Loading…
Infiltration of atrazine and metabolites from a stream to an alluvial aquifer
The infiltration of atrazine, deethylatrazine, and deisopropylatrazine from Walnut Creek, a tributary stream, to the alluvial valley aquifer along the South Skunk River in central Iowa occurred where the stream transects the river's flood plain. A preliminary estimate indicated that the infiltr...
Saved in:
| Published in: | Journal of the American Water Resources Association 1997-02, Vol.33 (1), p.89-95 |
|---|---|
| Main Authors: | , , |
| Format: | Article |
| Language: | English |
| Subjects: | |
| Online Access: | Get full text |
| Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
| cited_by | |
|---|---|
| cites | |
| container_end_page | 95 |
| container_issue | 1 |
| container_start_page | 89 |
| container_title | Journal of the American Water Resources Association |
| container_volume | 33 |
| creator | Squillace, P.J. (US Geological Survey, Rapid City, SD.) Burkart, M.R Simpkins, W.W |
| description | The infiltration of atrazine, deethylatrazine, and deisopropylatrazine from Walnut Creek, a tributary stream, to the alluvial valley aquifer along the South Skunk River in central Iowa occurred where the stream transects the river's flood plain. A preliminary estimate indicated that the infiltration was significant and warrants further investigation. Infiltration was estimated by measuring the loss of stream discharge in Walnut Creek and the concentrations of atrazine and its metabolites deethylatrazine and deisopropylatrazine, in ground water 1 m beneath the streambed. Infiltration was estimated before application of agrichemicals to the fields during a dry period on April 7, 1994, and after application of agrichemicals during a period of small runoff on June 8, 1994. On April 7, the flux of atrazine, deethylatrazine, and deisopropylatrazine from Walnut Creek into the alluvial valley aquifer ranged from less than 10 to 60 (microgram/d)/m2, whereas on June 8 an increased flux ranged from 270 to 3060 (microgram(d)/m2. By way of comparison, the calculated fluxes of atrazine beneath Walnut Creek, for these two dates, were two to five orders of magnitude greater than an estimated flux of atrazine to ground water caused by leaching from a field on a per-unit area basis. Furthermore, the unit-area flux rates of water from Walnut Creek to the alluvial valley aquifer were about three orders of magnitude greater than estimated recharge to the alluvial aquifer from precipitation. The large flux of chemicals from Walnut Creek to the alluvial valley aquifer was due in part to the conductive streambed and rather fast ground water velocities; average vertical hydraulic conductivity through the streambed was calculated as 35 and 90 m/d for the two sampling dates, and estimated ground water velocities ranged from 1 to 5 m/d |
| doi_str_mv | 10.1111/j.1752-1688.1997.tb04085.x |
| format | article |
| fullrecord | <record><control><sourceid>proquest_pasca</sourceid><recordid>TN_cdi_istex_primary_ark_67375_WNG_N2W35J72_H</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>15972220</sourcerecordid><originalsourceid>FETCH-LOGICAL-f273t-455cbdbb049fad7e397f5bbe405f76069f592b404baceca046d7d8bd8308eb2e3</originalsourceid><addsrcrecordid>eNo9kEFLxDAUhIMouK7-BCGIeGtNk6ZpjyK6rqzrQUVv4aVNJGvaapIV9dcbWdl3mYH5GB6D0ElB8iLd-SovBKdZUdV1XjSNyKMiJal5_rWDJttoN3nSsKwU5cs-OghhRUjBi5pN0N18MNZFD9GOAx4NhuR_7KAxDB3udQQ1Oht1wMaPPQYcotfQ4zgmAINz608LDsPH2hrtD9GeARf00b9O0dP11ePlTba4n80vLxaZoYLFrOS8VZ1KrzYGOqFZIwxXSpeEG1GRqjG8oaokpYJWt0DKqhNdrbqakVorqtkUnW163_34sdYhyt6GVjsHgx7XQRa8EZRSksDTfxBCC854GFob5Lu3PfhvSQUhVVpmirINZkPUX9sY_JusBBNcPi9nckmfGb8VVN4k_njDGxglvPpU-fTwtz_hqbBmv7YheaI</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>15972220</pqid></control><display><type>article</type><title>Infiltration of atrazine and