Article(id=1314921949344662111, tenantId=1146029695717560320, journalId=1234093305789726721, issueId=1314921940238828053, articleNumber=null, orderNo=null, doi=null, pmid=null, cstr=null, oa=null, hot=null, price=null, onlineType=0, articleFormat=0, articleType=null, articleTypeStr=null, receivedDate=1747238400000, receivedDateStr=2025-05-15, revisedDate=null, revisedDateStr=null, acceptedDate=null, acceptedDateStr=null, onlineDate=1791431422792, onlineDateStr=2026-10-08, pubDate=1768838400000, pubDateStr=2026-01-20, doiRegisterDate=null, doiRegisterDateStr=null, onlineIssueDate=1791431422792, onlineIssueDateStr=2026-10-08, onlineJustAcceptDate=null, onlineJustAcceptDateStr=null, onlineFirstDate=null, onlineFirstDateStr=null, sourceXml=null, magXml=null, createTime=1791431422792, creator=13701087609, updateTime=1791431422792, updator=13701087609, issue=Issue{id=1314921940238828053, tenantId=1146029695717560320, journalId=1234093305789726721, year='2026', volume='46', issue='1', pageStart='1', pageEnd='592', issueExtLink='null', onlineDate='null', pubDate='1768838400000', pubDateStr='2026-01-20', beforeIssueId=null, nextIssueId=null, price=null, status=1, issueComplete=1, articleOrder=1, issueType=-1, specialIssue=null, createTime=1791431420621, creator='13701087609', updateTime=1791431552947, updator='13701087609', preIssue=null, nextIssue=null, articleTotal=null, ext={EN=IssueExt(id=1314922495317210104, tenantId=1146029695717560320, journalId=1234093305789726721, issueId=1314921940238828053, language=EN, specialIssueTitle=, coverIllustrator=null, specialIssueEditor=, specialIssueAbout=), CN=IssueExt(id=1314922495317210105, tenantId=1146029695717560320, journalId=1234093305789726721, issueId=1314921940238828053, language=CN, specialIssueTitle=, coverIllustrator=null, specialIssueEditor=, specialIssueAbout=)}, issueFiles=null, downloadFileDto=null}, startPage=11, endPage=19, ext={EN=ArticleExt(id=1314921949499851361, articleId=1314921949344662111, tenantId=1146029695717560320, journalId=1234093305789726721, language=EN, title=High background of soil heavy metals developed from carbonate rocks: issues about formation and risk, columnId=null, journalTitle=China Environmental Science, columnName=null, runingTitle=null, highlight=null, articleAbstract=

The research progress of high background of soil heavy metals related to carbonate rocks was systematically reviewed from the aspects of spatial distribution, element combination, spatial coverage, controlling factors, formation process, and risk characteristics. At present, it was generally believed that the main causation for the formation of this type of high background was the "secondary enrichment" of elements in the weathering process of parent rock, that is, the leaching of major elements, e.g. Ca, caused the relative enrichment of trace elements, e.g. Cd. In this process, iron and manganese minerals played an important role in the in-situ concentration of these elements. From the geographical perspective, the hot and humid climate was conducive to the formation of a higher background content. In general, Cd and other elements in soil developed from carbonate eluvium had the character of "high background with low activity", while in the alluvial areas formed by carbonate weathered materials, high acid soluble state of Cd might have occurred with risks of activation under conditions such as soil acidification. With high spatial variation of soil heavy metals in such areas, especially in the medium and small spatial scales, problems such as differentiation between natural background and anthropogenic pollution, quantitative recognition of relative risks, and development of control measures for environmental management, were required to be solved in the future study.

