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物探与化探  2016, Vol. 40 Issue (4): 713-721    DOI: 10.11720/wtyht.2016.4.12
  区域地质调查 本期目录 | 过刊浏览 | 高级检索 |
福建龙海土壤垂向剖面元素分布特征
刘银飞1,2,3, 孙彬彬1,2,3, 贺灵2,3, 曾道明2,3, 刘占元2,3, 周国华2,3
1. 中国地质大学(北京) 地球科学与资源学院, 北京 100083;
2. 中国地质科学院 地球物理地球化学勘查研究所, 河北 廊坊 065000;
3. 国土资源部 地球化学勘查技术重点实验室, 河北 廊坊 065000
Vertical distribution of elements in soil profiles in Longhai,Fujian Province
LIU Yin-Fei1,2,3, SUN Bin-Bin1,2,3, HE Ling2,3, ZENG Dao-Ming2,3, LIU Zhan-Yuan2,3, ZHOU Guo-Hua2,3
1. School of Earth Sciences and Resources, China University of Geosciences(Beijing), Beijing 100083, China;
2. Institute of Geophysical and Geochemical Exploration, CAGS, Langfang 065000, China;
3. Key Laboratory for Geochemical Exploration Technology, MLR, Langfang 065000, China
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摘要 

基于福建省龙海市4类典型成土母质的垂向土壤剖面样品分析数据,研究了常量组分和微量元素含量及剖面分布特征。结果表明:研究区在温暖湿润气候条件下,化学风化作用强烈,Ca、Mg、Na、Si、K淋失贫化,含量明显低于全国均值,Al、Fe则相对富集,风化淋溶系数(ba)和硅铝铁率(Saf)值远低于全国土壤,土壤风化程度达到脱硅富铝铁阶段,花岗岩类成土母岩区风化作用尤为强烈;剖面土壤环境质量总体较好,微量元素含量与成土母质密切有关,九龙江口冲海积成因(剖面1)土壤重金属含量明显高于其他3个剖面;多数微量元素垂向分布受常量组分的控制,As、Cd、Cu、Hg、Pb、Zn与土壤中Fe等组分具有显著正相关性。因表层土壤中细粒黏质组分随地表径流淋失或下渗迁移,导致表层土壤低Fe、Al和重金属元素;在生物地球化学循环和人为污染的影响下,Hg、Cd、Pb、Zn等在表层土壤呈富集特征;多数重金属元素的相对富集系数小于1.0,且表层土壤无明显富集特征,认为除Hg、Pb等少数重金属元素外,其他元素受人为污染影响较小。

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Abstract

Based on geochemical data collected along four profiles at different types of geological setting and soil parent materials from Longhai, Fujian Province, the authors studied the concentrations and distribution patterns of major elements and trace elements. The results show that chemical weathering is intense. A lot of elements such as Ca, Mg, Na, Si and K have been seriously leached, but Fe and Al have been accumulated. The weathering-leaching index (ba value) and the ratio of Si to Fe and Al (Saf value) of the study area under the warm and humid subtropical condition are much lower than the average values of the whole country. The weathering degree has reached the stage of Si loss and Al-Fe enrichment, especially for the soils derived from granite rocks. Soil environmental quality is quite good due to its relative low concentration of heavy metals. It is found that the concentrations of trace elements including heavy metals are mainly controlled by the parent materials, and their vertical distribution along these profiles is mainly controlled by major components and organic carbon, indicating significant correlation between them. The concentrations of trace elements along profile 1 derived from alluvial and marine sediments are much higher than those of other three profiles. The relative low concentrations of Fe, Al as well as heavy metals may be attributed to the leaching of fine clay particles by surface runoff and infiltration. Several kinds of heavy metals such as Hg, Cd, Pb and Zn show accumulation in top soils under bio-geochemical cycle and human activities. The relative enrichment factors of most heavy metals are less than 1, which means that the anthropogenic influence are not serious except for Hg and P.

收稿日期: 2015-10-26      出版日期: 2016-08-10
:  P632  
基金资助:

国土资源部公益性行业科研专项经费项目“典型地质环境区红壤化过程地球化学特征研究”(201411091-2)

通讯作者: 周国华(1964-),博士,教授级高工,应用地球化学专业,主要从事环境地球化学调查与研究工作。E-mail:zhouguohua@igge.cn
作者简介: 刘银飞(1989-),硕士,地质工程专业。E-mail:416336373@qq.com
引用本文:   
刘银飞, 孙彬彬, 贺灵, 曾道明, 刘占元, 周国华. 福建龙海土壤垂向剖面元素分布特征[J]. 物探与化探, 2016, 40(4): 713-721.
LIU Yin-Fei, SUN Bin-Bin, HE Ling, ZENG Dao-Ming, LIU Zhan-Yuan, ZHOU Guo-Hua. Vertical distribution of elements in soil profiles in Longhai,Fujian Province. Geophysical and Geochemical Exploration, 2016, 40(4): 713-721.
链接本文:  
https://www.wutanyuhuatan.com/CN/10.11720/wtyht.2016.4.12      或      https://www.wutanyuhuatan.com/CN/Y2016/V40/I4/713

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