metabolites from a stream to an alluvial aquifer</title><source>Wiley-Blackwell Journals</source><creator>Squillace, P.J. (US Geological Survey, Rapid City, SD.) ; Burkart, M.R ; Simpkins, W.W</creator><creatorcontrib>Squillace, P.J. (US Geological Survey, Rapid City, SD.) ; Burkart, M.R ; Simpkins, W.W</creatorcontrib><description>The infiltration of atrazine, deethylatrazine, and deisopropylatrazine from Walnut Creek, a tributary stream, to the alluvial valley aquifer along the South Skunk River in central Iowa occurred where the stream transects the river's flood plain. A preliminary estimate indicated that the infiltration was significant and warrants further investigation. Infiltration was estimated by measuring the loss of stream discharge in Walnut Creek and the concentrations of atrazine and its metabolites deethylatrazine and deisopropylatrazine, in ground water 1 m beneath the streambed. Infiltration was estimated before application of agrichemicals to the fields during a dry period on April 7, 1994, and after application of agrichemicals during a period of small runoff on June 8, 1994. On April 7, the flux of atrazine, deethylatrazine, and deisopropylatrazine from Walnut Creek into the alluvial valley aquifer ranged from less than 10 to 60 (microgram/d)/m2, whereas on June 8 an increased flux ranged from 270 to 3060 (microgram(d)/m2. By way of comparison, the calculated fluxes of atrazine beneath Walnut Creek, for these two dates, were two to five orders of magnitude greater than an estimated flux of atrazine to ground water caused by leaching from a field on a per-unit area basis. Furthermore, the unit-area flux rates of water from Walnut Creek to the alluvial valley aquifer were about three orders of magnitude greater than estimated recharge to the alluvial aquifer from precipitation. The large flux of chemicals from Walnut Creek to the alluvial valley aquifer was due in part to the conductive streambed and rather fast ground water velocities; average vertical hydraulic conductivity through the streambed was calculated as 35 and 90 m/d for the two sampling dates, and estimated ground water velocities ranged from 1 to 5 m/d</description><identifier>ISSN: 1093-474X</identifier><identifier>ISSN: 0043-1370</identifier><identifier>EISSN: 1752-1688</identifier><identifier>DOI: 10.1111/j.1752-1688.1997.tb04085.x</identifier><identifier>CODEN: WARBAQ</identifier><language>eng</language><publisher>Oxford, UK: Blackwell Publishing Ltd</publisher><subject>AGUA SUPERFICIAL ; AGUAS SUBTERRANEAS ; alluvial aquifer ; ATRAZINA ; ATRAZINE ; CAPA FREATICA ; COURS D'EAU ; CURSOS DE AGUA ; DEBIT ; DEETHYLATRAZINE ; DEISOPROPATRAZINE ; deisopropylatrazine ; Earth sciences ; Earth, ocean, space ; EAU SOUTERRAINE ; EAU SUPERFICIELLE ; ESCORRENTIA ; Exact sciences and technology ; FLOOD PLAINS ; FLOW RATE ; Freshwater ; GASTO ; GROUNDWATER ; GROUNDWATER TABLE ; Hydrology. Hydrogeology ; INFILTRACION ; INFILTRATION ; INTERACTIONS ; IOWA ; LLANURA ALUVIAL ; METABOLITE ; METABOLITES ; METABOLITOS ; NAPPE SOUTERRAINE ; PLAINE D'INONDATION ; RIVERS ; RUISSELLEMENT ; RUNOFF ; stream aquifer interaction ; STREAM AQUIFER INTERACTIONS ; SURFACE WATER ; WALNUT CREEK ; Water resources</subject><ispartof>Journal of the American Water Resources Association, 1997-02, Vol.33 (1), p.89-95</ispartof><rights>1997 INIST-CNRS</rights><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>315,786,790,27957,27958</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=2700609$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Squillace, P.J. (US Geological Survey, Rapid City, SD.)