1 kilogram = 2.2 pounds
The LHS-1 Lunar Highlands Simulant, developed by Exolith Lab, is a high-fidelity, mineral-based simulant appropriate for a generic or average highlands location on the Moon. The highlands are considered to be the “lighter” regions of the moon’s surface which is mainly comprised of plagioclase, or often referred to as Anothrosite. The simulant is not made of a single terrestrial lithology, but accurately captures the texture of lunar regolith by combining both mineral and rock fragments in accurate proportions referencing the returned Apollo mission regolith.
To receive samples of our Lunar Highlands Simulant (LHS-1) material constituents click here.
The simulant is made of several terrestrial minerals, and accurately captures the texture of lunar regolith by combining both mineral and rock fragments (i.e., polymineralic grains) in precise proportions.
The particle size distribution of the simulant is targeted to match that of typical Apollo soils. LHS-1 does not currently simulate agglutinates or nanophase iron. However, our agglutinated simulant, LHS-1-25A, does simulate agglutinates characteristic of an intermediately mature Lunar Highlands Regolith. Custom simulated agglutinate mixes are also available upon request which can be found [here]. [link anorthosite agglutinates]
All of our simulants are an upgraded, high-fidelity alternative to the commonly known JSC-1A simulant.
For information on Mineralogy, bulk chemistry, and geotechnical properties, please see below:
Spec Sheet* SDS
*Previous spec sheets and data for past regolith simulant batches can be found at bottom of page.
Mineralogy
Component |
Wt.% |
Anorthosite |
74.4 |
Glass-rich basalt |
24.7 |
Ilmenite |
0.4 |
Pyroxene (Bronzite)
|
0.3 |
Olivine
|
0.2 |
The individual minerals that make up our Lunar Simulants are available here
Bulk Chemistry
This table shows the relative abundances of each element detected by X-ray fluorescence (XRF). The relative abundances of elements detected by XRF in geological samples are quantified as oxides. In the simulant, these elements are contained in the minerals described in the Mineralogy table above, and not necessarily in oxide form. These data are from the Hamilton Analytical Lab.
Oxide |
Wt% |
SiO2
|
51.2 |
TiO2
|
0.6
|
Al2O3
|
26.6
|
FeO |
2.7
|
MnO |
0.1
|
MgO |
1.6
|
CaO |
12.8
|
Na2O
|
2.9
|
K2O
|
0.5
|
P2O5
|
0.1 |
LOI* |
0.4 |
Total** |
99.4
|
*Loss on ignition
**Excluding volatiles and trace elements; see spec sheet.
Physical Properties
Mean Particle Size: 90 µm
Particle Size Range: <0.01 µm – 1000 µm
Bulk density*: 1.30 g/cm3
Grain Density: 2.75 g/cm3
Void Ratio: 1.11
Porosity: 52.7%
Angle of Repose (10g): 47.0°
Angle of Repose (250g): 39.5°
Note that bulk density is not an inherent property and depends on the level of compaction
*Spec Sheet (Before 06/2021)
*Spec Sheet (6/2021-Current)
We would love to hear about the success of your research. If you have any information you'd like to share with us, please send us an email at exolithlab@ucf.edu.
Photo Credit: Abigail Glover, Exolith Lab