Radioactivity of the Columbia River Effluent
Chromium-51 and zinc-65 were detected as far as 115 and 15 kilometers, respectively, from the mouth of the Columbia River; zinc-65 also was found at a few isolated stations. Zirconium-95 and niobium-95 from atmospheric fallout occurred in the river effluent but they were most abundant in surface wat...
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| Veröffentlicht in: | Science (American Association for the Advancement of Science) 1965-09, Vol.149 (3688), p.1088-1090 |
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| container_issue | 3688 |
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| container_title | Science (American Association for the Advancement of Science) |
| container_volume | 149 |
| creator | Gross, M. Grant Barnes, Clifford A. Riel, Gordon K. |
| description | Chromium-51 and zinc-65 were detected as far as 115 and 15 kilometers, respectively, from the mouth of the Columbia River; zinc-65 also was found at a few isolated stations. Zirconium-95 and niobium-95 from atmospheric fallout occurred in the river effluent but they were most abundant in surface waters further offshore. Distribution of the radionuclides is controlled largely by surface currents and by upwelling of sea water near the coast. |
| doi_str_mv | 10.1126/science.149.3688.1088 |
| format | Article |
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Grant ; Barnes, Clifford A. ; Riel, Gordon K.</creator><creatorcontrib>Gross, M. Grant ; Barnes, Clifford A. ; Riel, Gordon K. ; Univ. of Washington, Seattle</creatorcontrib><description>Chromium-51 and zinc-65 were detected as far as 115 and 15 kilometers, respectively, from the mouth of the Columbia River; zinc-65 also was found at a few isolated stations. Zirconium-95 and niobium-95 from atmospheric fallout occurred in the river effluent but they were most abundant in surface waters further offshore. 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Grant</creatorcontrib><creatorcontrib>Barnes, Clifford A.</creatorcontrib><creatorcontrib>Riel, Gordon K.</creatorcontrib><creatorcontrib>Univ. of Washington, Seattle</creatorcontrib><title>Radioactivity of the Columbia River Effluent</title><title>Science (American Association for the Advancement of Science)</title><addtitle>Science</addtitle><description>Chromium-51 and zinc-65 were detected as far as 115 and 15 kilometers, respectively, from the mouth of the Columbia River; zinc-65 also was found at a few isolated stations. Zirconium-95 and niobium-95 from atmospheric fallout occurred in the river effluent but they were most abundant in surface waters further offshore. Distribution of the radionuclides is controlled largely by surface currents and by upwelling of sea water near the coast.</description><subject>Amino acids</subject><subject>CHROMIUM 51</subject><subject>Coasts</subject><subject>COLUMBIA RIVER</subject><subject>CONFIGURATION</subject><subject>CONTAMINATION</subject><subject>DIFFUSION</subject><subject>DISTRIBUTION</subject><subject>FALLOUT</subject><subject>FISSION PRODUCTS</subject><subject>HEALTH AND SAFETY</subject><subject>HYDROLOGY</subject><subject>MONITORING</subject><subject>NIOBIUM 95</subject><subject>PACIFIC OCEAN</subject><subject>Proteins</subject><subject>QUANTITY RATIO</subject><subject>RADIOACTIVITY</subject><subject>Radionuclides</subject><subject>REACTION KINETICS</subject><subject>River deltas</subject><subject>River water</subject><subject>Salinity</subject><subject>SEA</subject><subject>Sea water</subject><subject>Surface water</subject><subject>Upwelling water</subject><subject>USA</subject><subject>WATER</subject><subject>ZINC 65</subject><subject>ZIRCONIUM 95</subject><issn>0036-8075</issn><issn>1095-9203</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1965</creationdate><recordtype>article</recordtype><recordid>eNpNkF1LwzAUhoMobk7_gUrxxhtbk-azlzLmBwyEodchSxOW0TWzSQf792a0oFeHw_ucczgPAHcIFgiV7DloZ1ptCkSqAjMhCgSFOANTBCuaVyXE52AKIWa5gJxOwFUIWwhTVuFLMEGcYy5IOQVPK1U7r3R0BxePmbdZ3Jhs7pt-t3YqW7mD6bKFtU1v2ngNLqxqgrkZ6wx8vy6-5u_58vPtY_6yzBVBMOaEE66MEtoyXDLKNNVVSlQlLBWMWiUsqnDquKJcC0ggrmvISsIE01XN8Aw8DHt9iE6mT6PRG-3b1ugoCYOEliJBjwO07_xPb0KUOxe0aRrVGt8HyTFGjJecJJIOpO58CJ2xct-5neqOEkF5kilHmTLJlCeZ8iQzzd2PF_r1ztR_U6O9BNwOwDZE3_3LEUum8S8Ln3kE</recordid><startdate>19650903</startdate><enddate>19650903</enddate><creator>Gross, M. Grant</creator><creator>Barnes, Clifford A.