2015
DOI: 10.1061/(asce)as.1943-5525.0000462
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Geotechnical Properties of BP-1 Lunar Regolith Simulant

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Cited by 35 publications
(10 citation statements)
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“…The C c value of KLS-1 (0.29) was similar to the suggested C c of 0.3 for loose lunar soil (Heiken et al 1991). The recompression index (C r ) values were 0.0043 (KLS-1), 0.0045 (JSC-1), and 0.0050 (FJS-1), which are consistent with the known C r value (0.0042) of initially compressed (dense) lunar simulants (Suescun-Florez et al 2015).…”
Section: Stress-strain (Compressibility) Characteristicssupporting
confidence: 69%
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“…The C c value of KLS-1 (0.29) was similar to the suggested C c of 0.3 for loose lunar soil (Heiken et al 1991). The recompression index (C r ) values were 0.0043 (KLS-1), 0.0045 (JSC-1), and 0.0050 (FJS-1), which are consistent with the known C r value (0.0042) of initially compressed (dense) lunar simulants (Suescun-Florez et al 2015).…”
Section: Stress-strain (Compressibility) Characteristicssupporting
confidence: 69%
“…Compressibility parameters (compression index, C c ; swelling or recompression index, C s or C r ) of lunar simulants are also important considerations for lunar vehicle and surface construction designs. The typical C c value of loose lunar soil is recommended to be 0.05-0.3 depending on the density conditions (Suescun-Florez et al 2015). In this study, a typical one-dimensional oedometer test (ASTM 2011b) was performed to evaluate compressibility parameters of JSC-1, FJS-1, and KLS-1 lunar simulants.…”
Section: Stress-strain (Compressibility) Characteristicsmentioning
confidence: 99%
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“…In general, due to the absence of atmosphere on the Moon, the iron is present in the form of Fe 2 and FeO (Markandeya Raju & Pranathi, ) on the real lunar regolith. However, for the regolith simulants low content of Fe 2 O 3 has been observed, in specific 14.60% for DNA‐1, 8% for DNA‐1A (this study), 6% for BP‐1 (Black Point‐1), and 3.41% for JSC‐1A (after Cesaretti et al, ; Rickman et al, ; Suescun‐Florez et al, ).…”
Section: Methodsmentioning
confidence: 46%
“…In general, a good resemblance observed between DNA-1A particles and images of JSC-1A regolith (Alshibli & Hasan, 2009) and lunar regolith (Carrier, 2003) in terms of angular shape with sharp corners and crevices on the surface. One major difference between the lunar regolith and its simulant is the presence of interparticle adhesion in the original Moon material (Costes & Mitchell, 1970;Suescun-Florez et al, 2014), which might be due to the different specific surfaces of the particles formed in different environmental conditions (Marzulli & Cafaro, 2019).…”
Section: General Description and Origin Of Dna-1a And Ottawa Sandmentioning
confidence: 99%