, authors=Ya-nan LI1, Xue-qi XIA1, *, Zhong-fang YANG1, Xin-zhe LU2, Chun-lei HUANG2, authorsList=Ya-nan LI, Xue-qi XIA, Zhong-fang YANG, Xin-zhe LU, Chun-lei HUANG, authorCompany=null, correspAuthors=Xue-qi XIA, authorNote=null, correspAuthorsNote=null, copyrightStatement=null, copyrightOwner=null, extLink=null, articleAbsUrl=null, sourceXml=null, magXml=null, pdfUrl=null, pdf=null, pdfFileSize=null, pdfExtLink=null, richHtmlUrl=null, mobilePdfUrl=null, reviewReport=null, pdfFirstPage=null, abstractGraph=null, abstractGraphContent=null, abstractVideo=null, citation=null, cebUrl=null, magXmlContent=null, mapNumber=null, fund=null), CN=ArticleExt(id=1314921949843784290, articleId=1314921949344662111, tenantId=1146029695717560320, journalId=1234093305789726721, language=CN, title=碳酸盐岩发育土壤重金属高背景:形成因素和风险特征, columnId=1314921943346802741, journalTitle=中国环境科学, columnName=岩溶关键带重金属污染成因, runingTitle=null, highlight=null, articleAbstract=

从空间分布、元素组合、高背景范围、元素富集程度的控制因素,以及形成原因和风险特征等方面,系统梳理碳酸盐岩有关的土壤重金属高背景研究进展.当前普遍认为,该类高背景形成的主要因素是母岩风化过程中的“次生富集”,即钙等常量元素淋失造成镉等微量元素的相对富集,在此过程中,铁锰矿物对这些元素的原地富集发挥了重要作用.从宏观角度,湿热的气候更有利于形成更高的背景含量.总体上,碳酸盐岩残积背景下镉等元素具有“高背景,低活性”特征,而在以其为物源的冲积区,存在酸溶态较高的现象,在土壤酸化等特定条件下,存在被活化风险.在中小尺度空间变异复杂的情况下,如何对该类高背景下自然背景与人为污染进行区分,开展相关风险定量识别,以及制定相关管控措施,是未来研究的重要方向.

, authors=李雅男1, 夏学齐1, *, 杨忠芳1, 卢新哲2, 黄春雷2, authorsList=李雅男, 夏学齐, 杨忠芳, 卢新哲, 黄春雷, authorCompany=null, correspAuthors=夏学齐, authorNote=

李雅男(2001-),女,黑龙江牡丹江人,中国地质大学(北京)硕士研究生,主要研究方向为环境地球化学..

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* 责任作者,教授,
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李雅男(2001-),女,黑龙江牡丹江人,中国地质大学(北京)硕士研究生,主要研究方向为环境地球化学..

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李雅男(2001-),女,黑龙江牡丹江人,中国地质大学(北京)硕士研究生,主要研究方向为环境地球化学..

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碳酸盐岩发育土壤重金属高背景:形成因素和风险特征
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李雅男 1 , 夏学齐 1, * , 杨忠芳 1 , 卢新哲 2 , 黄春雷 2
中国环境科学 | 岩溶关键带重金属污染成因 2026,46(1): 11-19
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中国环境科学 |岩溶关键带重金属污染成因 2026 , 46 (1) : 11 -19
碳酸盐岩发育土壤重金属高背景:形成因素和风险特征
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李雅男(2001-),女,黑龙江牡丹江人,中国地质大学(北京)硕士研究生,主要研究方向为环境地球化学..

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李雅男(2001-),女,黑龙江牡丹江人,中国地质大学(北京)硕士研究生,主要研究方向为环境地球化学..

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李雅男1 , 夏学齐1, * , 杨忠芳1, 卢新哲2, 黄春雷2
作者信息
  • 1.中国地质大学(北京)地球科学与资源学院,北京 100083
  • 2.浙江省地质院,浙江 杭州 310007
通讯作者:
* 责任作者,教授,
作者简介:

李雅男(2001-),女,黑龙江牡丹江人,中国地质大学(北京)硕士研究生,主要研究方向为环境地球化学..

