Major elements and Mg# of the Moon: Results from Chang’E-1 Interference Imaging Spectrometer (IIM) data

2012 ◽  
Vol 93 ◽  
pp. 214-234 ◽  
Author(s):  
Yunzhao Wu
2020 ◽  
Vol 12 (22) ◽  
pp. 3676
Author(s):  
Xuesen Xu ◽  
Jianjun Liu ◽  
Dawei Liu ◽  
Bin Liu ◽  
Rong Shu

The main objective of this study is to develop a Hapke photometric model that is suited for Chang’E-1 (CE-1) Interference Imaging Spectrometer (IIM) data. We first divided the moon into three areas including ‘maria’, ‘new highland’ and old ‘highland’ with similar photometry characteristic based on the Hapke parameters of the moon derived from Lunar Reconnaissance Orbiter Camera (LROC) Wide Angle Camera (WAC) multispectral data. Then, we selected the sample data in the ‘maria’ area and obtained a new set of Hapke model’s parameters that can best fit these data. Result shows that photometric correction using Hapke model with these new derived parameters can eliminate the effect of variations in viewing and luminating geometry, especially ‘opposition surge’, more efficiently than the empirical model. The corrected mosaic shows no significant artifacts along the tile boundaries and more detailed information of the image can be exhibited due to a better correction of ‘opposition surge’ at small phase angle (g < 15°).


2020 ◽  
Author(s):  
Audrey Vorburger ◽  
Peter Wurz ◽  
Manuel Scherf ◽  
Helmut Lammer ◽  
André Galli ◽  
...  

&lt;p&gt;The Moon is one of the best characterized objects in space science, yet its origin still actively researched. Available orbital, geophysical, and geochemical information imposes clear restrictions on the origin and evolution of the Earth-Moon system (e.g., Canup 2008, 2012; &amp;#262;uk and Stewart 2012; Young et al. 2016). In regard to geochemical constraints, one of the most puzzling conundrums is posed by the similar isotopic fingerprints of the Earth and the Moon (e.g., Wiechert et al. 2001; Armytage et al. 2012; Zhang et al. 2012; Young et al. 2016; Schiller et al. 2018), together with the apparent lunar depletion in volatile elements (e.g., Ringwood and Kesson 1977; Wanke et al. 1977; Albar&amp;#232;de et al. 2015; Taylor 2014). This apparent lunar volatile depletion is most notable in the low K content in comparison to U, a finding based on chemical analyses of samples collected from the lunar surface and lunar meteorites, and on spectroscopic observations of the lunar near-surface, despite both having been heavily processed in the past ~ 4.4 billion years.&lt;/p&gt;&lt;p&gt;In the past 4.4 billion years, space has been a harsh environment for our Moon, especially in the beginning, when the young Sun was still very active and the young Moon was continuously bombarded by meteorites of varying sizes. Solar wind and micro-meteoritic interactions with the lunar surface led to rapid and intensive processing of the lunar crust. Hence, the K/U depletion trend observable on today's lunar surface does not necessarily reflect a K/U ratio valid for the Moon in its entirety. We model the evolution of the abundances of the major elements over the past 4.3 to 4.4 billion years to derive the composition of the original lunar crust. Accounting for this processing, our model results show that the original crust is much less depleted in volatiles than the surface observable today, exhibiting a K/U ratio compatible with Earth and the other terrestrial planets, which strengthens the theory of a terrestrial origin for the Moon.&lt;/p&gt;


1993 ◽  
Vol 46 (6) ◽  
pp. 278-284 ◽  
Author(s):  
Lajpat R. Utreja

As one of the key elements of the Space Exploration Initiative, the Moon provides a waypoint for scientific exploration and travel to Mars. The Moon’s stable ground in the vacuum of space is an ideal platform for astronomical observatories. Conditions on the Moon are similar to what human beings will face on other planets, so it is a natural test bed to prepare for a manned mission to Mars. A knowledge of the lunar environment is therefore important before undertaking any missions of construction, operations, and habitation on the lunar surface. The purpose of this paper is to review and assemble information on the lunar environment so that engineers and scientists can refer to this as they begin lunar-based engineering studies. The lunar environment is categorized into three major elements: lunar physical constants, lunar atmosphere, and lunar surface. The description of lunar size, orientation, period of rotation, and lunar month are all treated as part of lunar physical constants. Lunar atmosphere includes gas composition, pressure and density, solar flux and radiation, micrometeorite flux, and lunar dust. The geophysical and geochemical properties are provided as lunar surface characteristics. The geophysical properties include terrain characteristics, topography and surface tremors; soil and rock characteristics; mechanical, thermal, electrical, magnetic, and optical properties. The chemical composition of the regolith and rocks are described in geochemical properties.


