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首页> 外文期刊>Journal of geophysical research. Planets >MSL-APXS titanium observation traymeasurements: Laboratory experiments and results for the Rocknest fines at the Curiosity field site in Gale Crater, Mars
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MSL-APXS titanium observation traymeasurements: Laboratory experiments and results for the Rocknest fines at the Curiosity field site in Gale Crater, Mars

机译:MSL-APXS钛观测托盘量:在MARS Gale Crater的好奇场现场的实验室实验和摇滚罚款的结果

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摘要

The Mars Science Laboratory (MSL) rover, Curiosity, has a titanium science observation tray (o-tray), upon which portions from drilled and scooped Martian samples can be delivered for analyses by the Alpha-Particle X-ray Spectrometer (APXS). The standard APXS calibration approach to derive elemental concentrations cannot be applied to samples on the o-tray because they (1) have a nonuniform three-dimensional distribution within the APXS field of view and (2) are thin ( 90 μm). To develop techniques for interpreting MSL-APXS o-tray measurements, we conducted laboratory measurements of thin particulate basalt samples on Ti metal with the Flight Equivalent APXS Unit. The experiments demonstrate that, relative to an "infinitely thick" sample, increasing areal coverage of particulates on a Ti metal substrate results in a proportional decrease in the Ti signal and increase in the sample signal. Count rates for heavier elements (Mn and Fe) drop with decreasing sample thickness because the mean thickness is smaller than the APXS information depth. Similar effects were seen in the MSL-APXS o-tray measurement of Rocknest fines on Martian solar day 95, an aliquot of material delivered to Sample Analysis at Mars and Chemistry and Mineralogy. The thin layer effect caused a drop in Mn and Fe signals, which cannot be quantitatively compared to the in situ Rocknest target "Portage" because sample thickness was unknown. Otherwise, Rocknest fines on the o-tray had no significant compositional differences from Portage, except for slight increases in S and Cl.
机译:MARS科学实验室(MSL)Rover Culiosity具有钛科学观察托盘(O-Tray),可以通过Alpha-Particle X射线光谱仪(APXS)对钻孔和sc的火星样品进行分析。标准的APXS校准方法推导元素浓度不能应用于O-stray上的样品,因为它们(1)在APXS视图中具有不均匀的三维分布,并且(2)与(2)相比(90μm)。为了开发用于解释MSL-APXS O垫测量值的技术,我们用飞行等效的APX单元对Ti金属上的薄颗粒玄武岩样品进行了实验室测量。该实验表明,相对于“无限厚”样品,在Ti金属底物上的颗粒覆盖率增加会导致Ti信号成比例降低并增加了样品信号。较重元素的计数率(MN和FE)下降,样品厚度降低,因为平均厚度小于APXS信息深度。在火星太阳日第95天的MSL-APXS O-tray测量中也观察到了类似的影响,这是Mars,化学和矿物学的样品分析的等分试样。薄层效应导致Mn和Fe信号的下降,与原位摇滚目标“ Portage”相比,这是无法定量的,因为样品厚度未知。否则,除了S和Cl的略有增加外,O-Stray上的Rocknest罚款与Portage没有显着的组成差异。

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