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长三角典型工业-农业复合区杭嘉湖平原土壤锡的空间分布与成因解析

Spatial Distribution and Controlling Factors of Tin in Soils of the Hangjiahu Plain: A Typical Industrial-Agricultural Integrated Area of the Yangtze River Delta

  • 摘要: 锡(Sn)作为一种具有潜在环境风险的新污染物,受关注程度较低,但人类活动(工业发展和农业生产)导致土壤Sn污染的现象逐渐凸显。本文以长三角典型工业-农业复合区——浙江杭嘉湖平原区为研究对象,采集表层(0~20cm,n=1982)、深层(150~200cm,n=510)及土壤垂向剖面样品,综合分析了土壤Sn的分布特征及影响因素。结果表明,表层土壤Sn含量变化范围为2.10~110.00mg/kg,深层土壤为1.75~100.00mg/kg,表层土壤Sn含量均值(10.72mg/kg)是深层土壤(4.07mg/kg)的2.63倍,Sn元素呈现显著的表层富集特征。土壤Sn高值区集中分布于杭州市及嘉善县、桐乡市等局部区域,表层和深层空间格局总体一致,但表层高值区范围显著扩大。土壤Sn元素垂向分布随深度的增加呈“先降后升”趋势,40~80cm深度出现明显低值带,80cm以下含量回升,这种分布模式可能与淋溶迁移和继承深层母质特性的共同作用有关。土壤理化性质分析显示,表层土壤呈酸性(pH 3.8~8.8,均值6.3)且有机碳富集(TOC均值1.40%),显著区别于深层土壤(pH 4.7~9.3,均值7.6;TOC均值0.8%)。相关性及主成分分析结果表明,表层土壤Sn含量分布主要受土壤pH调控(r=0.336,P<0.01)、有机碳络合(r=0.105,P<0.01)和土壤风化进程(r=−0.401,P<0.01)的共同作用;深层土壤Sn含量则以母质继承为主导(不同母质间P>0.05),但在海岸沉积物发育区,受表层酸化驱动的垂向迁移影响显著增强。研究揭示,人类活动(如电子废弃物处置、含Sn农药施用)通过改变表层土壤酸度和有机质动态,重塑Sn的空间分布格局,建议重点防控高迁移活性母质区与人为干扰热点区的叠加效应。

     

    Abstract: Tin (Sn), as an emerging pollutant with potential environmental risks, has received relatively limited attention. However, soil Sn pollution caused by human activities (industrial development and agricultural production) has become increasingly prominent. This study focused on the Hangjiahu Plain in Zhejiang Province, a typical industrial-agricultural integrated area of the Yangtze River Delta, China, as the study area. Surface soil samples (0–20cm, n=1982), deep soil samples (150–200cm, n=510), and soil vertical profile samples were collected to comprehensively analyze the spatial distribution patterns and controlling factors of soil Sn. Results showed that Sn content in surface soils ranged from 2.10 to 110.00mg/kg, while in deep soils it ranged from 1.75 to 100.00mg/kg. The mean Sn content in surface soils (10.72mg/kg) was 2.63 times higher than that in deep soils (4.07mg/kg), indicating substantial Sn enrichment in surface soils. Significant Sn hotspots were identified in Hangzhou City, Jiashan County, and Tongxiang City. While spatial distribution patterns were generally consistent across depths, surface soil hotspots exhibited pronounced spatial expansion. Vertical distribution profiles demonstrated a characteristic “decline-rise” pattern with depth, featuring a distinct low-value zone at 40–80cm followed by concentration recovery below 80cm, reflecting the combined influence of leaching processes and parent material inheritance. Geochemical characterization showed surface soils were predominantly acidic (pH 3.8–8.8; mean: 6.3) with elevated organic carbon content (mean TOC: 1.40%), differing significantly from deep soils (pH 4.7–9.3, mean: 7.6; mean TOC: 0.8%). Statistical analyses revealed that Sn distribution in surface soils was predominantly regulated by soil pH (r=0.336, P<0.01), organic carbon complexation (r=0.105, P<0.01), and soil weathering intensity (r=−0.401, P<0.01). In contrast, Sn contents in deep soils were primarily dominated by parent material inheritance (P>0.05 among different parent materials) but showed significantly intensified vertical migration effects driven by surface acidification in coastal sediment-developed areas. The study reveals that human activities (such as electronic waste disposal and Sn-containing agrochemical application) reshape the spatial Sn distribution patterns by altering surface soil acidity and organic matter dynamics. The findings highlight the need for targeted management strategies in areas where high parent material inheritance coincides with intensive anthropogenic inputs to mitigate potential synergistic environmental risks.

     

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