Automated astronaut traverses with minimum metabolic workload: Accessing permanently shadowed regions near the lunar south pole

被引:5
|
作者
Pena-Asensio, Eloy [1 ,2 ]
Sutherland, Jennifer [3 ,4 ]
Tripathi, Prateek [5 ]
Mason, Kashauna [6 ]
Goodwin, Arthur [7 ]
Bickel, Valentin T. [8 ]
Kring, David A. [9 ]
机构
[1] Univ Autonoma Barcelona, Dept Quim, Bellaterra 08193, Catalonia, Spain
[2] CSIC, Inst Ciencies Espai ICE, Campus UAB,C Can Magrans S-N, Cerdanyola Del Valles 08193, Catalonia, Spain
[3] Inst Laue Langevin, 71 Ave Martyrs, F-38000 Grenoble, France
[4] Tech Univ Berlin, Inst Aeronaut & Astronaut, Marchstr 12-14, D-10587 Berlin, Germany
[5] Indian Inst Technol, Dept Civil Engn, Roorkee 247667, Uttarakhand, India
[6] Texas A&M Univ, Dept Geol & Geophys, 400 Bizzell St, College Stn, TX 77843 USA
[7] Univ Manchester, Dept Earth & Environm Sci, Oxford Rd, Manchester M13 9PL, England
[8] Univ Bern, Ctr Space & Habitabil, Gesellschaftsstr 6, CH-3012 Bern, Switzerland
[9] Univ Space Res Assoc, Lunar & Planetary Inst, 3600 Bay Area Blvd, Houston, TX 77058 USA
基金
欧洲研究理事会;
关键词
Artemis; Permanently shadowed regions; Lunar south pole; Astronaut; VOLATILES; MOON; GENERATION; MAGMA;
D O I
10.1016/j.actaastro.2023.10.010
中图分类号
V [航空、航天];
学科分类号
08 ; 0825 ;
摘要
The Artemis exploration zone is a topographically complex impact-cratered terrain. Steep undulating slopes pose a challenge for walking extravehicular activities (EVAs) anticipated for the Artemis III and subsequent missions. Using 5 m/pixel Lunar Orbiter Laser Altimeter (LOLA) measurements of the surface, an automated Python pipeline was developed to calculate traverse paths that minimize metabolic workload. The tool combines a Monte Carlo method with a minimum-cost path algorithm that assesses cumulative slope over distances between a lander and stations, as well as between stations. To illustrate the functionality of the tool, optimized paths to permanently shadowed regions (PSRs) are calculated around potential landing sites 001, nearby location 001(6), and 004, all within the Artemis III 'Connecting Ridge' candidate landing region. We identified 521 PSRs and computed (1) traverse paths to accessible PSRs within 2 km of the landing sites, and (2) optimized descents from host crater rims into each PSR. Slopes are limited to 15 degrees degrees and previously identified boulders are avoided. Surface temperature, astronaut body illumination, regolith bearing capacity, and astronaut-to-lander direct view are simultaneously evaluated. Travel times are estimated using Apollo 12 and 14 walking EVA data. A total of 20 and 19 PSRs are accessible from sites 001 and 001(6), respectively, four of which maintain slopes <10 degrees. degrees . Site 004 provides access to 11 PSRs, albeit with higher EVA workloads. From the crater rims, 94 % of PSRs can be accessed. All round-trip traverses from potential landing sites can be performed in under 2 h with a constant walk. Traverses and descents to PSRs are compiled in an atlas to support Artemis mission planning.
引用
收藏
页码:324 / 342
页数:19
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