2021 ◽  
Vol 13 (12) ◽  
pp. 2359
Author(s):  
Jiafei Xu ◽  
Meizhu Wang ◽  
Rong Wang ◽  
Qi Feng ◽  
Honglei Lin ◽  
...  

In-situ measurements of the spectral information on the lunar surface are of significance to study the geological evolution of the Moon. China’s Chang’E-4 (CE-4) Yutu-2 rover has conducted several in-situ spectral explorations on the Moon. The visible and near-infrared imaging spectrometer (VNIS) onboard the rover has acquired a series of in-situ spectra of the regolith at the landing site. In general, the mineralogical research of the lunar surface relies on the accuracy of the in-situ data. However, the spectral measurements of the Yutu-2 rover may be affected by shadows and stray illumination. In this study, we analyzed 106 CE-4 VNIS spectra acquired in the first 24 lunar days of the mission and noted that six of these spectra were affected by the shadows of the rover. Therefore, a method was established to correct the effects of the rover shadow on the spectral measurements. After shadow correction, the FeO content in the affected area is corrected to 14.46 wt.%, which was similar to the result calculated in the normal regolith. Furthermore, according to the visible images, certain areas of the explored sites were noted to be unusually bright. Considering the reflectance, geometric information, and shining patterns of the multi-layer insulation (MLI), we examined the influence of the specular reflection of the MLI on the bright spot regionsd , and found that the five sets of data were likely not affected by the specular reflection of the MLI. The results indicated that the complex illumination considerably influences the in situ spectral data. This study can provide a basis to analyze the VNIS scientific data and help enhance the accuracy of interpretation of the composition at CE-4 landing sites.


Author(s):  
Chunlai Li ◽  
Zhendong Wang ◽  
Rui Xu ◽  
Gang Lv ◽  
Liyin Yuan ◽  
...  

The Chang&rsquo;e-4 (CE-4) lunar rover, equipped with The Visible and Near-IR Imaging Spectrometer(VNIS) which based on acousto-optic tunable filter spectroscopy, was launched to the far side of the moon on December 8, 2018. The detection band of VNIS ranges from 0.45 to 2.4&mu;m. Because of the weak reflection of infrared radiation from the lunar surface, a static electronic phase-locked acquisition method is adopted in the infrared channel for signal amplification. In this paper, full-link simulations and modeling are conducted of the infrared channel information flow of the instrument. The signal/noise characteristics of VNIS are analyzed in depth, and the signal-to-noise(SNR) ratio prediction and laboratory verification are presented. On January 4, 2019, the VNIS started working successfully and acquired high-resolution spectrum data of the far side of the moon for the first time. Through analysis, the SNR ratio is in line with predictions, and the data obtained by VNIS in orbit are consistent with the information model proposed in this paper.


2008 ◽  
Author(s):  
Paul D. LeVan ◽  
Brian P. Beecken ◽  
Cory Lindh

Author(s):  
T. Yu ◽  
Z. Liu ◽  
Z. Rong ◽  
Y. Wang ◽  
J. Wang ◽  
...  

Abstract. The Chang'e-4 successfully landed on the far side of the moon in January 2019. By the 12th lunar day, its Yutu-2 rover had achieved a breakthrough travel distance of greater than 300 m. A visible and near-infrared imaging spectrometer (VNIS), consisting of a visible and near-infrared (VNIR) imaging spectrometer and a shortwave infrared (SWIR) spectrometer was used for detecting mineralogical compositions of lunar-surface materials. Because VNIS is fixed on the front of the rover, and the field-of-view (FOV) of VNIR and SWIR are small (8.5° and 3.6° respectively), approaching and accurately pointing at the specific science target depend completely on the precise control of the moving rover.In this paper, a successful method of VNIS target detection based on vision measurement is proposed. First, the accurate position of the target is calculated via navigation camera imaging. Then, the moving path is planned by considering the terrain environment, illumination, communication condition, and other constraints. After the rover moves to the designed position, the binocular imaging of the hazard-avoidance cameras are activated, the detection direction and forward distance are calculated according to the images, and the FOV trajectory of the VINS is predicted while moving. Finally, by choosing the required moving control parameters, the imaging field of the VINS accurately cover the detected targets visually.These methods have been verified many times, and the results show that they are effective and feasible. The research results based on the VNIS data have successfully revealed the material composition on the far side of the moon and have deepened human understanding of its formation and evolution.


2021 ◽  
Vol 21 (2) ◽  
pp. 031
Author(s):  
Yu Lu ◽  
Yun-Zhao Wu ◽  
Cui Li ◽  
Jin-Song Ma ◽  
Wen-Wen Qi ◽  
...  

