首页 | 本学科首页   官方微博 | 高级检索  
     

广东乳源典型富硒区土壤硒元素地球化学特征及其影响因素探讨
引用本文:刘子宁, 李樋, 莫滨, 贾磊, 赵艺, 赵立波, 吴君毅. 2024. 广东乳源典型富硒区土壤硒元素地球化学特征及其影响因素探讨. 沉积与特提斯地质, 44(1): 185-193. doi: 10.19826/j.cnki.1009-3850.2023.08004
作者姓名:刘子宁  李樋  莫滨  贾磊  赵艺  赵立波  吴君毅
作者单位:1.广东省地质调查院,广东 广州 510080;; 2.成都理工大学地球科学学院,四川 成都 610059;; 3.中国地质大学(北京),北京 100083
基金项目:广东省地勘专项基金项目“广东南岭国家公园生态保护区生态地质调查”(2022-21);广东省生态环境调查项目“韶关市土壤环境质量详查:韶关市土壤背景值调查”(H2017067S)
摘    要:以广东省乳源瑶族自治县富硒(Se)土壤为研究对象,依据研究区422件表层土壤调查数据,探讨研究了土壤中不同要素下Se元素含量的地球化学特征、空间分布特征及其影响因素。研究结果表明:研究区土壤Se元素平均含量为0.65 mg·kg-1,分别是韶关市背景值、广东省背景值和全国丰度的1.97、2.71和2.95倍。富硒土壤主要分布在研究区的中西部地区,共圈定2061.31 km2富硒土壤,占研究区总面积的89.66%。不同土地利用类型下,Se含量整体呈现为林地>园地>草地>耕地。研究区土壤Se元素富集主要受到成土母质的控制,土壤中Se含量最高的成土母质类型为泥质岩类风化形成的土壤,富硒率为93.33%;其次受到研究区内表生地球化学作用及S、N等元素的吸附固定作用影响,有利于土壤Se元素的富集。研究区土壤中Se与pH呈显著的负相关关系,即pH值越低,Se含量越高。这些认识有利于对当地富硒土地资源的合理规划利用提供一定科学依据,具有较好的农业经济意义。

关 键 词:   土壤   地球化学   空间分布   乳源瑶族自治县
收稿时间:2022-11-04
修稿时间:2022-11-30

Selenium-rich soils in the area of Ruyuan,Guangdong, China: Se geochemistry and evaluation of factors controlling Se enrichment
LIU Zining, LI Tong, MO Bin, JIA Lei, ZHAO Yi, ZHAO Libo, WU Junyi. 2024. Selenium-rich soils in the area of Ruyuan, Guangdong, China: Se geochemistry and evaluation of factors controlling Se enrichment. Sedimentary Geology and Tethyan Geology, 44(1): 185-193. doi: 10.19826/j.cnki.1009-3850.2023.08004
Authors:LIU Zining  LI Tong  MO Bin  JIA Lei  ZHAO Yi  ZHAO Libo  WU Junyi
Affiliation:1.Guandong Institute of geological survey, Guangzhou 510080, China;; 2.School of Earth Science, Chengdu University of Technology, Chengdu 610059, China;; 3.China University of Geosciences (Beijing), Beijing 100083, China
Abstract:A survey of 422 surface soil samples in the Ruyuan Yao Autonomous County of Guangdong Province was done to determine the geochemistry and spatial distribution of Se, and to evaluate factors that could influence Se distributions in soils in the study area. Results showed that the average content of Se in soil of the study area was 0.65 mg·kg-1, which was 1.97, 2.71 and 2.95 times that of the background values of Shaoguan City, Guangdong Province, and the national average, respectively. The selenium-rich soil is mainly distributed in the central and western regions of the study area, and a total area of 2061.31 km2 of selenium-rich soil is delineated, accounting for 89.66% of the total study area. Soil Se concentrations vary by land use type: forest land > garden land > grassland > cultivated land. The enrichment of Se in the soil of the study area is mainly controlled by the parent material. The type of parent material with the highest soil Se content is soil formed by the weathering of argillaceous rocks, where soil selenium is enriched 93.33% relative to parent rock. Secondly, it is affected by the supergene geochemistry and the adsorption and fixation of S, N and other elements in the study area, which is conducive to the enrichment of Se in soil. There was a significant negative correlation between Se and pH in the soil of the study area, that is, the lower the pH value, the higher the Se content. These insights provide a scientific basis for the rational planning and utilization of local selenium-rich land resources, especially for considering agricultural land uses. Se can provide an essential nutrient or adversely affect crops, depending on Se concentrations and chemical form.
Keywords:selenium  soil  geochemistry  spatial distribution  Ruyuan Yao Autonomous County
点击此处可从《沉积与特提斯地质》浏览原始摘要信息
点击此处可从《沉积与特提斯地质》下载全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号