北京通州区第四系地下水化学特征及其成因分析
【目的】揭示通州区地下水化学特征及其影响因素。【方法】利用2018年在通州区采集的45件300 m深度的地下水水质检测数据，通过Piper三线图、Gibbs图、因子分析和聚类分析等多元统计分析方法，分析了第四系地下水水化学特征及其影响因素。【结果】通州区第四系地下水浅层水化学类型以HCO3-Ca.Mg型为主，深层地下水化学类型以HCO3-Na型为主。通过因子分析共提取了4个公因子，其累计方差占总方差的85.45%。因子1代表盐度因子，反映了碳酸盐、硅酸盐矿物风化过程；因子2代表铁锰污染因子，反映了富含铁锰元素的矿物的风化作用；因子3代表农业污染因子，反映了农业活动对地下水的影响；因子4代表氟化...
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| Veröffentlicht in: | Guanʻgai paishui xuebao 2022-01, Vol.41 (3), p.92-104 |
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| description | 【目的】揭示通州区地下水化学特征及其影响因素。【方法】利用2018年在通州区采集的45件300 m深度的地下水水质检测数据，通过Piper三线图、Gibbs图、因子分析和聚类分析等多元统计分析方法，分析了第四系地下水水化学特征及其影响因素。【结果】通州区第四系地下水浅层水化学类型以HCO3-Ca.Mg型为主，深层地下水化学类型以HCO3-Na型为主。通过因子分析共提取了4个公因子，其累计方差占总方差的85.45%。因子1代表盐度因子，反映了碳酸盐、硅酸盐矿物风化过程；因子2代表铁锰污染因子，反映了富含铁锰元素的矿物的风化作用；因子3代表农业污染因子，反映了农业活动对地下水的影响；因子4代表氟化物污染因子，反映了含氟矿物的风化及阳离子交换反应。【结论】农业活动主要影响通州北部宋庄、永顺一带；而碳酸盐、硅酸盐矿物风化作用，含铁锰元素矿物风化作用，含氟元素矿物风化作用及阳离子交换作用在通州全区普遍存在。 |
| doi_str_mv | 10.13522/j.cnki.ggps.2021190 |
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This work is published under https://creativecommons.org/licenses/by-nc-nd/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><rights>Copyright © Wanfang Data Co. Ltd. All Rights Reserved.</rights><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://www.wanfangdata.com.cn/images/PeriodicalImages/ggps/ggps.jpg</thumbnail><link.rule.ids>314,780,784,864,4024,27923,27924,27925</link.rule.ids></links><search><creatorcontrib>WANG, Xiaosong</creatorcontrib><creatorcontrib>LI, Baoxue</creatorcontrib><creatorcontrib>Yang, LI</creatorcontrib><title>北京通州区第四系地下水化学特征及其成因分析</title><title>Guanʻgai paishui xuebao</title><description>【目的】揭示通州区地下水化学特征及其影响因素。【方法】利用2018年在通州区采集的45件300 m深度的地下水水质检测数据，通过Piper三线图、Gibbs图、因子分析和聚类分析等多元统计分析方法，分析了第四系地下水水化学特征及其影响因素。【结果】通州区第四系地下水浅层水化学类型以HCO3-Ca.Mg型为主，深层地下水化学类型以HCO3-Na型为主。通过因子分析共提取了4个公因子，其累计方差占总方差的85.45%。因子1代表盐度因子，反映了碳酸盐、硅酸盐矿物风化过程；因子2代表铁锰污染因子，反映了富含铁锰元素的矿物的风化作用；因子3代表农业污染因子，反映了农业活动对地下水的影响；因子4代表氟化物污染因子，反映了含氟矿物的风化及阳离子交换反应。【结论】农业活动主要影响通州北部宋庄、永顺一带；而碳酸盐、硅酸盐矿物风化作用，含铁锰元素矿物风化作用，含氟元素矿物风化作用及阳离子交换作用在通州全区普遍存在。</description><subject>Agricultural pollution</subject><subject>Agricultural practices</subject><subject>Agricultural production</subject><subject>Agricultural wastes</subject><subject>Agronomy</subject><subject>Aquifers</subject><subject>Boreholes</subject><subject>Calcium</subject><subject>Cation exchange</subject><subject>Cation exchanging</subject><subject>Cluster analysis</subject><subject>Deep water</subject><subject>Discriminant analysis</subject><subject>Factor analysis</subject><subject>Fluorides</subject><subject>Fluorine</subject><subject>Groundwater</subject><subject>Iron</subject><subject>Manganese</subject><subject>Minerals</subject><subject>Water analysis</subject><subject>Water depth</subject><subject>Water sampling</subject><subject>Water supply</subject><subject>Weathering</subject><issn>1672-3317</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><sourceid>AFKRA</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><recordid>eNpFj8tKw0AYhWehYKl9A3fiMvGff3KZrESKNyi46b5MMplglbQ2Fre6UKoN2JWCleLKVYSC4qWCT9Np8S1MqSAcOJuPcyFkhYJJmY24XjeD-PDAjKJmYiIgpR4skAJ1XDQYo-4SKSVJHQDQBtf2WIFs6PRuPMp-zu71-0Cno2mW6X5_-vKlH4bjj-5k-KrTW_38NL361N_n-uZaX7xNOj3df9Sdy8mgt0wWlThKwtKfF0l1e6ta3jUq-zt75c2K0bS5ZVAuhPKtmQTYruS-CpUjGZO2h-g6jmIKqI_IXS4Dy7GkpEidIJ-PQoqAFcnaPPZUxErEUa3eaLfivLA2u5o_RWBArZxbnXPNVuO4HSYn_yADj-ddwDn7BUWPbd4</recordid><startdate>20220101</startdate><enddate>20220101</enddate><creator>WANG, Xiaosong</creator><creator>LI, Baoxue</creator><creator>Yang, LI</creator><general>Chinese Academy of Agricultural Sciences (CAAS) Farmland Irrigation Research Institute Editorial Office of Journal of Irrigation and Drainage</general><general>北京市地质工程勘察院,北京 100048</general><scope>3V.