Олег К писал(а):
Выше висит что это такое. Это-таки фейк, придуманный спецслужбами?
Читать Вам надо - матчастью не владеете совершенно. Вот зачем было сочинять, что имитатор начали делать чуть ли не в 90-х? Если бы Ви кроме бельгийских работ иногда отрывали серьезную литературу, то прочли бы и про назначение имитатора и про время начала работы над созданием "лунного" грунта, который жулики потом выдавали за настоящий. Ну, например...
"In summary, a highlands simulant can be made by combining crushed anorthite, pyroxene, and synthetic glass in proportions based on grain size, lithic or glassy character, and chemistry.
A High Titanium Mare Simulant
The target chemical composition for the high titanium mare simulant is the Apollo 11 soil average given in Table 1. The lithic and mineral component can be approximated by terrestrialbasalts plus ilmenite.HAW-11 (BasalticVolcanism StudyProject, 1981), whose chemical composition is also given in Table 1, is an example of a suitable basalt. Combining this basalt with ilmenite (FeTiO,) in a 9:l proportion raises the titanium content of the mixture to that of the Apollo 11 soil. The resulting mixture also improves the calculated fit to Si, Fe, and Mg percentages of the Apollo soil
Glass of high titanium mare composition can also be made from melting oxides. Naturally occurring, basaltic-composition volcanic glass, such as is found in Hawaii could be used, but probably will not have a titanium concentration as great as the high titanium mare soils. In summary, a high titanium mare simulant can be made by combining crushed Hawaiian basalt HAW-1 1, ilmenite, and synthetic glass in proportions based on grain size, lithic or glassy character, and chemistry.
Lunar soil simulants were prepared from mixtures of comminuted terrestrial anorthite (Q,), ilmenite (Quebec),olivine (Fo,,), and augite pyroxene (Wo5,En,,) in the weight ratio 4:1:1:4,respectively. Two size ranges (0.09-0.15 mm and 0.15-0.25 mm) were tested in air, and one size range (0.09-0.15 mm) was tested in nitrogen and in a vacuum of approximately 1o-~tom. Samples were weighed in quantities of 1-5 g and were washed and boiled in isopropylalcohol until the supernatantfluid appeared clear.Prior to separation, all samples were dried, first on filter paper and then in glass receptacles in an air oven at 120°-130°C overnight.
Nearly 2500 kg of a basalt simulant was fabricated and characterized for testing the lunar rover (Mitchelland Houston, 1970; Green and Melzer, 1971).
CONCLUSIONS
When planning experiments for activities to take place on the Moon, investigators should remember the following.
Lunar soil in the laboratory does not accurately represent lunar in situ conditions. The Apollo soils have lost their original particle packing and have adsorbed volatiles.
Simulants can be made by ordinary means that reproduce specific properties of lunar soil such as grain size distribution,gross mineral composition,or general chemical composition
A very small amount of lunar soil will be availablefor experimentation.Investigators should scale down their experiments and use simulant whenever possible
Substantial research was also directed toward developing novel methods of fragmentation involving mining equipment that minimizes moving parts. Work using electrothermal techniques for fragmenting
simulated lunar rocks has shown some promising results (Thirumalai and Demou, 1970). Laser technology may also be usell for rock fragmentationpurposes (Lindroth,1974;Lindroth and Krawza, 1971).
Книга "Lunar Bases and Space Activities of the 21st Century"
W. W. Mendell, ©1985, Lunar and Planetary Institute
http://www.lpi.usra.edu/publications/books/lunar_bases/Полная химия и все остальное, вкл. рецепты различных "лунных" смесей и методы их трансформации. Ну, еще не дошло, что речь идет о попытках создать полный заменитель лунного грунта, что отчасти удалось и что было представлено, как ЛГ по программе Аполлон?
В работе благоразумно не указываются даты ранее 1970-го года, но сканы я выкладывал.
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