Tracing surface seawater mixing and nutrient transport by 222Rn on the northern coast of Beibu Gulf, China

The transport and diffusion of substances in seawater are limited by the mixing motion of water bodies, while the main forms of mixing in offshore water bodies are advection and eddy diffusion. The eddy diffusion process of water indicates the possible transport direction of dissolved substances. Ho...

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Veröffentlicht in:Acta oceanologica Sinica 2023-08, Vol.42 (8), p.87-98
Hauptverfasser: Wang, Hao, Zhong, Qiangqiang, Zhang, Fule, Chen, Suiyuan, Bao, Hongyan, Lin, Jing, Huang, Dekun, Yu, Tao
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container_title Acta oceanologica Sinica
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Zhong, Qiangqiang
Zhang, Fule
Chen, Suiyuan
Bao, Hongyan
Lin, Jing
Huang, Dekun
Yu, Tao
description The transport and diffusion of substances in seawater are limited by the mixing motion of water bodies, while the main forms of mixing in offshore water bodies are advection and eddy diffusion. The eddy diffusion process of water indicates the possible transport direction of dissolved substances. However, the complex environment in the coastal zone makes it difficult to quantitatively assess the water diffusion process. 222 Rn is a useful tool to trace the diffusion process of water bodies. However, studies on the 222 Rn distribution and its behavior in the Beibu Gulf are scarce. In this study, the activity distribution characteristics of 222 Rn in surface seawater of the Guangxi shelf area of the Beibu Gulf were measured. Based on the one-dimensional, steady-state model, the vorticity diffusion coefficient of 222 Rn in the horizontal direction was calculated as (0.42–2.13) × 10 8 m 2 /d, and the offshore fluxes of 222 Rn under the influence of water mixing were calculated as 2.00 × 10 12 Bq/d. Correspondingly, the horizontal transport fluxes of silicate, phosphate, nitrite and nitrate were 6.28 × 10 −3 mol/(m 2 ·d), 0.10 × 10 −3 mol/(m 2 ·d), 0.20 × 10 −3 mol/(m 2 ·d) and 4.15 × 10 −3 mol/(m 2 ·d), respectively. These results indicate that the study of eddy current diffusion in offshore marine water facilitates a deeper understanding of the water mixing process and nutrient transport and migration.
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The eddy diffusion process of water indicates the possible transport direction of dissolved substances. However, the complex environment in the coastal zone makes it difficult to quantitatively assess the water diffusion process. 222 Rn is a useful tool to trace the diffusion process of water bodies. However, studies on the 222 Rn distribution and its behavior in the Beibu Gulf are scarce. In this study, the activity distribution characteristics of 222 Rn in surface seawater of the Guangxi shelf area of the Beibu Gulf were measured. Based on the one-dimensional, steady-state model, the vorticity diffusion coefficient of 222 Rn in the horizontal direction was calculated as (0.42–2.13) × 10 8 m 2 /d, and the offshore fluxes of 222 Rn under the influence of water mixing were calculated as 2.00 × 10 12 Bq/d. Correspondingly, the horizontal transport fluxes of silicate, phosphate, nitrite and nitrate were 6.28 × 10 −3 mol/(m 2 ·d), 0.10 × 10 −3 mol/(m 2 ·d), 0.20 × 10 −3 mol/(m 2 ·d) and 4.15 × 10 −3 mol/(m 2 ·d), respectively. 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Based on the one-dimensional, steady-state model, the vorticity diffusion coefficient of 222 Rn in the horizontal direction was calculated as (0.42–2.13) × 10 8 m 2 /d, and the offshore fluxes of 222 Rn under the influence of water mixing were calculated as 2.00 × 10 12 Bq/d. Correspondingly, the horizontal transport fluxes of silicate, phosphate, nitrite and nitrate were 6.28 × 10 −3 mol/(m 2 ·d), 0.10 × 10 −3 mol/(m 2 ·d), 0.20 × 10 −3 mol/(m 2 ·d) and 4.15 × 10 −3 mol/(m 2 ·d), respectively. These results indicate that the study of eddy current diffusion in offshore marine water facilitates a deeper understanding of the water mixing process and nutrient transport and migration.