Soil aluminum distribution in the near-stream zone at the Bear Brook watershed in Maine
Near-stream and upslope soil chemical properties were analyzed to infer linkages between soil and surface water chemistry atthe Bear Brook Watershed in Maine [BBWM]. Organic and mineral soil samples were collected along six 20 m transects perpendicular to the stream and one 200 m transect parallel t...
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| Veröffentlicht in: | Water, air, and soil pollution air, and soil pollution, 2002-02, Vol.134 (1-4), p.189-204 |
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| creator | PELLERIN, B. A FERNANDEZ, I. J NORTON, S. A KAHL, J. S |
| description | Near-stream and upslope soil chemical properties were analyzed to infer linkages between soil and surface water chemistry atthe Bear Brook Watershed in Maine [BBWM]. Organic and mineral soil samples were collected along six 20 m transects perpendicular to the stream and one 200 m transect parallel tothe stream. O horizon soils immediately adjacent to the streamhad a significantly higher pH (4.20) and lower soil organic matter percentage (54%) than upslope O horizons (3.84 and 76%,respectively). Additionally, near-stream O horizon soils hadsignificantly higher concentrations of water-soluble Al (2.7 ),exchangeable Al (2.3 ), and organically-bound Al (3.9 ) andsignificantly lower concentrations of exchangeable Ca (0.4 ) than O horizons upslope. These results suggest that Al can accumulate in non-hydric near-stream zone soils at this site. Mobilization of labile Al from near-stream zone soils duringhydrologic events could play a key role in explaining controls on Al in stream water at BBWM. |
| doi_str_mv | 10.1023/A:1014115717784 |
| format | Article |
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A ; FERNANDEZ, I. J ; NORTON, S. A ; KAHL, J. S</creator><creatorcontrib>PELLERIN, B. A ; FERNANDEZ, I. J ; NORTON, S. A ; KAHL, J. S</creatorcontrib><description>Near-stream and upslope soil chemical properties were analyzed to infer linkages between soil and surface water chemistry atthe Bear Brook Watershed in Maine [BBWM]. Organic and mineral soil samples were collected along six 20 m transects perpendicular to the stream and one 200 m transect parallel tothe stream. O horizon soils immediately adjacent to the streamhad a significantly higher pH (4.20) and lower soil organic matter percentage (54%) than upslope O horizons (3.84 and 76%,respectively). Additionally, near-stream O horizon soils hadsignificantly higher concentrations of water-soluble Al (2.7 ),exchangeable Al (2.3 ), and organically-bound Al (3.9 ) andsignificantly lower concentrations of exchangeable Ca (0.4 ) than O horizons upslope. These results suggest that Al can accumulate in non-hydric near-stream zone soils at this site. Mobilization of labile Al from near-stream zone soils duringhydrologic events could play a key role in explaining controls on Al in stream water at BBWM.</description><identifier>ISSN: 0049-6979</identifier><identifier>EISSN: 1573-2932</identifier><identifier>DOI: 10.1023/A:1014115717784</identifier><identifier>CODEN: WAPLAC</identifier><language>eng</language><publisher>Dordrecht: Springer</publisher><subject>Aluminum ; Applied sciences ; Bears ; Chemical properties ; Continental surface waters ; Earth sciences ; Earth, ocean, space ; Engineering and environment geology. Geothermics ; Environmental monitoring ; Exact sciences and technology ; Exchange ; Freshwater ; Horizon ; Natural water pollution ; Organic matter ; Organic soils ; Pollution ; Pollution sources. Measurement results ; Pollution, environment geology ; Soil (material) ; Soil and sediments pollution ; Soil horizons ; Soil organic matter ; Soil pollution ; Soil properties ; Soils ; Streams ; Surface water ; USA, Maine ; Water chemistry ; Water treatment and pollution ; Watersheds</subject><ispartof>Water, air, and soil pollution, 2002-02, Vol.134 (1-4), p.189-204</ispartof><rights>2002 INIST-CNRS</rights><rights>Kluwer Academic Publishers 2002</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a406t-361213da0b9590dd347505b5d6763437b7c0ba80584976e7a6745fd434acb92d3</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27901,27902</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=13512492$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>PELLERIN, B. A</creatorcontrib><creatorcontrib>FERNANDEZ, I. J</creatorcontrib><creatorcontrib>NORTON, S. A</creatorcontrib><creatorcontrib>KAHL, J. S</creatorcontrib><title>Soil aluminum distribution in the near-stream zone at the Bear Brook watershed in Maine</title><title>Water, air, and soil pollution</title><description>Near-stream and upslope soil chemical properties were analyzed to infer linkages between soil and surface water chemistry atthe Bear Brook Watershed in Maine [BBWM]. Organic and mineral soil samples were