Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/34533
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dc.contributor.authorYuan, Xiaojie-
dc.contributor.authorGuo, Zhanrong-
dc.contributor.authorLi, Wenquan-
dc.contributor.authorLiu, Jie-
dc.contributor.authorMa, Zhiyong-
dc.contributor.authorWang, Bo-
dc.date.accessioned2016-06-28T09:18:51Z-
dc.date.available2016-06-28T09:18:51Z-
dc.date.issued2014-10-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://hdl.handle.net/123456789/34533-
dc.description1811-1819en_US
dc.description.abstractSubmarine groundwater discharge (SGD) is part of the global water cycles, which delivers a large amount of solutes to the biogeochemical cycle and affects the coastal ecological environment. Natural radium isotopes (224Ra and 226Ra) were used to estimate the SGD in Jiaozhou Bay and the mass balance models were established.  Radium sources including river transport, sediment diffusion, desorption from re-suspended particles, open sea flood tide, municipal wastewater, and SGD are considered. Radium output owning to the radioactive decay and ebb tide are also considered. Our results show the SGD fluxes during September to October in 2011(autumn) and April to May in 2012 (spring) are 15.17 and 6.53×106 m3·d-1, respectively. In the same period of time, the input of the dissolved inorganic nitrogen (DIN) from SGD is very close to that from river, yet, the soluble silicate and reactive phosphate vary seasonally. SGD is the major source of the nutrient input of Jiaozhou Bay.en_US
dc.language.isoen_USen_US
dc.publisherNISCAIR-CSIR, Indiaen_US
dc.rights CC Attribution-Noncommercial-No Derivative Works 2.5 Indiaen_US
dc.sourceIJMS Vol.43(10) [October 2014]en_US
dc.subjectSubmarine groundwater dischargeen_US
dc.subjectRadium isotopeen_US
dc.subjectGroundwateren_US
dc.subjectNutrienten_US
dc.subjectJiaozhou bayen_US
dc.titleEstimating submarine groundwater discharge in the Jiaozhou Bay using radium isotopesen_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.43(10) [October 2014]

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