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Estimation of Lunar Surface Shock Effects and Optimization of Damping Scenarios: A Case Study in Response to NASA's Request for Proposal

 

 

Purpose of Research  

Estimation of Lunar Surface Shock Effects and Optimization of Damping Scenarios: A Case Study in Response to NASA's Request for Proposal

 

Abdi-Basid Ibrahim ADAN*

* Correspondance : abdi-basid@outlook.com

                             

 


                                                             A B S T R A C T                                         . 

The aim of the present work is to respond to NASA's request for proposals on understanding and reducing the adverse effects of   landing or take-off on the lunar surface. Two initiatives can be developed. The first is that of a natural satellite with no atmospheric layer, which suggests that any particle will fall at the same speed in the absence of any air friction effects. A rocket could land without any major impact.  The second is to take into account an atmosphere above the lunar surface. Terrestrial particles are likely to form and remain in suspension for some time. To remedy this situation, six scenarios were explored. Two alternatives have emerged from these investigations:

The first is the installation of a device (rocket accessories) to reduce the effects of the fuselage during ascent;

The second is the integration of new features into the rocket, such as vertical fuselages or a folding and unfolding locomotion slide to move the dust cloud away from the formation zone.

Keywords : NASA, Landing, Moon, Regolith, Lift-off, Artemis, Starship Virginia, Hampton, Human Lander


1.      Introduction

In space, granular and rocky materials are subject to both gravitational and atmospheric circulation forces during a disturbance. The latter derives its ancestral force from temperature, i.e. solar radiation [1]. Without the existence of an atmospheric layer and the spherical shape, atmospheric circulation modelling would certainly have taken a wrong turn. On the lunar surface, the conditions of reasonable distance from the solar source (i.e. 150,000,000 km [2]) and sphericity can be an asset for comparison with the Earth. In the absence of a layer of air enveloping its surface, the equilibrium of a homogeneous spatial temperature distribution around a mean value cannot be justified on the lunar surface (unlike Saturn's moon Titan). For this reason, winds would not exist on the moon, nor would a sandstorm or cyclonic season. In this case, the moon's sphericity would only be useful in the vertical meridian zone, to facilitate a short-distance landing, unlike at the north and south poles.

The aim of this first work is to contribute to a philosophical understanding of how granular and rocky materials of all sizes can behave on the lunar surface after being exposed to the landing or take-off force of a rocket weighing several thousand tonnes.

Until now, rocket take-off and landing missions have been carried out in vertical motion and are assumed to have the same impact effect on surfaces, even if the weight of the re-launch is slightly different from that of the ascent, due to the variation in the weight of the on-board fuel.

The gravity field on the lunar surface is calculated at 1.62 m/s2 [3], i.e. a gravitational acceleration some six times lower than on the Earth's surface (9.81 m/s2 [4]). An Artemis rocket with crew and cargo can weigh at least 2,000 tonnes [5]. The amount of fuel and its weight are astronomically proportional to the mission's round-trip distance, engine efficiency and on-board engine technology.

For a landing mission, there is a threshold altitude at which a surface covered in dust and rock is touched by the propulsion force (e.g. 39,144 kN [5]), which keeps the weight of the craft suspended in the void and slows down gravitational attraction. In principle, the slower the ascent, the greater the impact on the surface. Contrary to what happens on Earth, the return to normal after an ascent impact on the lunar surface for a landing mission would be faster with the same time interval, whatever the characteristics of the seed and rock lifted. For rocks thrown up with kinetic force, the impact does not seem to affect the craft directly or indirectly. On the other hand, the stronger the gravitational field, the faster the rocket's ascent is expected to be, so as not to over-consume on-board fuel, while avoiding a hard landing that would disable many of the craft's functions and features. Given the Earth's gravity field, a lunar landing mission would be around six times slower and six times more fuel-efficient.

In addition, thanks to the Lunar Atmosphere and Dust Environment Explorer (LADEE) mission, recent studies [6,7] have changed our perception of the Moon, confirming the presence of a lunar atmosphere, albeit almost negligible compared with that of the Earth. The sources of this atmosphere can be multiple: meteorite bombardment, rock decomposition, solar eruptions, etc.

