收藏切换
High background of soil heavy metals developed from carbonate rocks: issues about formation and risk
收藏切换
Ya-nan LI1, Xue-qi XIA1, *, Zhong-fang YANG1, Xin-zhe LU2, Chun-lei HUANG2
China Environmental Science | 2026, 46(1) : 11 - 19
Less
收藏切换
China Environmental Science | 2026, 46(1): 11-19
High background of soil heavy metals developed from carbonate rocks: issues about formation and risk
Full
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
Published: 2026-01-20
Outline
收藏切换

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 .
Year 2026 volume 46 Issue 1
65
20
Cite this Article
BibTeX
Article Info
  • Receive Date:2025-05-15
  • Online Date:2026-10-08
  • Published:2026-01-20
Article Data
Affiliations
History
  • Received:2025-05-15
Funding
Affiliations
    1.School of Earth Sciences and Resources, China University of Geosciences(Beijing), Beijing 100083, China
    2.Zhejiang Geology Institute, Hangzhou 310007, China
References
Share
https://castjournals.cast.org.cn/joweb/zghjkx/EN/
Share to
QR

Scan QR to access full text

Cite this article
BibTeX
Citations
表12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
关闭全屏
  • BibTeX
  • EndNote
  • RefWorks
  • TxT