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Composition and spatial distribution of elements and isotopes of a giant human bladder stone and environmental implications

机译:巨型人膀胱结石的元素和同位素的组成,空间分布以及对环境的影响

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The composition and spatial distribution of minerals, trace elements, as well as carbon and nitrogen isotopes from the outer crust to inner nucleus of a 20-year old giant human bladder stone comprising thirteen layers were intensively investigated. Calcium oxalate monohydrate (COM) was found to concentrate in the inner and middle layers, struvite was concentrated in middle and outer layers, and fluorapatite occurred in almost all layers. The spatial distribution of minerals has the potential to provide preliminary knowledge regarding the long-term urine composition, or even the physiological condition of the patient. The stable carbon isotope ratio (delta C-13) and stable nitrogen isotope ratio (delta N-15) were measured in each layer and significant correlation was found between delta C-13 with calcium oxalate monohydrate content and between delta N-15 and struvite content. Nearly constant values of -23.2% and 7.1% for delta C-13 and delta N-15, respectively, were found in the organic components of the stone. Both isotope ratios indicate a long-term fixed diet consisting mainly of C3 plants, such as rice and wheat, for the 20-year time period of the stone formation. In addition, eighteen elements (Ca, P, Mg, K, Na, Al, Fe, Zn, Pb, Cu, Sr, Ba, Ti, V, Cr, Ni, Mn and Co) were measured in all the layers. The trace elements Al, Fe, Cu, Zn, Pb, Sr, Ba and Ti showed a similar spatial distribution pattern from the outer crust to the inner core. Although there were complex correlations between elements and minerals, Factor Analysis suggests that the occurrence of these elements in stones may be mainly the result of environmental exposure to metals during the formation of the stone, indicating that urinary stones may serve as potential long-term biomonitors. In particular, Ni and Cr showed a distinct distribution pattern in the stone, which may relate to human metabolic activities. (C) 2018 Elsevier B.V. All rights reserved.
机译:深入研究了20年之久的十三层巨人膀胱结石从外壳到内核的矿物,微量元素以及碳氮同位素的组成和空间分布。发现草酸钙一水合物(COM)集中在内层和中间层,鸟粪石集中在中层和外层,并且氟磷灰石几乎在所有层中都发生。矿物质的空间分布有可能提供有关长期尿液成分甚至患者生理状况的初步知识。在每一层中测量了稳定的碳同位素比(δC-13)和稳定的氮同位素比(δN-15),发现δC-13与草酸钙一水合物含量之间以及δN-15和鸟粪石之间存在显着相关性。内容。在石材的有机成分中,δC-13和δN-15的几乎恒定值分别为-23.2%和7.1%。两种同位素的比率都表明在结石形成的20年时间内,长期固定饮食主要由C3植物(例如水稻和小麦)组成。另外,在所有层中测量了18种元素(Ca,P,Mg,K,Na,Al,Fe,Zn,Pb,Cu,Sr,Ba,Ti,V,Cr,Ni,Mn和Co)。微量元素Al,Fe,Cu,Zn,Pb,Sr,Ba和Ti从外壳到内芯显示出相似的空间分布模式。尽管元素和矿物质之间存在复杂的关联,但是因子分析表明,这些元素在结石中的发生可能主要是结石形成过程中环境暴露于金属的结果,这表明尿结石可能是潜在的长期生物监测器。尤其是,镍和铬在石头中显示出明显的分布模式,这可能与人类的代谢活动有关。 (C)2018 Elsevier B.V.保留所有权利。

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