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

机译:皮革厂废物污染地区的地球物理和物理化学研究:来自巴西南部的案例研究

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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:牛皮革鞣制过程中会产生多种废物,由于它们的高有机负荷,它们会消耗河道中的溶解氧。本研究的范围是通过电阻率(ER)和感应极化(IP)的地球物理方法对浅层地下进行调查,并对巴西南部制革业所在的地区的水样进行理化分析。该部门使用的主要元素是铬(Cr),该元素的浓度和迁移率与其形态有关。为了获得地球物理数据,在六个调查层(大约等于15 m的深度)上以偶极-偶极阵列(AB = MN = 10 m)执行了12条电阻率测量线。地球物理结果以二维和三维模型表示,该模型通过低电阻率(<50Ωm)来表征污染物羽流,而电阻率主要与低充电率(<3 mV / V)相符,而升高的指数(> 50Ωm和> 3 mV / V),这被解释为碎屑岩和下层未污染的砂岩。这些模型可以估算污染物羽流的尺寸(50 x 60 m和7 m深),并确定其流向优先位于下游。一些分析的理化参数,例如铬,铁和氨氮浓度;生化和化学需氧量;和电导率(sigma)超过了巴西参考文献所建议的最大值或浓度。六价铬的出现似乎与弱酸性和氧化性环境有关。结果表明,受污染区域仅限于污染源附近。使用这种方法的研究可能有助于环境管理。

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