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Magnetic signature of heavy metals pollution of sediments: case study from the East Lake in Wuhan, China

机译:沉积物重金属污染的磁特征:以武汉东湖为例

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摘要

Detailed magnetic measurements and geo-chemical analyses were performed on 114 sediment samples collected from the East Lake, Wuhan city, China, to establish a possible link between the enhanced concentration of anthropogenic magnetic particles and heavy metals with known sources. Relatively higher magnetic susceptibility values (mass-specific, x, >150 × 10~(-8) m~3 kg~(-1) were observed for samples near the pollution sources: e.g. the Wuhan Iron and Steel Company (WISC), the Qingshan Thermal Power Plant (QTPP), the banks (driveways) of the lake and near the sightseeing route of yachts on the lake. Moreover, x is positively correlated to the concentration of Pb (correlation coefficient r = 0.682), but negatively or weakly correlated with both Zn and Cu. In contrast, anhysteretic remanent magnetization (ARM) is significantly correlated with these major heavy metals (r = 0.645 for Zn-ARM, 0.699 for Pb-ARM and 0.841 for Cu-ARM, respectively), which indicate that ARMrnserves a better indicator for the pollution of heavy metals in this lake. Thermomagnetic analysis combined with magnetic hysteresis measurements revealed that magnetites in the pseudo-single-domain/multidomain grain-size regions are dominant. Scanning electron microscopy and energy dispersive X-ray examinations of the magnetic extracts showed that these Fe-rich particles have different morphologies: orange-peel structure, hollow structure with adhered smaller particles, Zr-rich melted-like irregular particles, pear-shaped spherules and spherules with slick surfaces. These features are typical for particles produced by anthropogenic activities. Because of the genetic relationship between the environmental setting of the East Lake and the nearby pollution sources, this study suggests that in situ magnetic surveys are sensitive to evaluate the environmental pollution on the lake bottom.
机译:对从中国武汉市东湖收集的114个沉积物样品进行了详细的磁测量和地球化学分析,以建立人为磁性颗粒与已知来源的重金属浓度增加之间的可能联系。在靠近污染源的样品中观察到较高的磁化率值(质量比,x,> 150×10〜(-8)m〜3 kg〜(-1):例如武汉钢铁公司(WISC),青山热电厂(QTPP),湖岸(车道)和湖上游艇观光路线附近;此外,x与Pb的浓度呈正相关(相关系数r = 0.682),而与Pb的浓度呈负相关与此相反,迟滞剩磁(ARM)与这些主要重金属显着相关(Zn-ARM分别为r = 0.645,Pb-ARM分别为0.699和Cu-ARM分别为0.841),表明ARMrns是该湖中重金属污染的更好指标,热磁分析和磁滞测量结果表明,伪单畴/多畴晶粒尺寸区域中的磁铁矿占主导地位。射线检查磁性提取物的检测表明,这些富铁颗粒具有不同的形态:橙皮结构,带有粘附的较小颗粒的空心结构,富Zr的熔融状不规则颗粒,梨形小球和表面光滑的小球。这些特征是人为活动产生的颗粒的典型特征。由于东湖的环境与附近污染源之间存在遗传关系,这项研究表明,就地磁测对评估湖底环境污染很敏感。

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