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Challenges in the Search for Perchlorate and Other Hydrated Minerals With 2.1-μm Absorptions on Mars

机译:在火星上寻找2.1μm吸收的高氯酸盐和其他水合矿物质的挑战

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摘要

A previously unidentified artifact has been found in Compact Reconnaissance Imaging Spectrometer for Mars targeted I/F data. It exists in a small fraction (<0.05%) of pixels within 90% of images investigated and occurs in regions of high spectral/spatial variance. This artifact mimics real mineral absorptions in width and depth and occurs most often at 1.9 and 2.1 μm, thus interfering in the search for some mineral phases, including alunite, kieserite, serpentine, and perchlorate. A filtering step in the data processing pipeline, between radiance and I/F versions of the data, convolves narrow artifacts (“spikes”) with real atmospheric absorptions in these wavelength regions to create spurious absorption-like features. The majority of previous orbital detections of alunite, kieserite, and serpentine we investigated can be confirmed using radiance and raw data, but few to none of the perchlorate detections reported in published literature remain robust over the 1.0- to 2.65-μm wavelength range.Plain Language SummaryMany minerals can be identified with remote sensing data by their characteristic absorptions in visible-shortwave infrared data. This type of data has allowed geological interpretation of much of Mars’ surface, using satellite-based observation. We have discovered an issue with the Compact Reconnaissance Imaging Spectrometer for Mars instrument’s data processing pipeline. In ~ <0.05% of pixels in almost all images, noise in the data is smoothed in such a way that it mimics real mineral absorptions, falsely making it look as though certain minerals are present on Mars’ surface. The vast majority of previously identified minerals are still confirmed after accounting for the artifact, but some to all perchlorate detections and a few serpentine detections were not confirmed, suggesting that the artifact created false detections. This means concentrated regions of perchlorate may not occur on Mars and so may not be available to generate possibly habitable salty liquid water at very cold temperatures.
机译:在紧凑侦察成像光谱仪中发现了先前未知的伪像,用于火星目标I / F数据。它存在于所研究图像的90%内的一小部分像素(<0.05%)中,并且发生在光谱/空间差异较大的区域。该伪像模仿了实际矿物在宽度和深度上的吸收,并且最常见于1.9和2.1μm,因此干扰了对某些矿物相的搜索,包括亚铝酸盐,钾铁矿,蛇纹石和高氯酸盐。在数据的辐射度和I / F版本之间,数据处理管道中的滤波步骤将狭窄的伪像(“尖峰”)与这些波长区域中的实际大气吸收进行卷积,以创建类似于虚假吸收的特征。我们以前研究过的亚矾石,钾铁矿和蛇纹石的大部分在轨探测都可以通过辐射和原始数据得到证实,但是在1.0-2.65μm的波长范围内,已发表的文献中报道的高氯酸盐检测很少甚至没有。语言摘要许多矿物可以通过其在可见-短波红外数据中的特征吸收来通过遥感数据进行识别。这种类型的数据允许使用基于卫星的观测对火星大部分表面进行地质解释。我们发现了用于火星仪器数据处理管道的紧凑侦察成像光谱仪存在问题。在几乎所有图像中,像素的0.05%像素中,噪声被平滑化,从而模仿了真实的矿物质吸收,从而错误地使其看起来像火星表面上存在某些矿物质。扣除伪影后,仍可确认绝大多数先前鉴定出的矿物,但某些高氯酸盐检测和一些蛇纹石检测均未确认,这表明伪影造成了虚假检测。这意味着高氯酸盐的浓缩区域可能不会在火星上出现,因此在非常冷的温度下可能无法生成可能适居的咸性液态水。

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