</creatorcontrib><creatorcontrib>Burkart, M.R</creatorcontrib><creatorcontrib>Simpkins, W.W</creatorcontrib><title>Infiltration of atrazine and metabolites from a stream to an alluvial aquifer</title><title>Journal of the American Water Resources Association</title><description>The infiltration of atrazine, deethylatrazine, and deisopropylatrazine from Walnut Creek, a tributary stream, to the alluvial valley aquifer along the South Skunk River in central Iowa occurred where the stream transects the river's flood plain. A preliminary estimate indicated that the infiltration was significant and warrants further investigation. Infiltration was estimated by measuring the loss of stream discharge in Walnut Creek and the concentrations of atrazine and its metabolites deethylatrazine and deisopropylatrazine, in ground water 1 m beneath the streambed. Infiltration was estimated before application of agrichemicals to the fields during a dry period on April 7, 1994, and after application of agrichemicals during a period of small runoff on June 8, 1994. On April 7, the flux of atrazine, deethylatrazine, and deisopropylatrazine from Walnut Creek into the alluvial valley aquifer ranged from less than 10 to 60 (microgram/d)/m2, whereas on June 8 an increased flux ranged from 270 to 3060 (microgram(d)/m2. By way of comparison, the calculated fluxes of atrazine beneath Walnut Creek, for these two dates, were two to five orders of magnitude greater than an estimated flux of atrazine to ground water caused by leaching from a field on a per-unit area basis. Furthermore, the unit-area flux rates of water from Walnut Creek to the alluvial valley aquifer were about three orders of magnitude greater than estimated recharge to the alluvial aquifer from precipitation. The large flux of chemicals from Walnut Creek to the alluvial valley aquifer was due in part to the conductive streambed and rather fast ground water velocities; average vertical hydraulic conductivity through the streambed was calculated as 35 and 90 m/d for the two sampling dates, and estimated ground water velocities ranged from 1 to 5 m/d</description><subject>AGUA SUPERFICIAL</subject><subject>AGUAS SUBTERRANEAS</subject><subject>alluvial aquifer</subject><subject>ATRAZINA</subject><subject>ATRAZINE</subject><subject>CAPA FREATICA</subject><subject>COURS D'EAU</subject><subject>CURSOS DE AGUA</subject><subject>DEBIT</subject><subject>DEETHYLATRAZINE</subject><subject>DEISOPROPATRAZINE</subject><subject>deisopropylatrazine</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>EAU SOUTERRAINE</subject><subject>EAU SUPERFICIELLE</subject><subject>ESCORRENTIA</subject><subject>Exact sciences and technology</subject><subject>FLOOD PLAINS</subject><subject>FLOW RATE</subject><subject>Freshwater</subject><subject>GASTO</subject><subject>GROUNDWATER</subject><subject>GROUNDWATER TABLE</subject><subject>Hydrology. Hydrogeology</subject><subject>INFILTRACION</subject><subject>INFILTRATION</subject><subject>INTERACTIONS</subject><subject>IOWA</subject><subject>LLANURA ALUVIAL</subject><subject>METABOLITE</subject><subject>METABOLITES</subject><subject>METABOLITOS</subject><subject>NAPPE SOUTERRAINE</subject><subject>PLAINE D'INONDATION</subject><subject>RIVERS</subject><subject>RUISSELLEMENT</subject><subject>RUNOFF</subject><subject>stream aquifer interaction</subject><subject>STREAM AQUIFER INTERACTIONS</subject><subject>SURFACE WATER</subject><subject>WALNUT CREEK</subject><subject>Water resources</subject><issn>1093-474X</issn><issn>0043-1370</issn><issn>1752-1688</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1997</creationdate><recordtype>article</recordtype><recordid>eNo9kEFLxDAUhIMouK7-BCGIeGtNk6ZpjyK6rqzrQUVv4aVNJGvaapIV9dcbWdl3mYH5GB6D0ElB8iLd-SovBKdZUdV1XjSNyKMiJal5_rWDJttoN3nSsKwU5cs-OghhRUjBi5pN0N18MNZFD9GOAx4NhuR_7KAxDB3udQQ1Oht1wMaPPQYcotfQ4zgmAINz608LDsPH2hrtD9GeARf00b9O0dP11ePlTba4n80vLxaZoYLFrOS8VZ1KrzYGOqFZIwxXSpeEG1GRqjG8oaokpYJWt0DKqhNdrbqakVorqtkUnW163_34sdYhyt6GVjsHgx7XQRa8EZRSksDTfxBCC854GFob5Lu3PfhvSQUhVVpmirINZkPUX9sY_JusBBNcPi9nckmfGb8VVN4k_njDGxglvPpU-fTwtz_hqbBmv7YheaI</recordid><startdate>19970201</startdate><enddate>19970201</enddate><creator>Squillace, P.J. (US Geological Survey, Rapid City, SD.)