High background of soil heavy metals developed from carbonate rocks: issues about formation and risk
Ya-nan LI1 , Xue-qi XIA1, * , Zhong-fang YANG1, Xin-zhe LU2, Chun-lei HUANG2
Affiliations
  • 1.School of Earth Sciences and Resources, China University of Geosciences(Beijing), Beijing 100083, China
  • 2.Zhejiang Geology Institute, Hangzhou 310007, China
出版时间: 2026-01-20
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从空间分布、元素组合、高背景范围、元素富集程度的控制因素,以及形成原因和风险特征等方面,系统梳理碳酸盐岩有关的土壤重金属高背景研究进展.当前普遍认为,该类高背景形成的主要因素是母岩风化过程中的“次生富集”,即钙等常量元素淋失造成镉等微量元素的相对富集,在此过程中,铁锰矿物对这些元素的原地富集发挥了重要作用.从宏观角度,湿热的气候更有利于形成更高的背景含量.总体上,碳酸盐岩残积背景下镉等元素具有“高背景,低活性”特征,而在以其为物源的冲积区,存在酸溶态较高的现象,在土壤酸化等特定条件下,存在被活化风险.在中小尺度空间变异复杂的情况下,如何对该类高背景下自然背景与人为污染进行区分,开展相关风险定量识别,以及制定相关管控措施,是未来研究的重要方向.

土壤  /  重金属  /  地质高背景  /  碳酸盐岩  /  形成原因  /  风险特征

The research progress of high background of soil heavy metals related to carbonate rocks was systematically reviewed from the aspects of spatial distribution, element combination, spatial coverage, controlling factors, formation process, and risk characteristics. At present, it was generally believed that the main causation for the formation of this type of high background was the "secondary enrichment" of elements in the weathering process of parent rock, that is, the leaching of major elements, e.g. Ca, caused the relative enrichment of trace elements, e.g. Cd. In this process, iron and manganese minerals played an important role in the in-situ concentration of these elements. From the geographical perspective, the hot and humid climate was conducive to the formation of a higher background content. In general, Cd and other elements in soil developed from carbonate eluvium had the character of "high background with low activity", while in the alluvial areas formed by carbonate weathered materials, high acid soluble state of Cd might have occurred with risks of activation under conditions such as soil acidification. With high spatial variation of soil heavy metals in such areas, especially in the medium and small spatial scales, problems such as differentiation between natural background and anthropogenic pollution, quantitative recognition of relative risks, and development of control measures for environmental management, were required to be solved in the future study.

soil  /  heavy metals  /  high geochemical background  /  carbonate rocks  /  causes of formation  /  risk characteristics
李雅男, 夏学齐, 杨忠芳, 卢新哲, 黄春雷. 碳酸盐岩发育土壤重金属高背景:形成因素和风险特征. 中国环境科学, 2026 , 46 (1) : 11 -19 .
Ya-nan LI, Xue-qi XIA, Zhong-fang YANG, Xin-zhe LU, Chun-lei HUANG. High background of soil heavy metals developed from carbonate rocks: issues about formation and risk[J]. China Environmental Science, 2026 , 46 (1) : 11 -19 .
  • 国家重点研发计划(2022YFC3702303)
  • 国家自然科学基金重点项目(42330703)
  • 浙江省财政地质专项资金项目[省资](2023021)
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  • 接收时间:2025-05-15
  • 首发时间:2026-10-08
  • 出版时间:2026-01-20
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  • 收稿日期:2025-05-15
基金
国家重点研发计划(2022YFC3702303)
国家自然科学基金重点项目(42330703)
浙江省财政地质专项资金项目[省资](2023021)
作者信息
    1.中国地质大学(北京)地球科学与资源学院,北京 100083
    2.浙江省地质院,浙江 杭州 310007

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* 责任作者,教授,
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2种不同金属材料的力学参数
科
Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)
属
Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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