National Science Review · 2021 · 460 citations · 35 references
Natural SciencesEarth SciencesGeologyGeochemistryPlanetary GeologySoil MineralogyLunar GeologyMineral Soil ClassificationPlanetary CompositionPlanetary MineralogySoil CompositionSoil GeochemistryBulk DensityLunar BrecciasLunar Mare BasaltsLunar MineralogyLunar StratigraphyMoon CompositionRegolith Bulk DensitySpecific Surface Area
After 45 years since the Apollo and Luna missions, China’s Chang’E‑5 mission returned new lunar samples from the mid‑latitude northeastern Oceanus Procellarum. CE‑5 lunar soils are fine (95 % of particles 1.40–9.35 µm, 95 % of mass 4.84–432.27 µm), have bulk density 1.24 g cm⁻³, true density 3.20 g cm⁻³, specific surface area 0.56 m² g⁻¹, consist mainly of low‑Ti/low‑Al/low‑K mare basalt clasts, and exhibit high FeO with low Mg index, indicating a new basalt class.
Abstract Forty-five years after the Apollo and Luna missions returned lunar samples, China's Chang’E-5 (CE-5) mission collected new samples from the mid-latitude region in the northeastern Oceanus Procellarum of the Moon. Our study shows that 95% of CE-5 lunar soil sizes are found to be within the range of 1.40–9.35 μm, while 95% of the soils by mass are within the size range of 4.84–432.27 μm. The bulk density, true density and specific surface area of CE-5 soils are 1.2387 g/cm3, 3.1952 g/cm3 and 0.56 m2/g, respectively. Fragments from the CE-5 regolith are classified into igneous clasts (mostly basalt), agglutinate and glass. A few breccias were also found. The minerals and compositions of CE-5 soils are consistent with mare basalts and can be classified as low-Ti/low-Al/low-K type with lower rare-earth-element contents than materials rich in potassium, rare earth element and phosphorus. CE-5 soils have high FeO and low Mg index, which could represent a new class of basalt.
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