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Lunar Highlands (LHS-1) High-Fidelity Moon Dirt Simulant
Lunar Highlands (LHS-1) High-Fidelity Moon Dirt Simulant
Lunar Highlands (LHS-1) High-Fidelity Moon Dirt Simulant
Lunar Highlands (LHS-1) High-Fidelity Moon Dirt Simulant
Lunar Highlands (LHS-1) High-Fidelity Moon Dirt Simulant
Lunar Highlands (LHS-1) High-Fidelity Moon Dirt Simulant
Scanning electron microscope image of LHS-1, magnification 50X
Scanning electron microscope image of LHS-1, magnification 100X
Scanning electron microscope image of LHS-1, magnification 500X
Scanning electron microscope image of LHS-1, magnification 1000X
Lunar Highlands (LHS-1) High-Fidelity Moon Dirt Simulant
Lunar Highlands (LHS-1) High-Fidelity Moon Dirt Simulant

Lunar Highlands (LHS-1) High-Fidelity Moon Dirt Simulant

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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

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