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珠江三角洲平原区土壤Pb元素地球化学特征及其影响因素研究
引用本文:郭思雨,侯青叶,宗庆霞,唐志敏,韦彬,庞世琦. 珠江三角洲平原区土壤Pb元素地球化学特征及其影响因素研究[J]. 现代地质, 2019, 33(3): 514-524. DOI: 10.19657/j.geoscience.1000-8527.2019.03.05
作者姓名:郭思雨  侯青叶  宗庆霞  唐志敏  韦彬  庞世琦
作者单位:1.中国地质大学(北京) 地球科学与资源学院,北京 1000832.云南省地质调查院,云南 昆明 6502163.中国地质调查局 南京地质调查中心,江苏 南京 210016
基金项目:国家自然科学基金项目(41773019);中国地质调查局地质大调查项目“珠江三角洲土壤重金属地球化学成因与风险评价”(12120115050401)
摘    要:以珠江三角洲平原为研究区域,对其7个区县102件水稻根系土样品进行土壤理化参数及Pb形态分析,探讨在第四系分布区土壤Pb全量及Pb活动态含量的特征及影响因素。结果表明:全部供试土壤样品中Pb元素平均含量为46.47mg/kg,略高于广东省土壤Pb含量背景值(36mg/kg),表现出一定的累积趋势。研究区自西北陆相沉积区至南部海陆交互相沉积区,元素含量增高。Pb元素主要以残渣态和铁锰氧化物形态赋存在土壤中,迁移能力弱。影响土壤Pb全量的因素主要有Al2O3、K2O、Tl、Mo;影响土壤Pb活动态的因素有Pb全量、pH、有机质、CEC、P、TFe2O3、Mn;其中,p H是控制Pb元素活动性的最主要因素。

关 键 词:珠江三角洲平原  土壤    地球化学形态  影响因素
收稿时间:2018-08-02
修稿时间:2018-10-30

Geochemical Characteristics and Influence Factors of Lead in the Soils of the Pearl River Delta Plain,China
GUO Siyu,HOU Qingye,ZONG Qingxia,TANG Zhimin,WEI Bin,PANG Shiqi. Geochemical Characteristics and Influence Factors of Lead in the Soils of the Pearl River Delta Plain,China[J]. Geoscience of Geosciences, 2019, 33(3): 514-524. DOI: 10.19657/j.geoscience.1000-8527.2019.03.05
Authors:GUO Siyu  HOU Qingye  ZONG Qingxia  TANG Zhimin  WEI Bin  PANG Shiqi
Affiliation:1. School of Earth Sciences and Resources,China University of Geosciences,Beijing 100083,China2. Yunnan Institute of Geological Survey,Kunming,Yunnan 650216 ,China3. Nanjing Center, China Geological Survey,Nanjing,Jiangsu 210016,China
Abstract:This paper took the Pearl River Delta plain in Guangdong Province as the study area. We collected 102 surface soil samples from paddy fields and analyzed their physico-chemical parameters and Pb geochemical fractions.The main aims were to investigate the geochemical characteristics and to discuss the influence factors of total Pb contents and mobility fraction Pb contents in the soils. The results showed that the average value of total Pb contents in the soils was 46.47 mg/kg, which was slightly higher than the background value of soil Pb in Guangdong Province (36 mg/kg), indicating a certain accumulation trend. From northwest land sedimentary environment to south sea-land interaction sedimentary environment, the elements contents in the soils normally increased. Soil Pb were mainly composed of residual and Fe-Mn oxidation fraction with weak mobility. The factors affecting total Pb contents in the soils are aluminum oxide(Al2O3),potassium oxide (K2O),thallium(Tl),molybdenum(Mo). The factors controlling the mobility fraction of Pb are total Pb contents, pH, organic matter contents, cation exchange capacity (CEC), phosphorus(P), iron oxide(TFe2O3) and manganese (Mn). Among these factors, pH is the most important factor controlling the mobility of soil Pb.
Keywords:the Pearl River Delta plain  soil  Pb  geochemical fraction  influence factors  
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