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Magnetic properties of street dust and topsoil in Beijing and its environmental implications

机译:北京街道尘土和表层土壤的磁学性质及其环境意义

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Environmental magnetic measurements were carried out on the samples of street dust and topsoil, which were collected along the roadway in the urban and suburb of Beijing, including magnetic susceptibility (chi), anhysteretic remanent magnetization (ARM), isothermal remanent magnetization (IRM) of all samples and temperature-dependence of magnetic susceptibilities and magnetic hysteresis parameters of representative samples. Obvious differences exist between the samples of street dust and those of topsoil. Compared with topsoil samples, the concentration of magnetic particles and high-coercivity components in street dust samples are higher, and the magnetic grains are coarser. Both dust and topsoil samples are dominated by ferrimagnetic minerals, and iron particles are only detected in some dust samples. These results suggest that street dust samples reflect the characteristic of particles produced by industrial and traffic activities, and the magnetic property of topsoil samples represents the characteristic of particles from both anthropogenic and natural sources. The distribution of magnetic parameters is influenced by the environment where the samples are collected, like industry, traffic density and other road conditions. Hard isothermal remanent magnetization (HIRM) may be used as an indicator of particles produced by traffic activity. Dust storm samples collected on 17 and 18 April, 2006 have different magnetic properties from street dust and natural particles, like loess and paleosol, which indicate that the dust storm might be mixed with anthropogenic particulates during transport and falling.
机译:对北京市区和郊区沿道路收集的街道灰尘和表土样品进行了环境磁测量,包括磁化率(chi),磁滞剩磁(ARM),等温剩磁(IRM)。所有样品以及代表性样品的磁化率和磁滞参数的温度依赖性。街道灰尘样品和表土样品之间存在明显差异。与表土样品相比,街道粉尘样品中的磁性颗粒和高矫顽力成分浓度更高,并且磁性颗粒更粗。尘土和表土样品均以亚铁磁性矿物为主,仅在某些尘土样品中检测到铁颗粒。这些结果表明,街道尘土样品反映了工业和交通活动产生的颗粒的特征,表土样品的磁性代表了人为和自然来源的颗粒的特征。磁参数的分布受样本收集环境的影响,例如工业,交通密度和其他道路条件。硬等温剩余磁化强度(HIRM)可以用作交通活动产生的颗粒的指示剂。 2006年4月17日至18日收集的沙尘暴样品具有不同于街道尘埃和天然颗粒(如黄土和古土壤)的磁性,这表明沙尘暴可能在运输和坠落过程中与人为颗粒混合。

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