Be, and 234Th as tracers. J Geophys Res Oceans 121:224–239
Gao Y, Arimoto R, Duce RA, Lee DS, Zhou MY (1992) Input of atmospheric trace elements and mineral matter to the Yellow Sea during the spring of a low-dust year. J Geophys Res 97(D4):3767–3777
Zhong Q, Guo W, Wang H, Ji J, Lin J, Du J, Huang D, Yu T (2023) 210Po and 210Pb as tracers for particle cycling in a shallow semi-enclosed bay of Taiwan Strait. Deep Sea Res Part II 207:105228
Acknowledgements
This work was supported by the National Natural Science Foundation of China (No. 42206166).
Funding
Funding was provided by National Natural Science Foundation of China (No. 42206166).
Author information
Authors and Affiliations
Contributions
Conceptualization: [Qiangqiang Zhong]; Methodology: [Wenqing Zhou]; Formal analysis and investigation: [Da Zhou]; Writing—original draft preparation: [Wenqing Zhou, Yi Shao, Da Zhou, Qiangqiang Zhong, Jianda Ji]; Writing—review and editing: [Qiangqiang Zhong]; Funding acquisition: [Qiangqiang Zhong]; Supervision: [Jianda Ji].
Corresponding authors
Ethics declarations
Conflict of interest
The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.
Additional information
Publisher's Note
Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
Rights and permissions
Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.
About this article
Cite this article
Zhou, W., Zhong, Q., Shao, Y. et al. Evaluation of excess Th-228 in surface bottom sediment of shallow marine ecosystem: a case study from Dongshan Bay. J Radioanal Nucl Chem (2024). https://doi.org/10.1007/s10967-024-09518-2
Received:
Accepted:
Published:
DOI: https://doi.org/10.1007/s10967-024-09518-2