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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creator | Wang, Hao 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. |
doi_str_mv | 10.1007/s13131-023-2233-3 |
format | Article |
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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.</description><identifier>ISSN: 0253-505X</identifier><identifier>EISSN: 1869-1099</identifier><identifier>DOI: 10.1007/s13131-023-2233-3</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>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</subject><ispartof>Acta oceanologica Sinica, 2023-08, Vol.42 (8), p.87-98</ispartof><rights>Chinese Society for Oceanography and Springer-Verlag GmbH Germany, part of Springer Nature 2023</rights><rights>Chinese Society for Oceanography and Springer-Verlag GmbH Germany, part of Springer Nature 2023.</rights><rights>Copyright © Wanfang Data Co. Ltd. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c258t-7f99e2e82516edbae4cdbde26d5e95fab62f6c1c62f34b6f9917fe6307ba5a3a3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://www.wanfangdata.com.cn/images/PeriodicalImages/hyxb-e/hyxb-e.jpg</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s13131-023-2233-3$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/2919477646?pq-origsite=primo$$EHTML$$P50$$Gproquest$$H</linktohtml><link.rule.ids>314,776,780,21367,27901,27902,33721,41464,42533,43781,51294</link.rule.ids></links><search><creatorcontrib>Wang, Hao</creatorcontrib><creatorcontrib>Zhong, Qiangqiang</creatorcontrib><creatorcontrib>Zhang, Fule</creatorcontrib><creatorcontrib>Chen, Suiyuan</creatorcontrib><creatorcontrib>Bao, Hongyan</creatorcontrib><creatorcontrib>Lin, Jing</creatorcontrib><creatorcontrib>Huang, Dekun</creatorcontrib><creatorcontrib>Yu, Tao</creatorcontrib><title>Tracing surface seawater mixing and nutrient transport by 222Rn on the northern coast of Beibu Gulf, China</title><title>Acta oceanologica Sinica</title><addtitle>Acta Oceanol. Sin</addtitle><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.</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 & 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, 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mixing and nutrient transport by 222Rn on the northern coast of Beibu Gulf, China</title><author>Wang, Hao ; Zhong, Qiangqiang ; Zhang, Fule ; Chen, Suiyuan ; Bao, Hongyan ; Lin, Jing ; Huang, Dekun ; Yu, Tao</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c258t-7f99e2e82516edbae4cdbde26d5e95fab62f6c1c62f34b6f9917fe6307ba5a3a3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2023</creationdate><topic>Advection</topic><topic>Climatology</topic><topic>Coastal zone</topic><topic>Coastal zones</topic><topic>Diffusion coefficient</topic><topic>Direction</topic><topic>Distribution</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Ecology</topic><topic>Eddy currents</topic><topic>Eddy diffusion</topic><topic>Engineering Fluid Dynamics</topic><topic>Environmental Chemistry</topic><topic>Fluxes</topic><topic>Horizontal orientation</topic><topic>Marine & Freshwater Sciences</topic><topic>Mixing</topic><topic>Nutrient transport</topic><topic>Nutrients</topic><topic>Oceanography</topic><topic>Offshore</topic><topic>Phosphates</topic><topic>Radon isotopes</topic><topic>Seawater</topic><topic>Seawater mixing</topic><topic>Silicates</topic><topic>Steady state models</topic><topic>Turbulent diffusion</topic><topic>Vorticity</topic><topic>Water mixing</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Wang, Hao</creatorcontrib><creatorcontrib>Zhong, Qiangqiang</creatorcontrib><creatorcontrib>Zhang, Fule</creatorcontrib><creatorcontrib>Chen, Suiyuan</creatorcontrib><creatorcontrib>Bao, Hongyan</creatorcontrib><creatorcontrib>Lin, Jing</creatorcontrib><creatorcontrib>Huang, Dekun</creatorcontrib><creatorcontrib>Yu, Tao</creatorcontrib><collection>CrossRef</collection><collection>Environment Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic 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Tao</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Tracing surface seawater mixing and nutrient transport by 222Rn on the northern coast of Beibu Gulf, China</atitle><jtitle>Acta oceanologica Sinica</jtitle><stitle>Acta Oceanol. Sin</stitle><date>2023-08-01</date><risdate>2023</risdate><volume>42</volume><issue>8</issue><spage>87</spage><epage>98</epage><pages>87-98</pages><issn>0253-505X</issn><eissn>1869-1099</eissn><abstract>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.</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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