When examining the lunar atmospheric layer, it will be vitally important to understand the atmospheric pressure with the elements that make up the lunar atmosphere, mainly argon, helium, sodium and hydrogen. The shock effect on the lunar surface would be based essentially on the interaction potentials of these latter chemical elements.

With a view to providing some answers to NASA's project, the remainder of this article is organized as follows:

- First, we analyze an approach in which cloud cover is neglected.

- Secondly, we counter this approach by proposing scenarios and draft solutions.


2.      Analysis of the Artemis landing mission: case without lunar atmosphere

The riskiest incident on a lunar mission would not be the suspension of rocks and other particles in lunar space, since all rocks, whatever their size, would fall at the same speed. In addition, the spiral effect observed in the drag of turbojet aircraft would not exist on the Moon, due to the absence of air particles. What's more, the projections caused by the blast effect on landing will be projected in all directions, from the source of the ascent to extremities whose distance is proportional to the force. In this context, the risks of a mission to the Moon are much lower than on Earth. Impact with the surface does not directly or indirectly endanger the spacecraft, except in the case of nearby installations.

Prospecting the lunar surface and its stiffness composition would appear to be an indispensable asset in the study of an initial landing strip. Meteorite impact zones can represent a major hazard for rocket landings and take-offs. Projections of elements from the lunar surface can cause fallout on the rocket, due to its specific funnel shape at the point of impact with the lunar surface. The geological characteristics of the more rigid zones should be compared between the Moon's surface and that of the Earth, in order to identify an optimum zone for reducing the impact of rocket engine propulsion.

 

3.      Analysis of the Artemis landing mission: case with lunar atmosphere

In this section, we analyze five scenarios whose feasibility seems to be approaching with the maturity of current technologies. This section takes into account the importance of the lunar atmosphere and proposes solutions to avoid complications with the dust cloud during ascent.

 

3.1.           Scenario 1 : absorption

In the scenario shown in figure 1, at a precise and optimal altitude during ascent, the rocket detaches a circular capsule (which can be unfolded and folded), absorbing the propelled granular and rocky materials and releasing the absorbed air by filtering. This device is designed to withstand the extreme temperature of the fuselage, and to incorporate artificial intelligence to identify rocks according to their respective risks. The prototype shown in figure 1 is essentially based on the capacity and performance of rock and dust aspirators, which will be released at a given altitude before landing. The parameters of these aspirators will be designed to ensure a safe landing of Artemis on the lunar surface.


Figure 1.
Circular vacuum cleaner for dust and granules.

 

3.2.           Scenario 2 : parachuting

The scenario described in figure 2 involves parachutes being released to trap granular and rocky material rising towards the summit during ascent.  The number of parachutes used may vary to optimize landing safety. The characteristics of these parachutes must correspond to the results expected for the safety mission. In addition, each parachute must be equipped with a device that detects and predicts the area most affected by the fuselage explosion, in order to optimize deployment on the priority area. This requires the use of artificial intelligence. The feasibility of such a device seems certain to reduce rock and granule heave, as well as the formation of dust clouds.


Figure 2.
Case of a parachute trapping the effects of shock.

 

                                                                           

3.3.           Scenario 3 : artificial vat

The scenario in figure 3 describes a prototype that deploys a device capable of sinking into the lunar soil (like a tomahawk missile) and deploying a kind of metal tank inside the soil. The latter is adapted to the overheated condition and will contain the blast, while sparing the lunar soil from being impacted by the blast.

This will prevent the formation of dust clouds and reduce the risk of dust impacting the rocket engine during landing [8].


Figure 3.
Case of a tank sinking to the surface of the moon.

 

3.4.           Scenario 4 : surface copper

In the scenario below (figure 4), as the rocket ascends, at a precise and ideal altitude, a slide ejects from the rocket and deploys over a wide lunar surface to serve as a landing point and avoid the lifting of granules and other rocky material. Unlike the previous scenario, this is a surface deployment with automatic ground engagement. This shows just how important automatic devices and artificial intelligence are for this mission.



