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现代地质 ›› 2025, Vol. 39 ›› Issue (04): 1098-1107.DOI: 10.19657/j.geoscience.1000-8527.2024.058

• 地球化学 • 上一篇    下一篇

黑龙江省庆安地区土壤-作物系统硒地球化学特征及影响因素

刘婷1,2,3(), 张立1,2,3,4,*(), 吕石佳1,2, 张思宇1, 王刚1,2, 孙振伟1   

  1. 1.黑龙江省自然资源调查院,黑龙江省 哈尔滨 150036
    2.黑龙江省黑土地水土资源研究重点实验室,黑龙江省 哈尔滨 150036
    3.哈尔滨黑土地地球关键带野外科学观测研究站,黑龙江省 哈尔滨 150086
    4.吉林大学地球科学学院,吉林 长春 130061
  • 出版日期:2025-08-10 发布日期:2025-08-27
  • 通信作者: *张立,男,正高级工程师,1981年出生,主要从事环境地球化学方面研究工作,Email:hljdcyzl@126.com
  • 作者简介:刘婷,女,助理工程师,1996年出生,主要从事环境地球化学方面研究工作,Email:1084595199@qq.com
  • 基金资助:
    黑龙江省自然科学基金项目(LH2022D030);黑龙江省地质勘查专项(黑国土资函[2017]454号)

Geochemical Characteristics and Influencing Factors of Selenium in Soil-Crop System of Qing’an Area, Heilongjiang Province

LIU Ting1,2,3(), ZHANG Li1,2,3,4,*(), LÜ Shijia1,2, ZHANG Siyu1, WANG Gang1,2, SUN Zhenwei1   

  1. 1. Natural Resources Survey Institute of Heilongjiang Province, Harbin, Heilongjiang 150036, China
    2. Key Laboratory of Black Soil and Water Resources Research of Heilongjiang Province, Harbin, Heilongjiang 150036, China
    3. Observation and Research Station of Earth Critical Zone in Black Soil, Harbin, Heilongjiang 150086, China
    4. College of Earth Sciences, Jilin University, Changchun, Jilin 130061, China
  • Published:2025-08-10 Online:2025-08-27

摘要:

我国土壤普遍缺硒(Se),近年来松嫩平原发现大面积富硒土壤带,但目前缺乏系统科学的评价,硒形成机制及其影响因素的研究不足,严重制约了富硒土地开发和可持续利用。以黑龙江省庆安地区土壤和农作物为研究对象,采集了8689件表层土壤样品、40件垂向剖面土壤样品、180套农作物及根系土样品,分析测试了各类样品总硒、重金属元素等理化指标。结果表明,表层土壤硒含量为0.03~0.93 mg/kg,平均含量0.28 mg/kg,以足硒土壤为主,占比93.93%,Se垂向分布特征表现为表聚型,次生富集作用明显;成土母质以湖积物发育的土壤Se含量较高,土壤类型对Se含量影响较小,黑土和草甸土Se含量相对较高,不同土地利用方式下,耕地土壤Se含量较高,不同作物籽实对Se元素富集能力强弱依次为:水稻>大豆>玉米。元素间的相关分析与统计结果表明,成土母质、土壤有机质、pH是影响研究区土壤硒含量的主要因素,土壤硒、土壤有机质是影响农作物籽实硒含量的关键因素,建议该地区以水稻、大豆逐渐代替玉米的种植结构调整可降低农作物缺硒风险,以满足居民硒健康的需求。

关键词: 土壤硒, 农作物, 地球化学特征, 影响因素, 庆安地区

Abstract:

Selenium (Se) deficiency is widespread in China’s soils. In recent years, large areas of selenium-rich soil zones have been discovered in the Songnen Plain; however, there is a lack of systematic scie.pngic evaluation, and research on the formation mechanism of selenium and its influencing factors is insufficient, which seriously restricts the development and sustainable utilization of selenium-rich land. Taking soil and crops in Qing’an Area, Heilongjiang Province as the research object, 8689 surface soil samples, 40 vertical soil profile samples, and 180 sets of crop and root soil samples were collected. Physical and chemical indicators such as total selenium and heavy metal elements in various samples were analyzed and tested.The results show that:(1) The selenium content in surface soil ranges from 0.03 to 0.93 mg/kg, with an average of 0.28 mg/kg, mainly dominated by selenium-sufficient soil (accounting for 93.93%). The vertical distribution of Se shows a surface-aggregated pattern with obvious secondary enrichment;(2) Soils developed from lacustrine sediments have relatively high Se content. Soil types have little impact on Se content, with black soil and meadow soil having relatively higher Se content. Under different land use patterns, cultivated land has higher Se content. The Se enrichment capacity of different crop grains in descending order is: rice>soybean>corn;(3) Correlation analysis and statistical results among elements indicate that parent material, soil organic matter, and pH are the main factors affecting soil Se content in the study area. Soil selenium and soil organic matter are key factors influencing Se content in crop grains. It is recommended that adjusting the planting structure by gradually replacing corn with rice and soybean in this region can reduce the risk of selenium deficiency in crops, meeting residents’ selenium-related health needs.

Key words: soil selenium, crop, geochemical characteristics, influencing factors, Qing’an Area

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