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Geochemical study of products associated with spontaneous oxidation of coal in the Cerro Pelado Formation, Venezuela

机译:委内瑞拉塞罗佩拉多组煤自发氧化产物的地球化学研究

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摘要

The aim of this research work is a geochemical, mineralogical, and textural characterization of spontaneously smouldered coal-derived products in northwestern Venezuela (Cerro Pelado Formation, some 10 km from Pedregal city). Several solid samples were collected from this formation, six of unweathering coal, an other six of resulting unmelted rocks forming on a surface coal bed, and the last four of mineralizations found accumulating around gas vents. The fresh coal and the unmelted material were analysed by scanning electron microscopy, X-ray diffraction, and proximate techniques. Products such as magnetite and chabazite-K were identified in the alteration rocks. Likewise, both materials were also studied in order to determine the mobilization of 17 elements into the environment; such elements were analysed through inductively coupled plasma atomic emission spectroscopy on extracts obtained by a sequential extraction method: each sample was firstly extracted with MilliQ water and then the resultant residue was washed. This and the subsequently resulting residues are extracted according to the mentioned procedure by using, respectively, ammonium acetate, chlorhydric acid, peroxide and chlorhydric acid, nitric acid and fluorhydric acid, and nitric acid. The studied elements are classified as highly mobile (Na, Ni,...), nearly immobile (Ti, P) and partially mobile (Mg, Fe, K,...). In regards to mineralizations around fumaroles associated with smoldering coal seams, Fourier-transform infrared spectroscopy and X-ray diffraction analyses have revealed the presence of salammoniac, mascagnite and other solid combustion compounds formed by reaction of gas emitted from coal oxidation, in addition to previously non-reported sulfur-rich by-products associated with gas fissures, particularly ammonium thiosulfate, a phase first obtained only synthetically in the laboratory. Another objective of the research was to collect and analyse gases escaping from surficial vents. Relatively high concentrations of several aromatic compounds were detected in the gas collected at the studied coal outcrop, as well as aliphatic hydrocarbons including ethane, propane, butanes, among others. High contents of carbon monoxide, methane and carbon dioxide were also measured for gas samples.
机译:这项研究工作的目的是对委内瑞拉西北部(塞罗佩拉多组,距佩德雷加尔市约10公里)的自燃煤粉衍生产品进行地球化学,矿物学和质地表征。从该地层中收集了几个固体样品,其中六个是未风化的煤,另外六个是在地表煤层上形成的未融化岩石,最后四个矿化物聚集在排气孔附近。通过扫描电子显微镜,X射线衍射和近距离技术分析了新鲜煤和未熔化的材料。在蚀变岩中发现了磁铁矿和菱沸石-K等产品。同样,还对两种材料进行了研究,以确定将17种元素迁移到环境中的情况。通过电感耦合等离子体原子发射光谱法对通过顺序萃取方法获得的萃取物进行分析:首先用MilliQ水萃取每个样品,然后洗涤所得残留物。根据上述方法,分别通过使用乙酸铵,盐酸,过氧化物和盐酸,硝酸和氟酸以及硝酸来萃取该残余物和随后得到的残余物。所研究的元素分为高迁移率(Na,Ni,...),几乎不迁移(Ti,P)和部分迁移(Mg,Fe,K ...)。关于与闷燃煤层有关的富马酚周围的矿化作用,傅立叶变换红外光谱和X射线衍射分析表明,除了煤氧化作用之外,还存在着由煤氧化产生的气体反应而形成的草,辉石和其他固体燃烧化合物。未报告的与气体裂缝有关的富硫副产物,特别是硫代硫酸铵,该相最初仅在实验室中通过合成获得。该研究的另一个目的是收集和分析从地表通风孔逸出的气体。在研究的煤层露头收集的气体中,以及包括乙烷,丙烷,丁烷等在内的脂肪烃中,检出了相对较高浓度的几种芳族化合物。还测量了气体样品中一氧化碳,甲烷和二氧化碳的含量。

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