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广东省普宁市土壤硒的分布特征及影响因素研究
引用本文:蒋慧豪,罗杰,蔡立梅,穆桂珍,唐翠华,王秋爽,王硕,孙蓉蓉.广东省普宁市土壤硒的分布特征及影响因素研究[J].现代地质,2019,33(1):161-168.
作者姓名:蒋慧豪  罗杰  蔡立梅  穆桂珍  唐翠华  王秋爽  王硕  孙蓉蓉
作者单位:1.长江大学 资源与环境学院, 湖北 武汉 4301002.中国科学院 广州地球化学研究所矿物学与成矿学重点实验室, 广东 广州 5106403.中国科学院 广州地球化学研究所有机地球化学国家重点实验室, 广东 广州 510640
基金项目:国家自然科学基金项目(41203061);湖北省自然科学基金项目(2015CFB603);湖北省教育厅科学技术研究重点项目(D20161301);中国科学院广州地球化学研究所有机地球化学国家重点实验室开放基金项目(OGL-201408);长江大学大学生创新创业训练项目(2015007);长江大学大学生创新创业训练项目(2016006)
摘    要:开展了广东省普宁市区域土壤硒调查研究,采集了413个表层土壤样品(0~20 cm)和103个深层土壤样品(> 150 cm),测定了土壤全硒含量,据此研究土壤硒分布特征及其影响因素。结果表明,普宁市土壤全硒含量变化于0. 16~2. 01 mg/kg,平均值为0. 63 mg/kg,总体上处于中硒及高硒水平,不存在缺硒和硒过剩土壤。砂页岩风化形成的赤红壤全硒含量较高,平均值达0. 86 mg/kg,以侏罗系页岩母质发育的土壤全硒含量最高,平均值达0. 89 mg/kg;三角洲第四系沉积物发育形成的水稻土全硒含量最低,平均值为0. 41 mg/kg。回归分析表明,土壤全硒含量与铁铝含量、有机碳含量具有极显著正相关,与p H呈极显著负相关。影响普宁市土壤硒含量的主要因素是成土母质,土壤p H、有机碳和铁铝含量及土地利用方式对土壤全硒含量分布与富集也有一定的影响。

关 键 词:普宁市  土壤全硒  分布特征  影响因素
收稿时间:2018-04-18
修稿时间:2018-09-24

Distribution of Selenium and Its Influencing Factors in Soils of Puning City,Guangdong Province
JIANG Huihao,LUO Jie,CAI Limei,MU Guizhen,TANG Cuihua,WANG Qiushuang,WANG Shuo,SUN Rongrong.Distribution of Selenium and Its Influencing Factors in Soils of Puning City,Guangdong Province[J].Geoscience——Journal of Graduate School,China University of Geosciences,2019,33(1):161-168.
Authors:JIANG Huihao  LUO Jie  CAI Limei  MU Guizhen  TANG Cuihua  WANG Qiushuang  WANG Shuo  SUN Rongrong
Institution:1. College of Resources and Environment, Yangtze University, Wuhan,Hubei 430100, China2. Key Laboratory of Mineralogy and Metallogeny, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou,Guangdong 510640, China3. State Key Laboratory of Organic Geochemistry, Chinese Academy of Sciences, Guangzhou,Guangdong 510640, China
Abstract:A systematic investigation of soil selenium in the region of Puning City was carried out, and 413 samples of surface soil (0-20 cm) and 103 samples of deep soil (>150 cm) were collected systematically and analyzed for content, distribution and influencing factors of soil Se. Results showed that the content of total selenium in the surface soils ranged from 0.16 mg/kg to 2.01 mg/kg with a mean value of 0.63 mg/kg, which meant that the soils were in the category of Se sufficiency or Se abundance on the whole, with none in the category of Se deficiency or excessive Se. Among the different types of soils, total Se content was the highest in red soil formed by sand shale, averaging 0.86 mg/kg,and the lowest in paddy soils developed in delta sediments, averaging 0.41 mg/kg. Among the different types of parent materials, the highest content was recorded in Jurassic shale with an average Se content of 0.89 mg/kg, while the lowest in Quaternary sediment with an average of 0.41 mg/kg. Correlation and regression analysis showed that soil Se content was significantly and positively related to contents of iron and aluminum, soil total organic carbon (SOC), but negatively to soil pH. Soil parent material was the major factor influencing selenium concentration and distribution in the soil of Puning City, whereas land use, soil pH, SOC, iron and aluminum also played important roles.
Keywords:Puning City  soil total selenium  distribution characteristic  influencing factor  
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