Trace elements characterisation in floodplain soils underlain by crystalline rocks, akure, southwestern Nigeria

Asowata I.T, Omokolade O.G
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引用次数: 1

Abstract

The results of the floodplain soils study on the spatial distribution of selected trace elements in top soils (0 – 30 cm) and sub soils (> 30 – 100 cm) near Ala River, Akure metropolis, are reported. The objectives of this study are to determine the concentration of trace elements in the top and bottom soils, and identify the possible enrichment sources of these elements in the floodplain area. Forty two samples (top soil 21; sub soil 21) were collected for the study. The samples were air dried at room temperature, disaggregated and sieved using 53 µg mesh size. The prepared samples were further digested using modified aqua regia of (1:1:1 HNO3: HCL: H2O). The digests were subjected to elemental analysis using Inductively Coupled Plasma-Emission Spectrometry (ICP-MS). The trace elements concentration in ppm exhibited the following distribution pattern. Cu range in ppm from 6.0 – 53.0 mean 27.43; Pb, 10.0 – 165.0, mean 58.43; Zn, 29.0 – 479.0 mean 223.1; Ni, 10.0 – 20.0, mean 14.86; Co, 16.0 – 33.0, mean 24.29; Mn, 250.0 – 1615.0, mean 983.29; Th 9.0 – 19.0, mean 14.43; V, 35.0 – 89.0, mean 73.05; La 26.0 – 84.0, mean 56.76 and Cr 11.0 – 60.0 mean 40.43. While the result for the sub soils range in ppm, Cu from 3.0 – 51.0, mean 21.24; Pb, 7.0 – 208.0, mean 56.33; Zn, 21.0 - 460.0. mean 149.14; Ni, 8.0 – 29.0, mean 13.76; Co, 12.0 – 37.0, mean 23.95; Mn, 138.0 – 2283.0, mean 806.43; Th 9.0 – 28.0, mean 17.48; V, 40.0 – 105.0, mean 68.71; La 25.0 – 96.0, mean 61.00 and Cr 12.0 – 58.0 mean 35.38. The results of both the top soils and sub soils showed higher concentration metal enrichment than the average shale values. The relative elemental mean concentration is such that Mn> Zn > V > La > Pb > Cr > Co > Cu > Th > Ni in that order. Elements such as Cu, Zn, Pb, V, Mn, Th and Cr had relatively moderate to very strong correlation coefficient (r = 0.54 0.97) with each other, which apparently indicate that these elements are of same source of enrichment in the floodplain. Pb, Zn, V, La, Th and Cr are elements that are of significant environmental concerns.   
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尼日利亚西南部阿库尔结晶岩下漫滩土壤中的微量元素特征
报道了阿库尔市阿拉河流域洪泛区土壤中微量元素在表层(0 ~ 30 cm)和底土(> 30 ~ 100 cm)中空间分布的研究结果。本研究的目的是确定河漫滩地区表层和底层土壤中微量元素的浓度,并确定这些元素可能的富集来源。42份样品(表层土21份;收集下层土壤(21)进行研究。样品在室温下风干,用53µg的筛孔尺寸进行分解和筛选。制备的样品用改性王水(1:1:1 HNO3: HCL: H2O)进一步消化。采用电感耦合等离子体发射光谱法(ICP-MS)进行元素分析。ppm中微量元素浓度的分布规律如下:铜的ppm范围为6.0 ~ 53.0,平均值为27.43;Pb, 10.0 ~ 165.0,平均值58.43;Zn, 29.0 ~ 479.0,平均223.1;Ni, 10.0 ~ 20.0,平均14.86;Co, 16.0 - 33.0,平均24.29;Mn, 250.0 ~ 1615.0,平均983.29;平均9.0 ~ 19.0,平均14.43;V, 35.0 ~ 89.0,均值73.05;La 26.0 ~ 84.0,平均56.76;Cr 11.0 ~ 60.0,平均40.43。土壤中Cu含量在ppm ~ 51.0之间,平均值为21.24;Pb 7.0 ~ 208.0,平均值56.33;Zn, 21.0 - 460.0。意思是149.14;Ni, 8.0 - 29.0,平均13.76;Co, 12.0 - 37.0,平均23.95;Mn, 138.0 ~ 2283.0,平均806.43;平均9.0 - 28.0,平均17.48;V值40.0 ~ 105.0,均值68.71;La 25.0 ~ 96.0,平均61.00;Cr 12.0 ~ 58.0,平均35.38。表层土和底土金属富集浓度均高于页岩平均值。相对元素平均浓度为Mn> Zn > V > La > Pb > Cr > Co > Cu > Th > Ni。Cu、Zn、Pb、V、Mn、Th、Cr等元素之间具有相对中~很强的相关系数(r = 0.54 0.97),说明这些元素在洪泛平原具有相同的富集来源。Pb、Zn、V、La、Th和Cr是具有重要环境意义的元素。
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