</creator><creator>Burkart, M.R</creator><creator>Simpkins, W.W</creator><general>Blackwell Publishing Ltd</general><general>American Water Resources Association</general><scope>FBQ</scope><scope>BSCLL</scope><scope>IQODW</scope><scope>7TV</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H97</scope><scope>L.G</scope></search><sort><creationdate>19970201</creationdate><title>Infiltration of atrazine and metabolites from a stream to an alluvial aquifer</title><author>Squillace, P.J. (US Geological Survey, Rapid City, SD.) ; Burkart, M.R ; Simpkins, W.W</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-f273t-455cbdbb049fad7e397f5bbe405f76069f592b404baceca046d7d8bd8308eb2e3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1997</creationdate><topic>AGUA SUPERFICIAL</topic><topic>AGUAS SUBTERRANEAS</topic><topic>alluvial aquifer</topic><topic>ATRAZINA</topic><topic>ATRAZINE</topic><topic>CAPA FREATICA</topic><topic>COURS D'EAU</topic><topic>CURSOS DE AGUA</topic><topic>DEBIT</topic><topic>DEETHYLATRAZINE</topic><topic>DEISOPROPATRAZINE</topic><topic>deisopropylatrazine</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>EAU SOUTERRAINE</topic><topic>EAU SUPERFICIELLE</topic><topic>ESCORRENTIA</topic><topic>Exact sciences and technology</topic><topic>FLOOD PLAINS</topic><topic>FLOW RATE</topic><topic>Freshwater</topic><topic>GASTO</topic><topic>GROUNDWATER</topic><topic>GROUNDWATER TABLE</topic><topic>Hydrology. Hydrogeology</topic><topic>INFILTRACION</topic><topic>INFILTRATION</topic><topic>INTERACTIONS</topic><topic>IOWA</topic><topic>LLANURA ALUVIAL</topic><topic>METABOLITE</topic><topic>METABOLITES</topic><topic>METABOLITOS</topic><topic>NAPPE SOUTERRAINE</topic><topic>PLAINE D'INONDATION</topic><topic>RIVERS</topic><topic>RUISSELLEMENT</topic><topic>RUNOFF</topic><topic>stream aquifer interaction</topic><topic>STREAM AQUIFER INTERACTIONS</topic><topic>SURFACE WATER</topic><topic>WALNUT CREEK</topic><topic>Water resources</topic><toplevel>online_resources</toplevel><creatorcontrib>Squillace, P.J. (US Geological Survey, Rapid City, SD.)</creatorcontrib><creatorcontrib>Burkart, M.R</creatorcontrib><creatorcontrib>Simpkins, W.W</creatorcontrib><collection>AGRIS</collection><collection>Istex</collection><collection>Pascal-Francis</collection><collection>Pollution Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 3: Aquatic Pollution & Environmental Quality</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Journal of the American Water Resources Association</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Squillace, P.J. (US Geological Survey, Rapid City, SD.)</au><au>Burkart, M.R</au><au>Simpkins, W.W</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Infiltration of atrazine and metabolites from a stream to an alluvial aquifer</atitle><jtitle>Journal of the American Water Resources Association</jtitle><date>1997-02-01</date><risdate>1997</risdate><volume>33</volume><issue>1</issue><spage>89</spage><epage>95</epage><pages>89-95</pages><issn>1093-474X</issn><issn>0043-1370</issn><eissn>1752-1688</eissn><coden>WARBAQ</coden><notes>T01</notes><notes>1997050068</notes><notes>ArticleID:JAWR89</notes><notes>ark:/67375/WNG-N2W35J72-H</notes><notes>istex:E0700F994D3ABF9DB122434E951565C6755FC532</notes><notes>Paper No. 96039 of the Journal of the American Water Resources Association (formerly Water Resources Bulletin). Discussions are open until August 1, 1997.