十年来耳石PIXE分析的价值

M. Elfman, K. Limburg, H. Svedäng, H. Wickström, M. Borysiuk, L. Ros, Naseem S. Abdel, P. Kristiansson, E. Nilsson, J. Pallon
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引用次数: 1

摘要

在过去的10年里,数千块耳石在隆德离子束分析设备(LIBAF,以前的LNMP隆德核微探针)上用pxie(使用2.55 MeV质子)进行了分析。在耳石中发现了40多种元素,其中许多元素的含量适合进行PIXE分析。从Ca开始的耳石中容易检测到的元素有:Ca(基体)、Ti、Cr、Mn、Fe、Co、Ni、Cu、Zn、As、Se、Br、Sr、Y、Zr、Mo、Cd、Sn(难)、I、Ba(有时难)、Pb(难)。在此期间使用的探测器系统比许多其他x射线探测器系统更敏感,因为它由8个HPGE探测器元件(每个100 mm2)组成,在光束入口周围形成环状结构。使用厚吸收体可以使我们使用相当高的光束电流,通常为12 nA,但有时高达20 nA。这允许我们在较短的分析时间内有较低的检测限。此外,轻稳定同位素的研究在包括生态学在内的科学领域也很广泛。氮的稳定同位素提供了有关营养水平的信息(“谁吃谁”),为绘制饮食从一种食物类型到另一种食物类型的转换提供了机会。氧同位素是有用的“环境温度计”。目前,大多数此类分析都需要破坏耳石,而氮同位素分析可能需要溶解整个耳石,从而丢失所有时间信息。我们提出了使用新型探测器的新技术,双面硅条探测器(DSSSD)。详细介绍了探测器、电子设备和实验室设置;我们的分析使用了一个MeV质子和一个LIBAF的氘微束。在PIXE分析后立即进行分析,不移动样品。
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A decade’s worth of otolith PIXE analyses
Over the past 10 years, several thousand otoliths have been analyzed with PIXE (using 2.55 MeV protons) at LIBAF (Lund Ionbeam Analysis Facility, formerly LNMP Lund Nuclear Micro Probe). Over 40 elements have been identified in otoliths, many at levels suitable for PIXE analysis. Readily detectable elements in otoliths starting with Ca are: Ca (the matrix), Ti, Cr, Mn, Fe, Co, Ni, Cu, Zn, As, Se, Br, Sr, Y, Zr, Mo, Cd, Sn (difficult), I, Ba (sometimes difficult), Pb (difficult). The detector system, used over this time period, is more sensitive than many other X-ray detector systems, since it consists of eight HPGE detector elements (100 mm2 each), in an annular formation around the beam entrance. Using a thick absorber allows us to use quite high beam current, typically 12 nA, but sometimes up to 20 nA. This permits us to have low detection limits within short analysis times. Additionally, light stable isotope research is widespread in the sciences including ecology. Stable isotopes of N provide information about trophic level (“who eats who”), providing the opportunity to map out the switching of diets from one food type to another. Oxygen isotopes are useful as “environmental thermometers”. Currently, most of such analyses require destruction of the otolith, and nitrogen isotope analysis may require dissolving entire otoliths, thus losing all temporal information. We present new techniques using new types of detectors, double side silicon strip detector (DSSSD). The detectors, electronics and the laboratory setup are described in detail; for our analysis, a MeV proton and a deuterium microbeam at LIBAF is used. The analysis is performed immediately after the PIXE analysis, without moving the sample.
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