佐潟湖水中ヒ素濃度の季節変動
Sakata lagoon, a sand-dammed dune lake fed by only spring water and precipitation, is located in Niigata City. The inflow water from the upper lagoon, Kami-sakata, and the outflow water to the general river, were collected biweekly 152 times over a period ranging from February 2011 to January 2017,...
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Veröffentlicht in: | Bunseki kagaku 2018/09/05, Vol.67(9), pp.557-564 |
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description | Sakata lagoon, a sand-dammed dune lake fed by only spring water and precipitation, is located in Niigata City. The inflow water from the upper lagoon, Kami-sakata, and the outflow water to the general river, were collected biweekly 152 times over a period ranging from February 2011 to January 2017, respectively. The total arsenic (T-As) and other parameters (temperature, pH, ORP, main ionic components including HCO3−, iron, and manganese) were measured. Based on the temporal variations, seasonal comparisons and factor analysis, the following conclusions were obtained: 1) The concentration of T-As increased in the warm season, and sometimes exceeded the environmental standard value of 10 μg L−1. Approximately, 80 % of the T-As is present in the soluble form. 2) The ORP of outflow water decreased during the warm seasons to approximately 86 % of that during the cold seasons. Further, during warm seasons, the concentrations of NO3− and SO42− significantly decreased, and the concentrations of HCO3− in both the inflow and outflow water remarkably increase during warm season. 3) The increase in the concentration of T-As during the warm season is considered to be caused by the reduced adsorption affinity of As onto the organic matter and/or Fe(III) hydroxide in the lake sediments. Biological activities in the sediments may induce the decomposition of organic matter and a decreased ORP; the increased concentration of HCO3− and pH occurred mainly in outflow water, which affords the following decreased adsorption affinity of As. |
doi_str_mv | 10.2116/bunsekikagaku.67.557 |
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The inflow water from the upper lagoon, Kami-sakata, and the outflow water to the general river, were collected biweekly 152 times over a period ranging from February 2011 to January 2017, respectively. The total arsenic (T-As) and other parameters (temperature, pH, ORP, main ionic components including HCO3−, iron, and manganese) were measured. Based on the temporal variations, seasonal comparisons and factor analysis, the following conclusions were obtained: 1) The concentration of T-As increased in the warm season, and sometimes exceeded the environmental standard value of 10 μg L−1. Approximately, 80 % of the T-As is present in the soluble form. 2) The ORP of outflow water decreased during the warm seasons to approximately 86 % of that during the cold seasons. Further, during warm seasons, the concentrations of NO3− and SO42− significantly decreased, and the concentrations of HCO3− in both the inflow and outflow water remarkably increase during warm season. 3) The increase in the concentration of T-As during the warm season is considered to be caused by the reduced adsorption affinity of As onto the organic matter and/or Fe(III) hydroxide in the lake sediments. Biological activities in the sediments may induce the decomposition of organic matter and a decreased ORP; the increased concentration of HCO3− and pH occurred mainly in outflow water, which affords the following decreased adsorption affinity of As.</description><identifier>ISSN: 0525-1931</identifier><identifier>DOI: 10.2116/bunsekikagaku.67.557</identifier><language>jpn</language><publisher>Tokyo: 公益社団法人 日本分析化学会</publisher><subject>Adsorption ; Affinity ; Annual variations ; Arsenic ; Factor analysis ; Inflow ; Iron ; Lagoons ; Manganese ; Organic matter ; Outflow ; pH ; Seasons ; Sediments ; Spring water</subject><ispartof>分析化学, 2018/09/05, Vol.67(9), pp.557-564</ispartof><rights>2018 The Japan Society for Analytical Chemistry</rights><rights>Copyright Japan Science and Technology Agency 2018</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,1877,27901,27902</link.rule.ids></links><search><creatorcontrib>福崎, 紀夫</creatorcontrib><title>佐潟湖水中ヒ素濃度の季節変動</title><title>Bunseki kagaku</title><addtitle>分析化学</addtitle><description>Sakata lagoon, a sand-dammed dune lake fed by only spring water and precipitation, is located in Niigata City. The inflow water from the upper lagoon, Kami-sakata, and the outflow water to the general river, were collected biweekly 152 times over a period ranging from February 2011 to January 2017, respectively. The total arsenic (T-As) and other parameters (temperature, pH, ORP, main ionic components including HCO3−, iron, and manganese) were measured. Based on the temporal variations, seasonal comparisons and factor analysis, the following conclusions were obtained: 1) The concentration of T-As increased in the warm season, and sometimes exceeded the environmental standard value of 10 μg L−1. Approximately, 80 % of the T-As is present in the soluble form. 2) The ORP of outflow water decreased during the warm seasons to approximately 86 % of that during the cold seasons. Further, during warm seasons, the concentrations of NO3− and SO42− significantly decreased, and the concentrations of HCO3− in both the inflow and outflow water remarkably increase during warm season. 