Question Earth Moon Origin

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Can we learn from the comets and rocks that are left over when the solar system formed?


[Submitted on 7 Mar 2025]

Design of a low-thrust gravity-assisted rendezvous trajectory to Halley's comet​

Roberto Flores, Alessandro Beolchi, Elena Fantino, Chiara Pozzi, Mauro Pontani, Ivano Bertini, Cesare Barbieri
Comets are the most pristine planetesimals left from the formation of the Solar System. They carry unique information on the materials and the physical processes which led to the presence of planets and moons. Many important questions about cometary physics, such as origin, constituents and mechanism of cometary activity, remain unanswered. The next perihelion of comet 1P/Halley, in 2061, is an excellent opportunity to revisit this object of outstanding scientific and cultural relevance. In 1986, during its latest approach to the Sun, several flyby targeted Halley's comet to observe its nucleus and shed light on its properties, origin, and evolution. However, due to its retrograde orbit and high ecliptic inclination, the quality of data was limited by the large relative velocity and short time spent by the spacecraft inside the coma of the comet. A rendezvous mission like ESA/Rosetta would overcome such limitations, but the trajectory design is extremely challenging due to the shortcomings of current propulsion technology. Given the considerable lead times of spacecraft development and the long duration of the interplanetary transfer required to reach the comet, it is imperative to start mission planning several decades in advance. This study presents a low-thrust rendezvous strategy to reach the comet before the phase of intense activity during the close approach to the Sun. The trajectory design combines a gravity-assist maneuver with electric propulsion arcs to maximize scientific payload mass while constraining transfer duration. A propulsive plane change maneuver would be prohibitive. To keep the propellant budget within reasonable limits, most of the plane change maneuver is achieved via either a Jupiter or a Saturn flyby. The interplanetary low-thrust gravity-assisted trajectory design strategy is described, followed by the presentation of multiple proof-of-concept solutions.
 
Life after the Moon and Earth impact theory.
With a pinch of salt.

[Submitted on 19 Mar 2025]

Deep Mantle-Atmosphere Coupling and Carbonaceous Bombardment: Options for Biomolecule Formation on an Oxidized Early Earth​

Klaus Paschek, Thomas K. Henning, Karan Molaverdikhani, Yoshinori Miyazaki, Ben K. D. Pearce, Ralph E. Pudritz, Dmitry A. Semenov
Understanding what environmental conditions prevailed on early Earth during the Hadean eon, and how this set the stage for the origins of life, remains a challenge. Geologic processes such as serpentinization and bombardment by chondritic material during the late veneer might have been very active, shaping an atmospheric composition reducing enough to allow efficient photochemical synthesis of HCN, one of the key precursors of prebiotic molecules. HCN can rain out and accumulate in warm little ponds (WLPs), forming prebiotic molecules such as nucleobases and the sugar ribose. These molecules could condense to nucleotides, the building blocks of RNA molecules, one of the ingredients of life. Here, we perform a systematic study of potential sources of reducing gases on Hadean Earth and calculate the concentrations of prebiotic molecules in WLPs based on a comprehensive geophysical and atmospheric model. We find that in a reduced H2-dominated atmosphere, carbonaceous bombardment can produce enough HCN to reach maximum WLP concentrations of ∼1−10mM for nucleobases and, in the absence of seepage, ∼10−100μM for ribose. If the Hadean atmosphere was initially oxidized and CO2-rich (90%), we find serpentinization alone can reduce the atmosphere, resulting in WLP concentrations of an order of magnitude lower than the reducing carbonaceous bombardment case. In both cases, concentrations are sufficient for nucleotide synthesis, as shown in experimental studies. RNA could have appeared on Earth immediately after it became habitable (about 100Myr after the Moon-forming impact), or it could have (re)appeared later at any time up to the beginning of the Archean.
 
This is incredible research.
This is like looking at a fossil SN in the past.
Looking at the evidence for the origin of the moon.