</description><subject>Advection</subject><subject>Climatology</subject><subject>Coastal zone</subject><subject>Coastal zones</subject><subject>Diffusion coefficient</subject><subject>Direction</subject><subject>Distribution</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Ecology</subject><subject>Eddy currents</subject><subject>Eddy diffusion</subject><subject>Engineering Fluid Dynamics</subject><subject>Environmental Chemistry</subject><subject>Fluxes</subject><subject>Horizontal orientation</subject><subject>Marine &amp; Freshwater Sciences</subject><subject>Mixing</subject><subject>Nutrient transport</subject><subject>Nutrients</subject><subject>Oceanography</subject><subject>Offshore</subject><subject>Phosphates</subject><subject>Radon isotopes</subject><subject>Seawater</subject><subject>Seawater mixing</subject><subject>Silicates</subject><subject>Steady state models</subject><subject>Turbulent diffusion</subject><subject>Vorticity</subject><subject>Water mixing</subject><issn>0253-505X</issn><issn>1869-1099</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp9kUFr3DAQhUVpoNskP6A3QQ-91O1IsmT72C7JNhAohA3kJsb2aNfLRt5KMsn--2hxIKeGOQw8vjcP5jH2RcAPAVD9jELlKUCqQkqlCvWBLURtmkJA03xkC5BaFRr0wyf2OcYdgBZaVQu2WwfsBr_hcQoOO-KR8AkTBf44PJ909D33UwoD-cRTQB8PY0i8PXIp5Z3no-dpS9xncUvB827EmPjo-G8a2omvpr37zpfbweMFO3O4j3T5us_Z_fXVevmnuP27uln-ui06qetUVK5pSFIttTDUt0hl17c9SdNrarTD1khnOtHlpcrWZFpUjoyCqkWNCtU5-zbffULv0G_sbpyCz4l2e3xuLcn8JKgB6kx-nclDGP9NFNMbKhvRlFVlSvMuVddlBVAqyJSYqS6MMQZy9hCGRwxHK8CeKrJzRTan21NFVmWPnD0xs35D4e3y_00vqtaTCA</recordid><startdate>20230801</startdate><enddate>20230801</enddate><creator>Wang, Hao</creator><creator>Zhong, Qiangqiang</creator><creator>Zhang, Fule</creator><creator>Chen, Suiyuan</creator><creator>Bao, Hongyan</creator><creator>Lin, Jing</creator><creator>Huang, Dekun</creator><creator>Yu, Tao</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><general>Third Institute of Oceanography,Ministry of Natural Resources,Xiamen 361005,China</general><general>College of Marine Sciences,Shanghai Ocean University,Shanghai 201306,China</general><general>Observation and Research Station of Coastal Wetland Ecosystem in Beibu Gulf,Ministry of Natural Resources,Beihai 536015,China%Third Institute of Oceanography,Ministry of Natural Resources,Xiamen 361005,China</general><general>Observation and Research Station of Coastal Wetland Ecosystem in Beibu Gulf,Ministry of Natural Resources,Beihai 536015,China%State Key Laboratory of Marine Environmental Science,College of Ocean and Earth Sciences,Xiamen University,Xiamen 361102,China</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7ST</scope><scope>7TG</scope><scope>7TN</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><scope>SOI</scope><scope>8FD</scope><scope>8FE</scope><scope>8FH</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BBNVY</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>H95</scope><scope>H97</scope><scope>H98</scope><scope>H99</scope><scope>HCIFZ</scope><scope>L.F</scope><scope>LK8</scope><scope>M7P</scope><scope>P64</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>2B.</scope><scope>4A8</scope><scope>92I</scope><scope>93N</scope><scope>PSX</scope><scope>TCJ</scope></search><sort><creationdate>20230801</creationdate><title>Tracing surface seawater mixing and nutrient transport by 222Rn on the northern coast of Beibu Gulf, China</title><author>Wang, Hao ; 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Based on the one-dimensional, steady-state model, the vorticity diffusion coefficient of 222 Rn in the horizontal direction was calculated as (0.42–2.13) × 10 8 m 2 /d, and the offshore fluxes of 222 Rn under the influence of water mixing were calculated as 2.00 × 10 12 Bq/d. Correspondingly, the horizontal transport fluxes of silicate, phosphate, nitrite and nitrate were 6.28 × 10 −3 mol/(m 2 ·d), 0.10 × 10 −3 mol/(m 2 ·d), 0.20 × 10 −3 mol/(m 2 ·d) and 4.15 × 10 −3 mol/(m 2 ·d), respectively. These results indicate that the study of eddy current diffusion in offshore marine water facilitates a deeper understanding of the water mixing process and nutrient transport and migration.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s13131-023-2233-3</doi><tpages>12</tpages></addata></record>
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subjects Advection
Climatology
Coastal zone
Coastal zones
Diffusion coefficient
Direction
Distribution
Earth and Environmental Science
Earth Sciences
Ecology
Eddy currents
Eddy diffusion
Engineering Fluid Dynamics
Environmental Chemistry
Fluxes
Horizontal orientation
Marine & Freshwater Sciences
Mixing
Nutrient transport
Nutrients
Oceanography
Offshore
Phosphates
Radon isotopes
Seawater
Seawater mixing
Silicates
Steady state models
Turbulent diffusion
Vorticity
Water mixing
title Tracing surface seawater mixing and nutrient transport by 222Rn on the northern coast of Beibu Gulf, China
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