</notes><notes>ObjectType-Article-1</notes><notes>SourceType-Scholarly Journals-1</notes><notes>ObjectType-Feature-2</notes><notes>content type line 23</notes><abstract>The infiltration of atrazine, deethylatrazine, and deisopropylatrazine from Walnut Creek, a tributary stream, to the alluvial valley aquifer along the South Skunk River in central Iowa occurred where the stream transects the river's flood plain. A preliminary estimate indicated that the infiltration was significant and warrants further investigation. Infiltration was estimated by measuring the loss of stream discharge in Walnut Creek and the concentrations of atrazine and its metabolites deethylatrazine and deisopropylatrazine, in ground water 1 m beneath the streambed. Infiltration was estimated before application of agrichemicals to the fields during a dry period on April 7, 1994, and after application of agrichemicals during a period of small runoff on June 8, 1994. On April 7, the flux of atrazine, deethylatrazine, and deisopropylatrazine from Walnut Creek into the alluvial valley aquifer ranged from less than 10 to 60 (microgram/d)/m2, whereas on June 8 an increased flux ranged from 270 to 3060 (microgram(d)/m2. By way of comparison, the calculated fluxes of atrazine beneath Walnut Creek, for these two dates, were two to five orders of magnitude greater than an estimated flux of atrazine to ground water caused by leaching from a field on a per-unit area basis. Furthermore, the unit-area flux rates of water from Walnut Creek to the alluvial valley aquifer were about three orders of magnitude greater than estimated recharge to the alluvial aquifer from precipitation. The large flux of chemicals from Walnut Creek to the alluvial valley aquifer was due in part to the conductive streambed and rather fast ground water velocities; average vertical hydraulic conductivity through the streambed was calculated as 35 and 90 m/d for the two sampling dates, and estimated ground water velocities ranged from 1 to 5 m/d</abstract><cop>Oxford, UK</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1111/j.1752-1688.1997.tb04085.x</doi><tpages>7</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 1093-474X |
| ispartof | Journal of the American Water Resources Association, 1997-02, Vol.33 (1), p.89-95 |
| issn | 1093-474X 0043-1370 1752-1688 |
| language | eng |
| recordid | cdi_istex_primary_ark_67375_WNG_N2W35J72_H |
| source | Wiley-Blackwell Journals |
| subjects | AGUA SUPERFICIAL AGUAS SUBTERRANEAS alluvial aquifer ATRAZINA ATRAZINE CAPA FREATICA COURS D'EAU CURSOS DE AGUA DEBIT DEETHYLATRAZINE DEISOPROPATRAZINE deisopropylatrazine Earth sciences Earth, ocean, space EAU SOUTERRAINE EAU SUPERFICIELLE ESCORRENTIA Exact sciences and technology FLOOD PLAINS FLOW RATE Freshwater GASTO GROUNDWATER GROUNDWATER TABLE Hydrology. Hydrogeology INFILTRACION INFILTRATION INTERACTIONS IOWA LLANURA ALUVIAL METABOLITE METABOLITES METABOLITOS NAPPE SOUTERRAINE PLAINE D'INONDATION RIVERS RUISSELLEMENT RUNOFF stream aquifer interaction STREAM AQUIFER INTERACTIONS SURFACE WATER WALNUT CREEK Water resources |
| title | Infiltration of atrazine and metabolites from a stream to an alluvial aquifer |
| url | http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-09-21T20%3A13%3A10IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_pasca&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Infiltration%20of%20atrazine%20and%20metabolites%20from%20a%20stream%20to%20an%20alluvial%20aquifer&rft.jtitle=Journal%20of%20the%20American%20Water%20Resources%20Association&rft.au=Squillace,%20P.J.%20(US%20Geological%20Survey,%20Rapid%20City,%20SD.)&rft.date=1997-02-01&rft.volume=33&rft.issue=1&rft.spage=89&rft.epage=95&rft.pages=89-95&rft.issn=1093-474X&rft.eissn=1752-1688&rft.coden=WARBAQ&rft_id=info:doi/10.1111/j.1752-1688.1997.tb04085.x&rft_dat=%3Cproquest_pasca%3E15972220%3C/proquest_pasca%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-f273t-455cbdbb049fad7e397f5bbe405f76069f592b404baceca046d7d8bd8308eb2e3%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=15972220&rft_id=info:pmid/&rfr_iscdi=true |