Figure 4.
Cas de cuivre dépliable comme point d’atterrissage.

 

3.5.           Scenario 5 : fuselage horizontal

In the scenario shown in Figure 5, the rocket fuselage would have to be redesigned to incorporate a new vertical fuselage system capable of slowing down gravity. Self-deploying vertical fuselages are intended to compensate for the traditional fuselage. This approach will minimize the blast effect of the fuselage on the lunar surface.

Other modifications can also be made, including the integration of a wheel to help the rocket move away from the dust cloud formation zone after landing.


Figure 5.
Feasibility scenario of additional fuselage rotation during Artemis landing.

 

3.6.           Scenario 6 : dust cover

In the final scenario of the Artemis mission back to the moon, the ship's skin should have physico-chemical properties that prevent dust from clinging to the ship. This proposal, presented in figure 6, can be based on the secret of dust adhering to materials, allowing the rocket to remain free of dust and rocks, while landing safely. In addition, it is possible to develop a device that propels small quantities of water to wet the dust and limit its effects.


Figure 6. 
Feasibility case for a dust cover on the Artemis surface.

 

4.      Relationship between distance, weight, projection effects and landing time

In this subsection, we set up an empirical program to model the impact phenomenon on a surface covered with dust and rock :

We consider the variables :

Ø  T, existence of atmospheric circulation

Ø  U, the surface area of the impact zone

Ø  V, rocket landing time.

Ø  W, shock absorption time.

Ø  X, rocket weight;

Ø  Y, local gravity field;

Ø  Z, kinetic force of the projected lunar rock fragment.

Based on this program, the following hypotheses can be formulated:

1.      The surface area of the impact zone increases with the weight of the rocket.

2.      The existence of atmospheric circulation contributes to a major risk during ascent.

3.       Landing time contributes to rocket blast impact area.

4.      Time to return to normal after landing depends on gravity and the existence of an atmosphere.

5.      The weight of the rocket is positively correlated with the level of risk of danger from surface impact effects.

To minimize the risk of clouds of dust and rocky material forming during the ascent of Artemis, this would require simulations based on mathematical formulations that describe the relationships between the variables defined above. In addition, observations of each of these variables can be used to develop a simpler model with a study of multidimensional variation.

 

Conclusion

On the lunar surface, a rocket will weigh 6 times less than on Earth. Rock fragments and the formation of lunar dust clouds can be mitigated by studying the physical properties of the chemical particles that make up the lunar atmosphere. The disturbance of lunar surface materials during rocket ascent is due not only to the gravity field, but also to the atmosphere, whose density is almost negligible for the moon.

Landing with the least possible effect will require the invention of new prototypes incorporating artificial intelligence to maximize decision-making in the shortest possible time. Fuselage modifications and the integration of new rocket functionalities will also be required.

 

Reference 

1.      Brian Hurley. (2012). D'où vient le vent ? Wind Site Evaluation Ltd.

2.      Pierre Bessemoulin,Jean Oliviéri. (2000).LE RAYONNEMENT SOLAIRE ET SA COMPOSANTE ULTRAVIOLETTE.La Météorologie 8e 42 série - n° 31.

3.      Dean Leslie Muirhead. (2021) .Development of a Planetary Water Treatment System. 50th International Conference on Environmental Systems ICES-2021-36.

4.      Sergio L. Pinski, M.D., 2002, Cleveland Clinic Florida, 2950 Cleveland Clinic Blvd., Weston, FL 33331. (954) 659-5292.

5.      Wikipedia. https://fr.wikipedia.org/wiki/Artemis_I.[Accessed 03/06/2023].

6.      Horányi, M., Sternovsky, Z., Lankton, M., Dumont, C., Gagnard, S., Gathright, D., … Wright, G. (2014). The Lunar Dust Experiment (LDEX) Onboard the Lunar Atmosphere and Dust Environment Explorer (LADEE) Mission. Space Science Reviews, 185(1-4), 93–113. doi:10.1007/s11214-014-0118-7.