</creator><creator>Riel, Gordon K.</creator><general>American Association for the Advancement of Science</general><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7X8</scope><scope>OTOTI</scope></search><sort><creationdate>19650903</creationdate><title>Radioactivity of the Columbia River Effluent</title><author>Gross, M. Grant ; Barnes, Clifford A. ; Riel, Gordon K.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a410t-4747aea8cf632656c5c9a41a98f5865fa8f19398f7a57c80403dd0624686c9d63</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1965</creationdate><topic>Amino acids</topic><topic>CHROMIUM 51</topic><topic>Coasts</topic><topic>COLUMBIA RIVER</topic><topic>CONFIGURATION</topic><topic>CONTAMINATION</topic><topic>DIFFUSION</topic><topic>DISTRIBUTION</topic><topic>FALLOUT</topic><topic>FISSION PRODUCTS</topic><topic>HEALTH AND SAFETY</topic><topic>HYDROLOGY</topic><topic>MONITORING</topic><topic>NIOBIUM 95</topic><topic>PACIFIC OCEAN</topic><topic>Proteins</topic><topic>QUANTITY RATIO</topic><topic>RADIOACTIVITY</topic><topic>Radionuclides</topic><topic>REACTION KINETICS</topic><topic>River deltas</topic><topic>River water</topic><topic>Salinity</topic><topic>SEA</topic><topic>Sea water</topic><topic>Surface water</topic><topic>Upwelling water</topic><topic>USA</topic><topic>WATER</topic><topic>ZINC 65</topic><topic>ZIRCONIUM 95</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Gross, M. Grant</creatorcontrib><creatorcontrib>Barnes, Clifford A.</creatorcontrib><creatorcontrib>Riel, Gordon K.</creatorcontrib><creatorcontrib>Univ. of Washington, Seattle</creatorcontrib><collection>PubMed</collection><collection>CrossRef</collection><collection>MEDLINE - Academic</collection><collection>OSTI.GOV</collection><jtitle>Science (American Association for the Advancement of Science)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Gross, M. Grant</au><au>Barnes, Clifford A.</au><au>Riel, Gordon K.</au><aucorp>Univ. of Washington, Seattle</aucorp><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Radioactivity of the Columbia River Effluent</atitle><jtitle>Science (American Association for the Advancement of Science)</jtitle><addtitle>Science</addtitle><date>1965-09-03</date><risdate>1965</risdate><volume>149</volume><issue>3688</issue><spage>1088</spage><epage>1090</epage><pages>1088-1090</pages><issn>0036-8075</issn><eissn>1095-9203</eissn><abstract>Chromium-51 and zinc-65 were detected as far as 115 and 15 kilometers, respectively, from the mouth of the Columbia River; zinc-65 also was found at a few isolated stations. Zirconium-95 and niobium-95 from atmospheric fallout occurred in the river effluent but they were most abundant in surface waters further offshore. Distribution of the radionuclides is controlled largely by surface currents and by upwelling of sea water near the coast.</abstract><cop>United States</cop><pub>American Association for the Advancement of Science</pub><pmid>17737842</pmid><doi>10.1126/science.149.3688.1088</doi><tpages>3</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0036-8075 |
| ispartof | Science (American Association for the Advancement of Science), 1965-09, Vol.149 (3688), p.1088-1090 |
| issn | 0036-8075 1095-9203 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_733167274 |
| source | Science Magazine; JSTOR Archive Collection A-Z Listing |
| subjects | Amino acids CHROMIUM 51 Coasts COLUMBIA RIVER CONFIGURATION CONTAMINATION DIFFUSION DISTRIBUTION FALLOUT FISSION PRODUCTS HEALTH AND SAFETY HYDROLOGY MONITORING NIOBIUM 95 PACIFIC OCEAN Proteins QUANTITY RATIO RADIOACTIVITY Radionuclides REACTION KINETICS River deltas River water Salinity SEA Sea water Surface water Upwelling water USA WATER ZINC 65 ZIRCONIUM 95 |
| title | Radioactivity of the Columbia River Effluent |
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