</scope><scope>7X2</scope><scope>8FE</scope><scope>8FH</scope><scope>8FK</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>HCIFZ</scope><scope>M0K</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>2B.</scope><scope>4A8</scope><scope>92I</scope><scope>93N</scope><scope>PSX</scope><scope>TCJ</scope></search><sort><creationdate>20220101</creationdate><title>北京通州区第四系地下水化学特征及其成因分析</title><author>WANG, Xiaosong ; LI, Baoxue ; Yang, LI</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-p584-18aafb4fb4fa057d8bfef6d33d5922766f3f01b22878dc464dd1216c1902adac3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>chi ; eng</language><creationdate>2022</creationdate><topic>Agricultural pollution</topic><topic>Agricultural practices</topic><topic>Agricultural production</topic><topic>Agricultural wastes</topic><topic>Agronomy</topic><topic>Aquifers</topic><topic>Boreholes</topic><topic>Calcium</topic><topic>Cation exchange</topic><topic>Cation exchanging</topic><topic>Cluster analysis</topic><topic>Deep water</topic><topic>Discriminant analysis</topic><topic>Factor analysis</topic><topic>Fluorides</topic><topic>Fluorine</topic><topic>Groundwater</topic><topic>Iron</topic><topic>Manganese</topic><topic>Minerals</topic><topic>Water analysis</topic><topic>Water depth</topic><topic>Water sampling</topic><topic>Water supply</topic><topic>Weathering</topic><toplevel>online_resources</toplevel><creatorcontrib>WANG, Xiaosong</creatorcontrib><creatorcontrib>LI, Baoxue</creatorcontrib><creatorcontrib>Yang, LI</creatorcontrib><collection>ProQuest Central (Corporate)</collection><collection>Agricultural Science Collection</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>SciTech Premium Collection</collection><collection>Agricultural Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central China</collection><collection>Wanfang Data Journals - Hong Kong</collection><collection>WANFANG Data Centre</collection><collection>Wanfang Data Journals</collection><collection>万方数据期刊 - 香港版</collection><collection>China Online Journals (COJ)</collection><collection>China Online Journals (COJ)</collection><jtitle>Guanʻgai paishui xuebao</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>WANG, Xiaosong</au><au>LI, Baoxue</au><au>Yang, LI</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>北京通州区第四系地下水化学特征及其成因分析</atitle><jtitle>Guanʻgai paishui xuebao</jtitle><date>2022-01-01</date><risdate>2022</risdate><volume>41</volume><issue>3</issue><spage>92</spage><epage>104</epage><pages>92-104</pages><issn>1672-3317</issn><abstract>【目的】揭示通州区地下水化学特征及其影响因素。【方法】利用2018年在通州区采集的45件300 m深度的地下水水质检测数据，通过Piper三线图、Gibbs图、因子分析和聚类分析等多元统计分析方法，分析了第四系地下水水化学特征及其影响因素。【结果】通州区第四系地下水浅层水化学类型以HCO3-Ca.Mg型为主，深层地下水化学类型以HCO3-Na型为主。通过因子分析共提取了4个公因子，其累计方差占总方差的85.45%。因子1代表盐度因子，反映了碳酸盐、硅酸盐矿物风化过程；因子2代表铁锰污染因子，反映了富含铁锰元素的矿物的风化作用；因子3代表农业污染因子，反映了农业活动对地下水的影响；因子4代表氟化物污染因子，反映了含氟矿物的风化及阳离子交换反应。【结论】农业活动主要影响通州北部宋庄、永顺一带；而碳酸盐、硅酸盐矿物风化作用，含铁锰元素矿物风化作用，含氟元素矿物风化作用及阳离子交换作用在通州全区普遍存在。</abstract><cop>Xinxiang City</cop><pub>Chinese Academy of Agricultural Sciences (CAAS) Farmland Irrigation Research Institute Editorial Office of Journal of Irrigation and Drainage</pub><doi>10.13522/j.cnki.ggps.2021190</doi><tpages>13</tpages></addata></record> |
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| subjects | Agricultural pollution Agricultural practices Agricultural production Agricultural wastes Agronomy Aquifers Boreholes Calcium Cation exchange Cation exchanging Cluster analysis Deep water Discriminant analysis Factor analysis Fluorides Fluorine Groundwater Iron Manganese Minerals Water analysis Water depth Water sampling Water supply Weathering |
| title | 北京通州区第四系地下水化学特征及其成因分析 |
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