IMPACT OF POLLUTION ON THE CLAY MINERALOGICAL COMPOSITION OF SOME SOILS FROM ZLATNA AREA (ROMANIA)

C. Crǎciun, A. Manea, Laura Paulette, M. Eftene, V. Mocanu, Environment Protection-Bucharest
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Abstract

Zlatna area is a high polluted zone with heavy metals due to industrial activity (extraction and processing of non-ferrous area). In spite of the fact that industrial activity was stoped for 2-3 years, the effect of pollution are still obvious. The aim of this paper is to make evident some aspects concerning the impact of pollution on the mineralogical composition of the clay fraction (below 2µ) from some soils belonging to dystric cambisol and luvisol type. From the chemical point of view, the effect of pollution is the acidifiation and depletion of bases, reflected by the decrease of values of indices which express soil reaction (pH) and soil exchange properties, especially in the surface horizon. From mineralogical point of view, the acidifiation determines a strong alteration of primary minerals (micas and feldspars) and just of secondary minerals (illite), evolution beeing towards hydroxy interlayered minerals (intergrade) and kaolinite. As result of this alteration the content of kaolinite increases, achiving a double content in the surface horizon of some polluted soils. Sometimes kaolinite becomes the dominant mineral in the clay fraction of some strong polluted soil.
污染对罗马尼亚兹拉特纳地区部分土壤粘土矿物组成的影响
由于工业活动(有色金属地区的开采和加工),Zlatna地区是重金属高污染地区。尽管工业活动停止了2-3年,但污染的影响仍然很明显。本文的目的是明确污染对某些属于难塑cambisol和luvisol类型的土壤的粘土组分(低于2µ)的矿物学组成的影响。从化学角度看,污染的影响是碱基的酸化和耗竭,表现为土壤反应性指数(pH)和土壤交换性指数的下降,特别是在地表水平层。从矿物学的角度来看,酸化决定了原生矿物(云母和长石)和次生矿物(伊利石)的强烈蚀变,向羟基层间矿物(间级)和高岭石演化。由于这种变化,高岭石的含量增加,在一些受污染的土壤的表层层中达到双重含量。有时高岭石成为某些强污染土壤粘土组分中的主要矿物。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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