2020 ◽  
Author(s):  
Michelle Lavagna ◽  
Fabrizio Fiore

&lt;p&gt;Assessing the chemical composition of the Moon is a key part of its investigation. Elements can be grouped according to their condensation and geochemical behavior, and thus chemical abundances of key elements can be used to asses both the origin and the evolution of the body.&lt;/p&gt; &lt;p&gt;The relative abundance of the surface (down to a few &amp;#181;m) major elements with atomic number &amp;#163;20 can be estimated using X-ray fluorescence, using solar X-rays to excite element&amp;#8217;s atoms (both quiescent Sun X-ray emission, in particular during solar maxima, and solar flares).&lt;/p&gt; &lt;p&gt;Only an handle of successful X-ray fluorescence experiments have been flown so far, including Apollo15 XRFS, Chandrayaan-1 C1XS, SMART-1 D-C1XS at the Moon, Messanger-XRS, BepiColombo-MIXS at Mercury, and NEAR-XRS at EROS, Hayabusa-XRS at Itokawa, OSIRIS-REX/REXIS at Bennu (Allen et al. 2013, arXiv:1309.6665 and refs. therein).&lt;/p&gt; &lt;p&gt;The main goal of fluorescent X-ray spectroscopy of asteroids is to determine the intensity of Fe-L, Fe-K, Al-K, Mg-K, Si-K complexes and S-Ka, S-Kb fluorescent lines. From these lines mass abundance ratios can be determined [Mg/Si], [Fe/Si]. The comparison of these abundance ratio to those of meteorites can understand whether the surface of the Moon resembles a particular chondritic meteorite.&lt;/p&gt; &lt;p&gt;Gamma-ray spectroscopy of nuclear lines can also be used to assess abundances of elements in the planetary surface (down to 10-20cm, e.g. Reedy et al. 1978, Proc. Lunar Planet Sci. Conf. 9th 1978). The main source of gamma-ray lines are: decay of natural radionuclides, reaction induced by energetic cosmic rays, capture of low-energy neutrons, and solar-proton induced radioactivity. Gamma-ray spectroscopy can provide information on many elements, including those with high atomic number, hardly accessible to X-ray fluorescence spectroscopy. Several successful gamma-ray experiment have been performed so far, including early spectroscopy of the Moon (Luna10, Apollo15, 16), Mars (Mars-5). More recently, Kayuga gamma-ray spectrometer obtained a detailed mapping of radioactive elements on the Moon (K, Th, U), as well major elements, O, Al, Mg, Si, Ca, Ti, Fe (Yamashita et al. EPSC Abstracts Vol. 5, EPSC210-580, 2010, Hasebe et al. Proc. Int. Workshop Advances in Cosmic Ray Science J. Phys. Soc. Jpn. 78, 2009). Other lunar experiments include Lunar prospector and Chang&amp;#8217;E. Other experiments include more Mars spectroscopy (MARS Odyssey) Mercury (Messenger) and the asteroids EROS (NEAR) and 4 Vesta (Dawn). The K/Th ratio is a diagnostic of the body bulk composition and provide information about where and when the body was formed. The collecting area of most X-ray and gamma-ray spectrometers used for planetary observations is quite small, a few cm2. The REXIS instrument working today at Bennu as a collecting area of 25cm2. The largest instrument flown so far is the Kaguya-XRS with a collecting are of 100cm2. A new miniaturize payload is here proposed, currently under development for astrophysics goals and to be installed on a 3U cubesat platform; the sensors uses GAGG scintillator crystals and Silicon Drift Detectors to both detect direct X-ray photons and optical photons produced in the scintillators by interaction with gamma-rays, and can cover a unique wide band, from a few keV to several MeV, providing at the same time both X-ray fluorescent spectroscopy and gamma-ray spectroscopy. The collecting area of a compact instrument (~3-4kg) can be conservatively ~100cm2. A passive collimator can shield the SDD from most Cosmic X-ray Background, reducing the background at energies &lt;20keV, where it is largely dominated by the CXB. Laboratory calibration in the next few months will provide more precise numbers on the resolution achievable. The gamma-ray line sensitivity of this instruments with collecting area ~ 100 cm2 and active anticoincidences (efficiency &amp;#160;&amp;#187; twice that of Kayuga spectrometer) should therefore be a factor several better than that of other planetary gamma-ray spectrometers. The paper shows the proposed scientific mission goals around which the miniaturized payload is designed, and its possible embarking on a cubesat like space segments, 6U large; the whole feasibility study for a smallsat scientific mission is presented, showing the generality of the approach and its applicability also for small bodies exploration as well.&lt;/p&gt;


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