Department of Earth and Environmental Sciences, University of Texas at Arlington, Arlington, Texas 76019, United States.
Environ Sci Technol. 2012 Feb 21;46(4):2025-32. doi: 10.1021/es2023785. Epub 2012 Feb 9.
Laser ablation with inductively coupled plasma-mass spectrometry (LA-ICP-MS) was used to measure elemental concentrations at the 100-μm scale in a 3-dimensional manner within a basaltic clast sample collected from the Hanford 300 Area in south-central Washington State, United States. A calibration method was developed to quantify the LA-ICP-MS signal response using a constant-sum mass fraction of eight major elements; the method produced reasonable concentration measurements for both major and trace elements when compared to a standard basalt sample with known concentrations. 3-Dimensional maps (stacked 2-D contour layers, each representing 2100 μm × 2100 μm) show relatively uniform concentration with depth for intrinsic elements such as Si, Na, and Sr. However, U and Cu accumulation were observed near the sample surface, consistent with the site's release history of these contaminants. U and Cu show substantial heterogeneity in their concentration distributions within horizontal slices, while the intrinsic elements are essentially uniformly distributed. From these measured U concentrations and published grain size distributions, gravel and cobbles were estimated to contain about 1% of the contaminant U, implicating the coarse fraction as a long-term release source.
激光烧蚀与电感耦合等离子体质谱法(LA-ICP-MS)用于测量美国华盛顿州中南部汉福德 300 区采集的玄武质岩屑样本中元素的浓度,其在 100-μm 尺度上以三维方式进行。开发了一种校准方法,通过 8 种主要元素的恒定总和质量分数来量化 LA-ICP-MS 信号响应;与具有已知浓度的标准玄武岩样品相比,该方法可对主要和微量元素进行合理的浓度测量。3D 地图(堆叠的 2D 等高线层,每个代表 2100μm×2100μm)显示 Si、Na 和 Sr 等固有元素随深度的浓度相对均匀。然而,在样品表面附近观察到 U 和 Cu 的积累,这与该地点这些污染物的释放历史一致。U 和 Cu 的浓度分布在水平切片内存在很大的不均匀性,而固有元素则基本均匀分布。根据这些测量的 U 浓度和已发表的粒度分布,砾石和卵石估计含有约 1%的污染物 U,这表明粗粒级是长期释放源。