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Geophysical and physicochemical investigations of an area contaminated by tannery waste: a case study from southern Brazil

机译:制革废弃物污染的区域的地球物理和物理化学研究 - 以巴西南部的一个案例研究

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The process of tanning bovine leather produces several types of waste that, due to their high organic load, can deplete the dissolved oxygen in watercourses. The scope of this study is the investigation of the shallow subsurface by geophysical methods of electrical resistivity (ER) and induced polarization (IP) and physicochemical analyses of water samples in an area in southern Brazil in which a tannery industry is located. The main element used in this sector is chromium (Cr), and the concentration and mobility of this element are related to its speciation. To obtain the geophysical data, 12 resistivity survey lines were performed in a dipole-dipole array (AB = MN = 10 m) at six investigation levels ( approximately equal to 15 m deep). The geophysical results were represented in two- and three-dimensional models that characterized the contaminant plume by low resistivities ( 50 omega m) that coincide predominantly with low chargeabilities ( 3 mV/V) in contrast to elevated indices ( 50 omega m and 3 mV/V), which were interpreted as regoliths and underlying uncontaminated sandstones. The models made it possible to estimate the dimensions of the contaminant plume (50 x 60 m and 7 m deep) and to determine that its flow direction was preferentially downstream. Some of the analyzed physicochemical parameters, such as chromium, iron, and ammoniacal nitrogen concentrations; biochemical and chemical oxygen demand; and conductivity (sigma), exceeded the maximum values or concentrations recommended by Brazilian references. The occurrence of hexavalent chromium seems to be associated with slightly acidic and oxidizing environments. The results suggest that the contaminated area is restricted to the area near the pollution source. Studies using this approach could contribute to environmental management.
机译:鞣牛皮革的过程产生了几种类型的废物,由于它们的高有机载荷,可以在水道中耗尽溶解的氧气。本研究的范围是通过电阻率(ER)的地球物理方法对浅层地下进行调查,并诱导南巴西南部地区水样的偏振(IP)和物理化学分析,其中制革业位于其中。该扇区中使用的主要元件是铬(Cr),并且该元素的浓度和迁移率与其物种有关。为了获得地球物理数据,在六次调查水平下在偶极子 - 偶极子阵列(AB = Mn = 10m)中进行12个电阻率测量线(大约等于15米)。地球物理结果以二维和三维模型表示,其用低电阻率(<50ωM)的污染羽流,其与升高的指数相比主要是低电平的(<3 mV / v)(> 50 omega m和> 3 mV / v),被解释为凝固性和底层未受污染的砂岩。该模型使得可以估计污染物羽流(50×60m和7m深)的尺寸,并确定其流动方向优先下游。一些分析的物理化学参数,如铬,铁和氨氮浓度;生物化学和化学需氧量;和电导率(Sigma)超过巴西参考文献推荐的最大值或浓度。六价铬的发生似乎与微酸性和氧化环境有关。结果表明,污染区域仅限于污染源附近的区域。使用这种方法的研究可能有助于环境管理。

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