7.      Elphic, R. C., Delory, G. T., Hine, B. P., Mahaffy, P. R., Horanyi, M., … Noble, S. K. (2014). The Lunar Atmosphere and Dust Environment Explorer Mission. Space Science Reviews, 185(1-4), 3–25. doi:10.1007/s11214-014-0113-z.

8.      A Korzun, M Mehta. Plume-Surface Interaction: Maturing Predictive Environments for Propulsive Landing on the Moon and Mars International Planetary Probe Workshop 2021. ntrs.nasa.gov

 

 

 

 



Complementarity of Time and Space

 ___________________Complementarity of Time and Space

 

The Gregorian calendar (in honour of Pope Gregory XIII of the Catholic Church) was born in 1582, after the reforms made to the Roman Republican calendar and then to the Julian calendar (in honour of Julius Caesar, 46 BC).

To see the beginnings of this evolution, we must go back to the 5th millennium to discover the first solar calendar, the one adopted by the Egyptians, based on the star Sirius (the second brightest star in our galaxy). However, with the recent discovery in 2013 by a team from the University of Birmingham, Scotland, of a lunar calendar dating back over 10 millennia, the record for the oldest calendar has been broken.

Put simply, it takes us 8772 hours (on average) to complete an elliptical orbit around the sun. But with the expansion of the Universe (according to the Hubble constant of 67.4 km/s/Mpc (kilometres per second per megaparsec)), the journey of our galaxy since the Big Bang event means that time is no longer static in a cycle, like the hand on a clock. By moving from one point in the Universe to another in the course of a year, the Milky Way must travel through the Cosmos.

The logical possibility of going back in time would be to eventually bring the galaxy back to its starting point of one year. However, this probability is infinitesimally small, because it would involve disrupting the revolution of the sun around its axis, the solar system or the spiral-moving nayau of the galaxy. Infinitesimally small, because if the Andromeda galaxy moves in a different direction to the opposite direction on the Milky Way, things will take on a new time dimension in the system.

Abdi-Basid ADAN, 2022

Multidisciplinary Interpretation of Precipitation: Principles and Concepts (Part I)

 

Multidisciplinary Interpretation of Precipitation: Principles and Concepts (Part I)

 

Etymologically derived from the Latin expression "praecipitatio" which literally means "fall". Precipitation, according to the meteorological sense, takes another dimension of concept to designate a particular natural phenomenon of the climate called "rain". This last one has the possibility to occur in a region, in several states (liquid, solid... etc.). With the breakthrough of scientific research in the nineteenth and twentieth centuries, the most abundant element in the Universe and on Earth are coincidentally the elements that constitute water, that is, hydrogen in the Universe and oxygen on Earth. We owe this important discovery to the precursor of modern chemistry, Antoine Lavoisier (1743-1794), who succeeded in identifying the components of water in a world where technology was sorely lacking to carry out scientific research.

From the well-known characteristic forms attributed to precipitation, it is also known that there is a secondary specificity that categorizes precipitation, depending on the area of coverage; intensity and duration. It seems quite reasonable to assume that less extensive cloud cover will tend to result in precipitation of higher intensity and shorter duration. The latter is defined as convective precipitation, as opposed to stratiform precipitation. In the seven layers that make up the atmosphere, the different cloud classifications are generally located at an altitude between 1000 and 12000 m, barely exceeding the troposphere (13000 m).

The real cradle of precipitation begins with the partial blocking of stellar radiation by the ozone layer of the stratosphere. In fact, once they reach the surface of the earth, the emitted radiations cause, through the temperature, the warming that results in the evaporation of the surface of the seas (which is none other than the evapotranspiration). Thus, the water vapor generated as a result of this phenomenon, causes an upward movement under the impulse of the atmospheric pressure which gradually decreases in altitude. A lower pressure due to a low density of molecules present in the air with a lower temperature leads in turn to the condensation of water vapor around a core, consisting of charged and neutral particles.  These combine to reach the saturation point of humidity (high density of water vapor in the air) and marks the appearance of the cloud in its irregular forms that we observe during the day. With its almost negligible weight compared to its immense size, the quantity of visible clouds manages however to remain suspended in the atmosphere and thus escapes, for a time, the gravitational attraction of the terrestrial gravity.