[Submitted on 26 Mar 2025]

To detect strong nugget with an acoustic array​

Haoyang Qi, Renxin Xu
This article discusses strong nuggets (SNs) which means strong interaction condensed matter clusters with a mass of about 106g. They may originate from the early universe, supernova, pulsar merger event, and so on. Depending on the equation of state, the SNs could be stable and even be one of the candidates for dark matter. In order to detect SNs which hitting the Earth or the Moon at a non-relativistic velocity, a new messenger, the acoustic array, is analysed. The results of the calculations show that the impact signal of an SN can be detected at a distance of about 30 kilometers from the nugget's trajectory. By using microphone boxes, hydrophones or seismographs to construct an array in the bedrock, ocean or on the Moon, it is possible to reconstruct the velocity, mass, and interacting cross section of SNs, and then constrain also the nature of supra-nuclear matter. The acoustic array can also be used for distributed acoustic sensing of meteorites or earthquakes. The sonar localisation system on the proposed High-energy Underwater Neutrino Telescope (HUNT) is suggested as a pathfinder for acoustic array detection.
 

Catastrophe

"Science begets knowledge, opinion ignorance.
Here is a more comprehensive reference:


This includes a NASA article with a very good video much lower down under "Model Behavior"
Best put on "Full Screen" right away by clicking on symbol bottom right of black box.
This is not visible until you click at bottom right corner.



Cat :)
 
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Sometimes we need to look beyond to understand the evolution of our solar system.

[Submitted on 2 Mar 2025]

Investigating the formation of small Solar System objects using stellar occultations by satellites: present, future and its use to update satellite orbits​

Felipe Braga-Ribas, Frederic Vachier, Josselin Desmars, Giuliano Margoti, Bruno Sicardy
The history of the outer solar system is intrinsically related to the Giant Planets migration. A massive disk of material within a radius of 30~au was scattered during the planetary migration, creating different dynamic populations in the Transneptunian region. They were formed in a collisional environment when massive collisions allowed them to grow and form much smaller moons than the primary body. The dynamical group, known as the Cold Classicals, was formed in a sparse disk from 42 to about 47~au and did not suffer much from planet migration. Observations show that many of Cold Classical are binary, consistent with the streaming instability process. The stellar occultation technique, with a spatial resolution of a few kilometres, can be used to search for binaries where other techniques are unable to do so, and to characterise the known satellites of Trans-Neptunian Objects (TNO), constraining their formation scenarios. We review here the first stellar occultations by TNO's satellites (besides Charon), discuss the methods used to detect these events. We also fit new orbital elements and system mass for Vanth (Orcus/1) and Weywot (Quaoar/1), finding reasonable solutions for pure Keplerian orbits. Finally, we discuss the prospects regarding the stellar occultations by TNO binaries and their implications for the study of the history of the Solar System.
 
For those who want to search deeper into the origin of our Solar System.
The structure of the moons and the planets may have a similar origin.
The disc formed from our Sun billions of years ago may have originated from our Sun expelling matter in the form of an hourglass.
Yes, our Sun may have passed through a Nebula millions of years ago and added to the Sun's Core and matter throughout the Solar System.


[Submitted on 3 Apr 2025]

Size and shape of the trans-Neptunian object (470316) 2007 OC10: Comparison with thermal data​

