首页> 外文期刊>International Journal of Coal Geology >Petrographic and geochemical characteristics of organic matter associated with stream sediments in Trail area British Columbia, Canada
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Petrographic and geochemical characteristics of organic matter associated with stream sediments in Trail area British Columbia, Canada

机译:加拿大不列颠哥伦比亚省径迹地区与河流沉积物相关的有机质的岩石学和地球化学特征

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摘要

Fifty-six samples of stream sediments from 12 creeks in the vicinity of Trail, British Columbia, Canada were examined to determine their origin, characterize their organic matter and their relation to natural/geogenic and anthropogenic sources. The samples were initially screened by Rock-Eval~R 6 pyrolysis for their TOC, HI, and OI contents and then examined by both reflected (polarized) and fluorescent light microscopy. It was found that organic matter in stream sediments is mostly from natural/biological sources from local vegetation, such as woody tissue, suberin, spores, and pollen, as well as altered natural/ biological input from char formed due to forest fires. Anthropogenic organic matter, mostly coke particles, was also found in the stream sediments. The coke particles have anisotropic properties with medium grained texture formed from medium volatile bituminous coal. The occurrence of coke particles is limited to Ryan Creek located close to an area were some small gold, nickel, and lead smelting operations previously occurred. There is no evidence to indicate that the coke particles found in the creek are emitted from the lead and zinc smelter currently in operation in the area. There are no coal-bearing strata in the area that may have a direct input of coal fragments in any of the creeks.
机译:对加拿大不列颠哥伦比亚省特洛附近的12条小溪中的56条河流沉积物样本进行了检查,以确定其起源,特征化的有机质以及它们与自然/地质和人为来源的关系。首先通过Rock-Eval〜R 6热解法筛选样品的TOC,HI和OI含量,然后通过反射(偏光)和荧光显微镜检查。研究发现,河流沉积物中的有机物主要来自当地植被的自然/生物来源,例如木质组织,木粉,孢子和花粉,以及由于森林大火而形成的木炭改变了自然/生物输入。在河流沉积物中还发现了人为的有机质,主要是焦炭颗粒。焦炭颗粒具有各向异性的特性,具有由中等挥发性的烟煤形成的中等粒度的织构。焦炭颗粒的产生仅限于Ryan Creek,该区域位于先前曾发生过一些金,镍和铅冶炼操作的区域附近。没有证据表明在该小溪中发现的焦炭颗粒是从该地区目前正在运行的铅和锌冶炼厂释放出来的。该地区没有任何含煤地层,可能在任何一条小河中都直接输入了煤屑。

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