Drawn at will by wind circulations, the new cooling and condensation improvise the cloud to take more weight in the process of supersaturation and favors the phenomenon of precipitation and previously conditioned by the humidity of the air of the coverage area. Once again, between the humid area and the dry air, the temperature and the equinox play in favor or against a precipitation phenomenon that can give life to the ground without vaporizing into the atmosphere. Although essential for the supply of groundwater, which is sometimes found almost in the fourth layer of the earth's crust (lower mantle), the chemical composition of precipitation can be altered by the polluting components present in the air. Therefore, it would not be a prejudice to consider precipitation as a major factor of a rapid response disease in a locality.

Due to the rotation, revolution, tilt and sphericity of the Earth, the unevenly distributed global temperature results in the occurrence of wind circulations in multiple directions. For example, a warm air mass gaining altitude cools and creates convection to interact with water vapour as it condenses and, on the other hand, causes wind to be driven.  In addition, the horizontal force of atmospheric pressures and the perpendicular force of inertia known as its precursor Coriolis (Gaspard-Gustave Coriolis (1792-1843)) explain in the literature to a large extent the direction and intensity of wind in atmospheric circulations, which is a major means of locomotion of clouds across continents and oceans.

On a global scale, there are three distinct zones of wind circulation: the Hadley cell, the Ferrel convection and the polar circulation. For the first, the Hadley cell, located from the Equator to 30°N and 30°S, winds blow from the Northeast to the Southwest and from the Southeast to the Northwest (called Trade Winds) and marks the low pressure intertropical convergence zone. The second, the Ferrel zone, is characterized by transient low pressure areas with winds blowing generally towards the West. North and south of the 60th parallel is the polar zone with eastward wind speeds. These three zones of the globe are interconnected by the so-called "fast air" atmospheric current (polar and subtropical type) whose directions are almost sinusoidal over the globe.

Through these atmospheric currents, oceanic circulations are also affected by seasonal variability as pointed out by Walker (1868-1958) and Humboldt (1769-1859). For example, the decrease of the circulation in the Hadley cell, can displace the Walker cell and favor the displacement of warm surface waters of the South Pacific: this meteorological phenomenon is known under the famous expression "El Niño", which in turn influences the precipitation, just as "La Niña" would disrupt the temperature of other lands.

In addition, the topographic nature of the Earth's surface also interacts with the climate. For example, by blocking the circulation of temperature at high altitudes and weather, mountainous areas contribute to the supply of precipitation over several kilometers and change the climatic conditions of the surrounding area.

Eccentrically, the Paleocene-Eocene period (56 million years) has been identified as a breakthrough in the knowledge of paleoclimatic variability. This highlights the existence of a major factor, beyond a simple meteorite impact on the Earth, to upset the climate balance.  The change in the Earth's orbit, or the deformation of the Earth's ellipse, according to scientists at the University of Pennsylvania, marked the warmest period since the Earth's birth 4.6 billion years ago. Such warming has certainly traced the history of precipitation evolution on Earth.

From a theological point of view, the links between atmospheric circulations and precipitation have been mentioned since the seventh century in, for example, the Holy Quran of Islam. In particular, it is reported in Sura 30, verse 48:

« It is Allah Who sends the winds, which then stir up ˹vapour, forming˺ clouds, which He then spreads out in the sky or piles up into masses as He wills, from which you see rain come forth. Then as soon as He causes it to fall on whoever He wills of His servants, they rejoice, ».

 

 

And from Sura 24, verse 43:

« Do you not see that Allah gently drives the clouds, then joins them together, piling them up into masses, from which you see raindrops come forth? And He sends down from the sky mountains ˹of clouds˺ loaded with hail, pouring it on whoever He wills and averting it from whoever He wills. The flash of the clouds’ lightning nearly takes away eyesight. ».

 

In general, in the process of precipitation formation, several different atmospheric phenomena according to specific standards, some known, others unknown, and exo-atmospheric phenomena contribute directly and indirectly.

 

 

Abdi-Basid ADAN, 2022.

The Abdi-Basid Courses Institute