J.M. Gómez-Limón, R. Leiva, J. L. Ortiz, N. Morales, M. Kretlow, M. Vara-Lubiano, P. Santos-Sanz, A. Álvarez-Candal, J. L. Rizos, R. Duffard, E. Fernández-Valenzuela, Y. Kilic, S. Cikota, B. Sicardy, F. Bragas-Ribas, M. R. Alarcon, S. Alis, Z. Benkhaldoun, A. Burdanov, J. de Wit, S. Calavia Belloc, J. Calvo Fernández, O. Canales Moreno, G. Catanzaro, S. Fisek, A. Frasca, R. Iglesias-Marzoa, R. Infante-Sainz, A. Jiménez-Guisado, S. Kaspi, T. Kuutma, D. Lafuente Aznar, J. Licandro, J. L. Maestre, P. Martorell, A. Nastasi, G. Occhipinti, C. Perelló, C. Rinner, B. Samper-Doménech, A. San Segundo, T. Santana-Ros, M. Serra-Ricart
The shapes of only 12 trans-Neptunian objects have been directly measured, offering crucial insights into their internal structure. These properties are strongly connected to the processes that shaped the early Solar System, and provide important clues about its evolution.
The aim of the present work is to characterise the size, shape, geometric albedo, and beaming parameter of the TNO (470316) 2007 OC10 . We compared these values to the effective diameter and geometric albedo obtained from thermal data by the TNOs are Cool survey. We also combined occultation and thermal data to constrain the size of a putative unresolved satellite.
We predicted an occultation of the star Gaia DR3 2727866328215869952 by 2007 OC10 on 2022 August 22. Four stations detected the occultation. We implemented an elliptical shape model for the projection of 2007 OC10. Following a Bayesian approach, we obtained the posterior probability density in the model parameter space using a Markov chain Monte Carlo method.
The elliptical limb of 2007 OC10 has semi-axes of 215+10−7×141+24−23 km, and thus the projected axis ratio is b/a=0.58+0.16−0.16. The area-equivalent diameter is 330+56−55,km. From our own absolute magnitude value of HV=5.40±0.02, the geometric albedo is pV=11.2+2.1−5.0 %. Combining the occultation results with thermal data, we constrain the beaming parameter to η=1.42+0.75−0.58. Occultation data reveal that the star is double. The secondary star has a position angle with respect to the primary of 56+3−17 degrees, has an angular separation of 57+4−11 mas, and is 1.18+0.07−0.07 magnitudes fainter than the primary.
 
Research keeps going deeper.

[Submitted on 2 Apr 2025]

Observational diversity of bright long-lived Type II supernovae​

T. Nagao, T. M. Reynolds, H. Kuncarayakti, R. Cartier, S. Mattila, K. Maeda, J. Sollerman, P. J. Pessi, J. P. Anderson, C. Inserra, T.-W. Chen, L. Ferrari, M. Fraser, D. R. Young, M. Gromadzki, C. P. Gutiérrez, G. Pignata, T. E. Muller-Bravo, F. Ragosta, A. Reguitti, S. Moran, M. González-Bañuelos, M. Kopsacheili, T. Petrushevska
In various types of supernovae (SNe), strong interaction between the SN ejecta and circumstellar material (CSM) has been reported. This raises questions on their progenitors and mass-loss processes shortly before the explosion. Recently, the bright long-lived Type~II SN 2021irp was proposed to be a standard Type II SN interacting with disk-like CSM. The observational properties suggest that the progenitor was a massive star in a binary system and underwent a mass-ejection process due to the binary interaction just before the explosion. Here, we study the diversity of the observational properties of bright long-lived Type II (21irp-like) SNe. We analyse the diversity of their CSM properties, in order to understand their progenitors and mass-loss mechanisms and their relations with the other types of interacting SNe. We performed photometry, spectroscopy, and/or polarimetry for four 21irp-like SNe. Based on these observations as well as published data of SN~2021irp itself and well-observed bright and long-lived type II SNe including SNe~2010jl, 2015da and 2017hcc, we discuss their CSM characteristics. This sample of SNe shows luminous and long-lived photometric evolution, with some variations in the photometric evolution (from ∼−17 to ∼−20 absolute mag in the r/o band even at ∼200 days after the explosion). They show photospheric spectra characterized mainly by Balmer lines for several hundreds of days, with some variations in the shapes of the lines. They show high polarization with slight variations in the polarization degrees with rapid declines with time (from ∼3−6 \% before the peak to ∼1 \% at ∼200 days after the peak). The observational properties are consistent with the disk-CSM-interaction scenario, i.e., typical Type~II SNe interacting with disk-like CSM.
 

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