3) The increase in the concentration of T-As during the warm season is considered to be caused by the reduced adsorption affinity of As onto the organic matter and/or Fe(III) hydroxide in the lake sediments. Biological activities in the sediments may induce the decomposition of organic matter and a decreased ORP; the increased concentration of HCO3− and pH occurred mainly in outflow water, which affords the following decreased adsorption affinity of As.</description><subject>Adsorption</subject><subject>Affinity</subject><subject>Annual variations</subject><subject>Arsenic</subject><subject>Factor analysis</subject><subject>Inflow</subject><subject>Iron</subject><subject>Lagoons</subject><subject>Manganese</subject><subject>Organic matter</subject><subject>Outflow</subject><subject>pH</subject><subject>Seasons</subject><subject>Sediments</subject><subject>Spring water</subject><issn>0525-1931</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2018</creationdate><recordtype>article</recordtype><recordid>eNpVkDFLw0AYhm9QsNT-Azc3IfW7u9zlMkrRKhRcdD6-pJeapLY1aQY3pZO4FEFXBcWt6tBBheKPaZP-DSsVweV9l4f3hYeQDQpVRqnc9rJOauIwxhbGWVU6VSGcFVICwYRFXU7XSCVNQw-AKcaA2SWyNZsMi8l98XFXvI1n76Pp4GY-fii-Bvnn8_TyJR89zl8v8qer_Pp2nawG2E5N5bfL5Hhv96i2bzUO6we1nYYVMSqURUGAj4GnAsd1HckdNJQLkAKNZ0BRu8moUsBR2WBoE5SxIZAuCJ_5DH3Oy2RzudtLumeZSfs66mZJZ3GpGWOupJyDWlD1JRWlfWwZ3UvCU0zONSb90G8b_U-Flo52f2Lh44_wTzDREfJvZ0ttcA</recordid><startdate>20180905</startdate><enddate>20180905</enddate><creator>福崎, 紀夫</creator><general>公益社団法人 日本分析化学会</general><general>Japan Science and Technology Agency</general><scope>7U5</scope><scope>8FD</scope><scope>L7M</scope></search><sort><creationdate>20180905</creationdate><title>佐潟湖水中ヒ素濃度の季節変動</title><author>福崎, 紀夫</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-j2158-1050cafb8f7997637ae135065aebe0814d218803a840e1d08e40f6905c2c2ac33</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>jpn</language><creationdate>2018</creationdate><topic>Adsorption</topic><topic>Affinity</topic><topic>Annual variations</topic><topic>Arsenic</topic><topic>Factor analysis</topic><topic>Inflow</topic><topic>Iron</topic><topic>Lagoons</topic><topic>Manganese</topic><topic>Organic matter</topic><topic>Outflow</topic><topic>pH</topic><topic>Seasons</topic><topic>Sediments</topic><topic>Spring water</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>福崎, 紀夫</creatorcontrib><collection>Solid State and Superconductivity Abstracts</collection><collection>Technology Research Database</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Bunseki kagaku</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>福崎, 紀夫</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>佐潟湖水中ヒ素濃度の季節変動</atitle><jtitle>Bunseki kagaku</jtitle><addtitle>分析化学</addtitle><date>2018-09-05</date><risdate>2018</risdate><volume>67</volume><issue>9</issue><spage>557</spage><epage>564</epage><pages>557-564</pages><issn>0525-1931</issn><abstract>Sakata lagoon, a sand-dammed dune lake fed by only spring water and precipitation, is located in Niigata City. The inflow water from the upper lagoon, Kami-sakata, and the outflow water to the general river, were collected biweekly 152 times over a period ranging from February 2011 to January 2017, respectively. The total arsenic (T-As) and other parameters (temperature, pH, ORP, main ionic components including HCO3−, iron, and manganese) were measured. Based on the temporal variations, seasonal comparisons and factor analysis, the following conclusions were obtained: 1) The concentration of T-As increased in the warm season, and sometimes exceeded the environmental standard value of 10 μg L−1. Approximately, 80 % of the T-As is present in the soluble form. 2) The ORP of outflow water decreased during the warm seasons to approximately 86 % of that during the cold seasons. Further, during warm seasons, the concentrations of NO3− and SO42− significantly decreased, and the concentrations of HCO3− in both the inflow and outflow water remarkably increase during warm season. 3) The increase in the concentration of T-As during the warm season is considered to be caused by the reduced adsorption affinity of As onto the organic matter and/or Fe(III) hydroxide in the lake sediments. Biological activities in the sediments may induce the decomposition of organic matter and a decreased ORP; the increased concentration of HCO3− and pH occurred mainly in outflow water, which affords the following decreased adsorption affinity of As.</abstract><cop>Tokyo</cop><pub>公益社団法人 日本分析化学会</pub><doi>10.2116/bunsekikagaku.67.557</doi><tpages>8</tpages><oa>free_for_read</oa></addata></record> |
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source | J-STAGE (Japan Science & Technology Information Aggregator, Electronic) Freely Available Titles - Japanese; Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals; Free Full-Text Journals in Chemistry |
subjects | Adsorption Affinity Annual variations Arsenic Factor analysis Inflow Iron Lagoons Manganese Organic matter Outflow pH Seasons Sediments Spring water |
title | 佐潟湖水中ヒ素濃度の季節変動 |
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