collected along six 20 m transects perpendicular to the stream and one 200 m transect parallel tothe stream. O horizon soils immediately adjacent to the streamhad a significantly higher pH (4.20) and lower soil organic matter percentage (54%) than upslope O horizons (3.84 and 76%,respectively). Additionally, near-stream O horizon soils hadsignificantly higher concentrations of water-soluble Al (2.7 ),exchangeable Al (2.3 ), and organically-bound Al (3.9 ) andsignificantly lower concentrations of exchangeable Ca (0.4 ) than O horizons upslope. These results suggest that Al can accumulate in non-hydric near-stream zone soils at this site. Mobilization of labile Al from near-stream zone soils duringhydrologic events could play a key role in explaining controls on Al in stream water at BBWM.</description><subject>Aluminum</subject><subject>Applied sciences</subject><subject>Bears</subject><subject>Chemical properties</subject><subject>Continental surface waters</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Engineering and environment geology. 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Measurement results</subject><subject>Pollution, environment geology</subject><subject>Soil (material)</subject><subject>Soil and sediments pollution</subject><subject>Soil horizons</subject><subject>Soil organic matter</subject><subject>Soil pollution</subject><subject>Soil properties</subject><subject>Soils</subject><subject>Streams</subject><subject>Surface water</subject><subject>USA, Maine</subject><subject>Water chemistry</subject><subject>Water treatment and pollution</subject><subject>Watersheds</subject><issn>0049-6979</issn><issn>1573-2932</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2002</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNqF0ElLxjAQBuAgCn4uZ69BcLlUM1kbbypuoHhQ8VimbT6MtqkmLaK_3ricPOhcMrw8MzAhZAPYHjAu9g8PgIEEUAaMKeUCmeVWFNwKvkhmjElbaGvsMllJ6ZHlsqWZkfubwXcUu6n3Yepp69MYfT2NfgjUBzo-OBocxiLHDnv6PgRHcfzKj3JOj-IwPNFXHF1MD679nLlCH9waWZpjl9z6z7tK7k5Pbo_Pi8vrs4vjw8sCJdNjITRwEC2y2irL2lZIo5iqVauNFlKY2jSsxpKpUlqjnUFtpJq3UkhsastbsUp2vvc-x-Flcmmsep8a13UY3DClymjOtZXMZrn7pwRTarCMlSbT7b-pBgEi179Qambha-PmL_g4TDHkn6nywUIrJSGjrR-EqcFuHjE0PlXP0fcY3yoQCri0XHwAxACUdw</recordid><startdate>20020201</startdate><enddate>20020201</enddate><creator>PELLERIN, B. 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A</au><au>FERNANDEZ, I. J</au><au>NORTON, S. A</au><au>KAHL, J. S</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Soil aluminum distribution in the near-stream zone at the Bear Brook watershed in Maine</atitle><jtitle>Water, air, and soil pollution</jtitle><date>2002-02-01</date><risdate>2002</risdate><volume>134</volume><issue>1-4</issue><spage>189</spage><epage>204</epage><pages>189-204</pages><issn>0049-6979</issn><eissn>1573-2932</eissn><coden>WAPLAC</coden><abstract>Near-stream and upslope soil chemical properties were analyzed to infer linkages between soil and surface water chemistry atthe Bear Brook Watershed in Maine [BBWM]. Organic and mineral soil samples were collected along six 20 m transects perpendicular to the stream and one 200 m transect parallel tothe stream. O horizon soils immediately adjacent to the streamhad a significantly higher pH (4.20) and lower soil organic matter percentage (54%) than upslope O horizons (3.84 and 76%,respectively). Additionally, near-stream O horizon soils hadsignificantly higher concentrations of water-soluble Al (2.7 ),exchangeable Al (2.3 ), and organically-bound Al (3.9 ) andsignificantly lower concentrations of exchangeable Ca (0.4 ) than O horizons upslope. These results suggest that Al can accumulate in non-hydric near-stream zone soils at this site. Mobilization of labile Al from near-stream zone soils duringhydrologic events could play a key role in explaining controls on Al in stream water at BBWM.</abstract><cop>Dordrecht</cop><pub>Springer</pub><doi>10.1023/A:1014115717784</doi><tpages>16</tpages></addata></record> |
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| ispartof | Water, air, and soil pollution, 2002-02, Vol.134 (1-4), p.189-204 |
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| subjects | Aluminum Applied sciences Bears Chemical properties Continental surface waters Earth sciences Earth, ocean, space Engineering and environment geology. Geothermics Environmental monitoring Exact sciences and technology Exchange Freshwater Horizon Natural water pollution Organic matter Organic soils Pollution Pollution sources. Measurement results Pollution, environment geology Soil (material) Soil and sediments pollution Soil horizons Soil organic matter Soil pollution Soil properties Soils Streams Surface water USA, Maine Water chemistry Water treatment and pollution Watersheds |
| title | Soil aluminum distribution in the near-stream zone at the Bear Brook watershed in Maine |
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