Geochemical Investigation of Selected Elements in an Agricultural Soil: Case Study in Sumani Watershed West Sumatera in Indonesia

Aflizar, Muzakkir, R. Afrizal, Muhammad Azadur Rahman
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引用次数: 1

Abstract

This paper presents the geochemical study of agricultural soil and river sediments along Sumani watershed, West Sumatra in Indonesia. We examined the distribution and abundances of 16 elements (Pb, Zn, Cu, Ni, Cr,V, Sr, Rb, Ce, Th, Zr, Si, Ti, Fe Ca, and P) in vegetable soil, sawah soil =and river sediment sample, to evaluate the factors controlling their abundances, possible sources, and environmental implications. Average concentrations of Pb, Zn, Cu, Ni, Cr,V, Sr, Rb, Ce, Th, Zr at vegetable (1) soil were 38, 88.3, 38.7, 3, 8, 101, 96, 98, 87, 31 and 218 mg kg-1 , 26, 39.05, 8.8, 13.5, 31, 231.5, 37, 19, 78, 16 and 303.5 mg kg-1 at sawah soil (3, 4) and 30, 61.6, 35.7, 9, 22, 294, 65, 12, 78, 14 and 232 mg kg-1 at river sediment (2), respectively. The concentration of Pb, Rb, Th and Zr at upland vegetables, V and Zr at sawah soil and river sediment were mostly two time Sumatra BCSCST or BCC in several samples. Enrichment factor values showed low to moderate enrichment of Pb, Zn, Cu, Rb, Ce and Zr, whereas Th showed significant contamination at vegetables soil, suggesting contributions from anthropogenic sources. Anthropogenic contributions of most metals mainly originate from natural processes. However, Pb, Ce, Th and Zr ranges of 527–108, 41-89, 66-117 and 35-100%, respectively, at Vegetable and sawah soil and river sediment confirm their anthropogenic contribution. Factor analysis and correlation matrices suggested that elevated metal concentrations at agricultural soil in Sumani watershed might be controlled by pH, CEC, Fe-oxy-hydroxides. Deposition of metals at vegetable and sawah soil and river sediment might be controlled by non-ferrous metal (i.e., aluminosilicates), sediment grain size, or source rock composition (andesite, alluvial fan, undifferentiated volcanic material, granite and gneiss). Keyword: Agricultural soil, anthropogenic activities, enrichment factor, metals source, river sediment, watershed trace Normal 0 false false false IN X-NONE X-NONE [ How to Cite : Aflizar, Muzakkir, R Afrizal and MA Rahman. 2016. Geochemical Investigation of Selected Elements in an Agricultural Soil: Case Study in Sumani Watershed West Sumatera in Indonesia. J Trop Soils 21: 49-66. Doi: 10.5400/jts.2016.21.1.49 ]
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农业土壤中选定元素的地球化学研究——以印度尼西亚西苏门答腊苏马尼流域为例
本文介绍了印度尼西亚西苏门答腊岛苏马尼流域农业土壤和河流沉积物的地球化学研究。研究了16种元素(Pb、Zn、Cu、Ni、Cr、V、Sr、Rb、Ce、Th、Zr、Si、Ti、Fe、Ca和P)在蔬菜土壤、沙土和河流沉积物样品中的分布和丰度,以评价其丰度的控制因素、可能的来源和环境影响。蔬菜(1)土壤中Pb、Zn、Cu、Ni、Cr、V、Sr、Rb、Ce、Th、Zr的平均浓度分别为:38、88.3、38.7、3、8、101、96、98、87、31、218 mg kg-1、26、39.05、8.8、13.5、31、231.5、37、19、78、16、303.5 mg kg-1;河流底泥(2)土壤中Pb、Zn、Cu、Ni、Cr、Sr、Rb、Ce、Th、Zr的平均浓度分别为:30、61.6、35.7、9、22、294、65、12、78、14、232 mg kg-1。旱地蔬菜中Pb、Rb、Th和Zr的浓度,沙瓦土壤和河流沉积物中V和Zr的浓度,多数为两次苏门答腊BCSCST或BCC。富集因子值显示,蔬菜土壤中Pb、Zn、Cu、Rb、Ce和Zr的富集程度为低至中等,而Th的污染程度较重,提示存在人为污染。大多数金属的人为贡献主要来自自然过程。然而,蔬菜和沙华土壤和河流沉积物的Pb、Ce、Th和Zr分别为527 ~ 108、41 ~ 89、66 ~ 117和35 ~ 100%,证实了它们的人为贡献。因子分析和相关矩阵分析表明,苏马尼流域农业土壤中金属浓度升高可能受pH、CEC、铁氧氢氧化物的控制。蔬菜和沙瓦土壤和河流沉积物中的金属沉积可能受有色金属(即铝硅酸盐)、沉积物粒度或烃源岩成分(安山岩、冲积扇、未分异火山物质、花岗岩和片麻岩)的控制。关键词:农业土壤,人为活动,富集因子,金属来源,河流沉积物,流域痕量正常0 false false false IN X-NONE X-NONE[如何引用:Aflizar, Muzakkir, R Afrizal和MA Rahman。2016。]农业土壤中选定元素的地球化学研究——以印度尼西亚西苏门答腊苏马尼流域为例。[J]热带土壤学报,21(2):49-66。[Doi: 10.5400/jts.2016.21.1.49]
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