SERPENTINITE-WATER INTERACTION AND CHROMIUM(VI) RELEASE IN SPRING WATERS: EXAMPLES FROM TUSCAN OPHIOLITES

IF 1.2 4区 地球科学 Q2 GEOLOGY
A. Langone, I. Baneschi, C. Boschi, A. Dini, M. Guidi, A. Cavallo
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引用次数: 10

Abstract

Since 2006 the Regional Environmental Agency (ARPA) of Tuscany has found Cr(VI) concentration in groundwater above the maximum acceptable con- centration (5 ppb) according to the Italian regulation (D.M. 25 October 1999, n. 471). Recently, hydrogeological investigations (Grassi, 2009) confirmed high total Cr and Cr(VI) contents in soils and waters related to ultramafic rocks from coastal Tuscany. To study the release of Cr(VI) to water from geogenic sources we examined the spring waters, soils and bedrocks compositions within two serpentinized bodies of the coastal Tuscany, namely Santa Luce and Querceto. These selected sites are characterized by Cr(VI)-free and Cr(VI)-bearing spring waters, respec- tively. The prevalence of Mg-HCO3 waters at these sites indicates that waters are primarily interacting with serpentinites. Samples from Querceto are enriched in Mg suggesting the leaching of brucite. Soil profiles and bedrocks were analysed for major and trace elements by XRF to assess the fate of Cr during weather- ing. Detailed petrographic and chemical analyses of both soil and rock samples revealed that Cr is mainly hosted within chromites. Chemical data and alteration features indicate a metasomatism coeval to the oceanic serpentinization leading to a Mn-enrichment of the alteration products of primary spinel. The co-occur- rence of Mn-bearing and Fe-rich oxides with Cr-rich spinels creates a chemical system potentially able to promote the Cr(III) to Cr(VI) oxidation. However, the occurrence of Mn-rich minerals seems to be not correlated to the oxidation state of chromium in the spring waters. In fact, they are ubiquitous in both the study localities, while Cr(VI) has been detected only at Querceto. Unlike Santa Luce, serpentinites from Querceto contain a significant amount of Fe-rich brucite and show evidence for ongoing brucite dissolution coupled with precipitation of hydromagnesite crusts and veinlets. Formation of complex hydroxy-carbonate min- erals could be an alternative way for producing the proper environment for oxidative leaching of chromium from serpentinites to spring waters.
泉水中的蛇纹岩-水相互作用和铬(vi)释放:来自托斯卡纳蛇绿岩的例子
自2006年以来,托斯卡纳地区环境局(ARPA)发现地下水中的铬(VI)浓度超过了意大利法规(1999年10月25日D.M.,第471号)规定的最大可接受浓度(5 ppb)。最近,水文地质调查(Grassi, 2009)证实,在托斯卡纳沿海的超镁铁质岩石相关的土壤和水中,总铬和铬(VI)含量很高。为了研究从地质来源中释放到水中的Cr(VI),我们检查了托斯卡纳沿海的两个蛇纹岩体(即圣卢斯和Querceto)的泉水、土壤和基岩成分。这些选定的地点分别具有不含Cr(VI)和含Cr(VI)的泉水的特征。这些地点普遍存在Mg-HCO3水,表明水主要与蛇纹岩相互作用。Querceto样品富含镁,提示水镁石的浸出。用XRF分析了土壤剖面和基岩的主微量元素,以评价Cr在风化过程中的去向。土壤和岩石样品的详细岩石学和化学分析表明,铬主要赋存于铬铁矿中。化学资料和蚀变特征表明,原尖晶石的蚀变产物与海洋蛇纹石作用同时发生交代作用,使其富锰。富锰和富铁氧化物与富Cr尖晶石的共生形成了一个化学体系,有可能促进Cr(III)氧化为Cr(VI)。然而,富锰矿物的出现似乎与泉水中铬的氧化状态无关。事实上,它们在两个研究地点都普遍存在,而Cr(VI)仅在Querceto被检测到。与Santa Luce不同,来自Querceto的蛇纹岩含有大量富铁的水镁石,并且有证据表明水镁石的溶解伴随着氢菱镁矿结壳和细脉的沉淀。复合羟基碳酸盐矿物的形成可能是为蛇纹石铬氧化浸出到泉水中创造适宜环境的一种替代方法。
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来源期刊
Ofioliti
Ofioliti 地学-地质学
CiteScore
2.40
自引率
7.70%
发文量
1
期刊介绍: Since 1976, Ofioliti provides an international forum for original contributions and reviews in the field of the geodynamics, petrology, geochemistry, biostratigraphy, stratigraphy, tectonics and paleogeography applied to ophiolitic terrains and modern oceanic lithosphere, including their sedimentary cover. Studies of topics such as geodynamics of the mantle, the evolution of orogens including ophiolites and paleoceanography are also welcome
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