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Bulk hydrogen abundances in the lunar highlands: Measurements from orbital neutron data

机译:月球高地上的大量氢丰度:来自轨道中子数据的测量

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The first map of bulk hydrogen concentrations in the lunar highlands region is reported. This map is derived using data from the Lunar Prospector Neutron Spectrometer (LP-NS). We resolve prior ambiguities in the interpretation of LP-NS data with respect to non-polar hydrogen concentrations by comparing the LP-NS data with maps of the 750 nm albedo reflectance, optical maturity, and the wavelength position of the thermal infrared Christiansen Feature. The best explanation for the variations of LP-NS epithermal neutron data in the lunar highlands is variable amounts of solar-wind-implanted hydrogen. The average hydrogen concentration across the lunar highlands and away from the lunar poles is 65 ppm. The highest hydrogen values range from 120 ppm to just over 150 ppm. These values are consistent with the range of hydrogen concentrations from soils and regolith breccias at the Apollo 16 highlands landing site. Based on a moderate-to-strong correlation of epithermal neutrons and orbit-based measures of surface maturity, the map of highlands hydrogen concentration represents a new global maturity index that can be used for studies of the lunar soil maturation process. We interpret these hydrogen concentrations to represent a bulk soil property related to the long-term impact of the space environment on the lunar surface. Consequently, the derived hydrogen concentrations are not likely related to the surficial enhancements (top tens to hundreds of microns) or local time variations of OH/H2O measured with spectral reflectance data. (c) 2015 The Authors. Published by Elsevier Inc.
机译:据报道,在月球高地地区,氢原子浓度的第一张图。该图是使用Lunar Prospector中子光谱仪(LP-NS)的数据得出的。通过将LP-NS数据与750 nm反照率反射率,光学成熟度和热红外Christiansen Feature的波长位置的图进行比较,我们解决了关于非极性氢浓度的LP-NS数据解释中的先前歧义。登月高地LP-NS超热中子数据变化的最好解释是太阳风注入氢的数量可变。穿过月球高地和远离月球极的平均氢浓度为65 ppm。最高氢值范围从120 ppm到刚好超过150 ppm。这些值与阿波罗16号高地着陆点土壤和and石角砾岩中的氢浓度范围一致。基于超热中子的中到强相关性以及基于轨道的表面成熟度测量,高地氢浓度图代表了一种新的全球成熟度指数,可用于研究月球土壤成熟过程。我们将这些氢浓度解释为代表与空间环境对月球表面的长期影响有关的整体土壤性质。因此,得出的氢浓度可能与光谱反射率数据测得的表面增强(数十至数百微米)或OH / H2O的局部时间变化无关​​。 (c)2015作者。由Elsevier Inc.发布

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