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[典型地质高背景区土壤硒镉迁移累积特征及其生物有效性]

[Characteristics of Soil Selenium-cadmium Migration and Accumulation and Its Bioeffectiveness in Typical Geological High Background Area].

作者信息

Zhou Ya-Long, Peng Min, Yang Zhi-Bin, Chen Jie, Wang Cheng-Wen, Han Wei

机构信息

Institute of Geophysical & Geochemical Exploration, Chinese Academy of Geological Sciences, Langfang 065000, China.

Research Center of Geochemical Survey and Assessment on Land Quality, China Geological Survey, Langfang 065000, China.

出版信息

Huan Jing Ke Xue. 2024 Aug 8;45(8):4860-4869. doi: 10.13227/j.hjkx.202309030.

Abstract

The prevalence of selenium-cadmium (Se-Cd) symbiosis in soils of geologically high background areas directly affects the safe utilization of Se-rich land resources. To investigate the migration and accumulation characteristics and bio-effectiveness of Se-Cd in the soil-crop system in typical geological high background areas of Southwest China and to realize the safe use of natural Se-rich land resources in geological high background areas, we collected 84 samples of agricultural crops (maize) and their supporting root systems and analyzed the Se-Cd content and physicochemical properties. Se-Cd accumulation characteristics, influencing factors, and bio-effectiveness of the soil-crop system were evaluated using geostatistics, bioenrichment factors, and geographic detectors. The results showed that the Se-Cd content in the study area was significantly higher than the background value of the soil in the whole country and in Yunnan Province. Influenced by the geological background, secondary enrichment in the process of soil formation, and agricultural activities, the accumulation and enrichment characteristics of Se in the root soil varied from no enrichment to slightly enriched, and the occurrence form was dominated by the residue state. The accumulation index of soil Cd was mainly in the medium pollution level, and the occurrence form was mainly in the residual state and the combined state of iron and manganese. The Se-enrichment rate of crop seeds reached 98.8% (DB 50/T 524-2013 standard), and the average value of bioconcentration factor was 5.8%. The exceeding rate of Cd content in crop seeds was only 1.19% (GB 2762-2022 standard), and the average value of Cd bioconcentration factor was 2.11%, so the ecological risk of heavy metal Cd in crop seeds was relatively low. In the Se-Cd symbiosis area under geological background, the weak alkaline environment of the soil could effectively reduce the bioavailability of Cd in crop seeds, and the Se-rich soil could inhibit the uptake of Cd by the crops to a certain extent. Correlation analysis showed that the migration and accumulation of Se and Cd from soil to crop seeds in the soil-crop system were affected by the elemental accumulation pattern and the physical and chemical properties (pH) of the soil, and at the same time, there was a certain synergistic-antagonistic effect between Se and Cd in the soil-crop system. Correlation analysis showed that the migration and accumulation of Se and Cd from soil to crop seeds in the soil-crop system was influenced by the occurrence of elements, soil physicochemical properties (pH), and other factors, and there was also a certain synergistic-antagonistic interaction between Se and Cd in the soil-crop system.

摘要

地质高背景区土壤中硒镉(Se-Cd)共生现象的普遍存在直接影响着富硒土地资源的安全利用。为研究中国西南典型地质高背景区土壤-作物系统中Se-Cd的迁移累积特征及生物有效性,实现地质高背景区天然富硒土地资源的安全利用,我们采集了84份农作物(玉米)及其配套根系样本,分析了Se-Cd含量和理化性质。利用地统计学、生物富集系数和地理探测器对土壤-作物系统的Se-Cd累积特征、影响因素及生物有效性进行了评价。结果表明,研究区Se-Cd含量显著高于全国及云南省土壤背景值。受地质背景、土壤形成过程中的次生富集及农业活动影响,根际土壤中Se的累积富集特征从无富集到轻度富集不等,赋存形态以残渣态为主。土壤Cd的累积指数主要处于中度污染水平,赋存形态主要为残渣态及铁锰结合态。作物种子的Se富集率达98.8%(DB 50/T 524-2013标准),生物富集系数平均值为5.8%。作物种子中Cd含量超标率仅为1.19%(GB 2762-2022标准),Cd生物富集系数平均值为2.11%,因此作物种子中重金属Cd的生态风险相对较低。在地质背景下的Se-Cd共生区,土壤的弱碱性环境可有效降低作物种子中Cd的生物有效性,富硒土壤可在一定程度上抑制作物对Cd的吸收。相关性分析表明,土壤-作物系统中Se和Cd从土壤向作物种子的迁移累积受元素累积模式和土壤理化性质(pH值)的影响,同时,土壤-作物系统中Se和Cd之间存在一定的协同-拮抗效应。相关性分析表明,土壤-作物系统中Se和Cd从土壤向作物种子的迁移累积受元素赋存形态、土壤理化性质(pH值)等因素影响,土壤-作物系统中Se和Cd之间也存在一定的协同-拮抗相互作用。

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