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高校地质学报 ›› 2026, Vol. 32 ›› Issue (01): 38-48.DOI: 10.16108/j.issn1006-7493.2025020

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巢湖湖水中纳米颗粒的时空分布及其对元素循环的制约

徐子涛,周跃飞*,刘 焱,杜蒙蒙,谢巧勤,李全忠,陈天虎   

  1. 纳米矿物与污染控制安徽普通高校重点实验室,合肥工业大学 资源与环境工程学院,合肥 230009
  • 出版日期:2026-02-14 发布日期:2026-02-14

Temporal and Spatial Distribution of Nanoparticles in Lake Chaohu and Their Impact on Elemental Cycling

XU Zitao,ZHOU Yuefei*,LIU Yan,DU Mengmeng,XIE Qiaoqin,LI Quanzhong,CHEN Tianhu   

  1. Key Laboratory of Nanomaterials and Pollution Control, Hefei University of Technology, School of Resources and
    Environmental Engineering, Hefei 230009, China
  • Online:2026-02-14 Published:2026-02-14

摘要: 天然水中粒径小于0.22 μm的纳米颗粒物(NP)对溶解态元素的化学性质及其生物可利用性具有重要影响,但NP的小粒径及低浓度特征导致目前很难对其进行量化。该研究尝试采用电感耦合等离子体质谱仪(ICP-MS)和高分辨透射电镜
(HR-TEM)分析巢湖湖水中NP的种类、时空分布和微量元素特征。结果表明,ICP-MS直接测量过0.22 μm滤膜水样中元素(真实溶解态)的精密度高,该方法可以用于天然水中NP的分析。NP态(溶解态—真实溶解态)元素以Fe、Al为主,相对于春季,夏季前者减小,后者增大;NP-Fe高值区域两季均位于巢湖东南近出湖口,NP-Al高值区域春季位于巢湖南部,夏季位于巢湖北部。相关性分析表明,Cr、Mn、Zn、Ge、Cd在两季均与NP-Fe正相关,Ni、稀土、Pb夏季与NP-Fe正相关;对NP-Al则仅有Ti、Sc和中稀土夏季与之正相关。HR-TEM分析表明NP中主要物相为无定形物质、钙碳酸盐及具有一定晶形的针铁矿和铝硅酸盐,包括针铁矿在内的铁(氢)氧化物对巢湖中溶解态元素的循环产生重要制约作用。该文认为,NP主要来自河流,夏季河水流量和流速的增大导致NP输入增加;夏季湖水pH升高会促进NP态铁(氢)氧化物沉淀和铝硅酸盐分散。

关键词: 巢湖, 纳米颗粒物, 电感耦合等离子体质谱, 透射电镜, 铁(氢)氧化物, 微量元素

Abstract: Nanoparticles (NP) in natural waters with particle sizes <0.22 μm significantly influence the chemical properties and
bioavailability of dissolved elements. However, the small size and low concentration of NPs make their quantification challenging. This study employed inductively coupled plasma mass spectrometry (ICP-MS) and high-resolution transmission electron microscopy (HR-TEM) to analyze the species, spatiotemporal distribution, and trace element characteristics of NPs in Chaohu Lake. Results show that ICP-MS direct measurements of elements (truly dissolved fraction) in 0.22 μm membrane-filtered water samples exhibited high precision, validating this method for NP analysis in natural waters. NP-associated elements (dissolved fraction minus truly dissolved fraction) were dominated by Fe and Al, with their average concentrations remaining stable between spring and summer. High NP-Fe concentrations were consistently observed in the southeastern area near the lake outlet across both seasons, while NP-Al hotspots shifted from the southern lake region in spring to the northern region in summer. Correlation analysis revealed that Cr, Mn, Zn, Ge, and Cd showed positive correlations with NP-Fe in both seasons, whereas Pb, rare earth elements (REEs), and Ni exhibited summer-specific correlations with NP-Fe. For NP-Al, only Ti, Sc, and middle REEs displayed summer correlations. HR-TEM characterization identified amorphous Fe (hydr)oxides, aluminosilicates, and Ca carbonates as the predominant NP phases, with the first category playing a critical role in regulating dissolved element cycling in Chaohu Lake. The study concluded that riverine inputs constitute the primary NP source, with increased summer discharge enhancing NP influx. The increase in lake water pH during summer facilitates the precipitation of NP-iron (hydr)oxides and the dispersion of NPaluminosilicates. 

Key words: Chaohu Lake, nanoparticle, inductively coupled plasma-mass spectrometry, transmission electron microscopy, iron
(hydr)oxide,
trace elements

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