<?xml version="1.0" encoding="UTF-8"?><!DOCTYPE article  PUBLIC "-//NLM//DTD Journal Publishing DTD v3.0 20080202//EN" "http://dtd.nlm.nih.gov/publishing/3.0/journalpublishing3.dtd"><article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" dtd-version="3.0" xml:lang="en" article-type="research article"><front><journal-meta><journal-id journal-id-type="publisher-id">JHEPGC</journal-id><journal-title-group><journal-title>Journal of High Energy Physics, Gravitation and Cosmology</journal-title></journal-title-group><issn pub-type="epub">2380-4327</issn><publisher><publisher-name>Scientific Research Publishing</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.4236/jhepgc.2021.74084</article-id><article-id pub-id-type="publisher-id">JHEPGC-112406</article-id><article-categories><subj-group subj-group-type="heading"><subject>Articles</subject></subj-group><subj-group subj-group-type="Discipline-v2"><subject>Physics&amp;Mathematics</subject></subj-group></article-categories><title-group><article-title>
 
 
  Solar System. Angular Momentum. Dark Matter Reactors
 
</article-title></title-group><contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Vladimir</surname><given-names>S. Netchitailo</given-names></name><xref ref-type="aff" rid="aff1"><sub>1</sub></xref><xref ref-type="corresp" rid="cor1"><sup>*</sup></xref></contrib></contrib-group><aff id="aff1"><label>1</label><addr-line>Biolase Inc., Irvine, USA</addr-line></aff><pub-date pub-type="epub"><day>26</day><month>08</month><year>2021</year></pub-date><volume>07</volume><issue>04</issue><fpage>1353</fpage><lpage>1372</lpage><history><date date-type="received"><day>26,</day>	<month>August</month>	<year>2021</year></date><date date-type="rev-recd"><day>9,</day>	<month>October</month>	<year>2021</year>	</date><date date-type="accepted"><day>12,</day>	<month>October</month>	<year>2021</year></date></history><permissions><copyright-statement>&#169; Copyright  2014 by authors and Scientific Research Publishing Inc. </copyright-statement><copyright-year>2014</copyright-year><license><license-p>This work is licensed under the Creative Commons Attribution International License (CC BY). http://creativecommons.org/licenses/by/4.0/</license-p></license></permissions><abstract><p>
 
 
  The developed Hypersphere World-Universe Model (WUM) is consistent with all Concepts of the World [1]. In WUM, we postulate the principal role of Angular Momentum and Dark Matter in Cosmological theories of the World. The most widely accepted model of Solar System formation, known as the Nebular hypothesis, does not solve the Angular Momentum problem—why is the orbital momentum of Jupiter larger than rotational momentum of the Sun? WUM is the only cosmological model in existence that is consistent with this Fundamental Law. The Nebular hypothesis does not solve Internal Heating and Diversity problems for all Planets and Moons in Solar system—why the actual mean surface temperature of them is higher than their effective temperature calculated based on the Sun’s heat for them and how could each one be so different if all of them came from the same nebula? The proposed concept of Dark Matter Reactors in Cores of all gravitationally-rounded Macroobjects successfully resolves these problems.
 
</p></abstract><kwd-group><kwd>Hypersphere World-Universe Model</kwd><kwd> Medium of the World</kwd><kwd> Dark Matter Particles</kwd><kwd> Macroobjects Structure</kwd><kwd> Rotational Fission</kwd><kwd> Law of Conservation of Angular Momentum</kwd><kwd> Dark Epoch</kwd><kwd> Light Epoch</kwd><kwd> Solar Corona</kwd><kwd> Solar Wind</kwd><kwd> Dark Matter Reactor</kwd></kwd-group></article-meta></front><body><sec id="s1"><title>1. Introduction. Short History of Solar System Formation</title><p>The most widely accepted model of Solar system formation, known as the Nebular hypothesis, was first proposed in 1734 by E. Swedenborg [<xref ref-type="bibr" rid="scirp.112406-ref2">2</xref>] [<xref ref-type="bibr" rid="scirp.112406-ref3">3</xref>] and later elaborated and expanded upon by I. Kant in 1755 in his “Universal Natural History and Theory of the Heavens” [<xref ref-type="bibr" rid="scirp.112406-ref4">4</xref>].</p><p>Nebular Hypothesis maintains that 4.6 billion years ago, the Solar System (SS) formed from the gravitational collapse of a giant molecular cloud, which was light years across. Most of the mass collected in the Centre, forming the Sun; the rest of the mass flattened into a protoplanetary disc, out of which the planets and other objects in SS formed.</p><p>The Nebular hypothesis is not without its critics. In his “The Wonders of Nature”, V. Ferrell outlined the following counter-arguments [<xref ref-type="bibr" rid="scirp.112406-ref5">5</xref>]:</p><p>&#183; It contradicts the obvious physical principle that gas in outer space never coagulates; it always spreads outward;</p><p>&#183; Each planet and moon in Solar system has unique structures and properties. How could each one be different if all of them came from the same nebula;</p><p>&#183; A full 98 percent of all the angular momentum in the Solar system is concentrated in the planets, yet a staggering 99.8 percent of all the mass in our Solar system is in our Sun;</p><p>&#183; Jupiter itself has 60 percent of the planetary angular motion. Evolutionary theory cannot account for this. This strange distribution was the primary cause of the downfall of the Nebular hypothesis;</p><p>&#183; There is no possible means by which the angular momentum from the Sun could be transferred to the planets. Yet this is what would have to be done if any of the evolutionary theories of Solar system origin are to be accepted.</p><p>Lunar Origin Fission Hypothesis was proposed by G. Darwin in 1879 to explain the origin of the Moon by rapidly spinning Earth, on which equatorial gravitative attraction was nearly overcome by centrifugal force [<xref ref-type="bibr" rid="scirp.112406-ref6">6</xref>]. D. U. Wise made a detailed analysis of this hypothesis in 1966 and concluded that “it might seem prudent to include some modified form of rotational fission among our working hypothesis” [<xref ref-type="bibr" rid="scirp.112406-ref7">7</xref>].</p><p>Solar Fission Theory was proposed by L. Jacot in 1951 who stated that [<xref ref-type="bibr" rid="scirp.112406-ref8">8</xref>]:</p><p>&#183; The planets were expelled from the Sun one by one from the equatorial bulge caused by rotation;</p><p>&#183; One of these planets shattered to form the asteroid belt;</p><p>&#183; The moons and rings of planets were formed from the similar expulsion of material from their parent planets.</p><p>T. Van Flandern further extended this theory in 1993 [<xref ref-type="bibr" rid="scirp.112406-ref9">9</xref>]. He proposed that planets were expelled from the Sun in pairs at different times. Six original planets exploded to form the rest of the modern planets. It solves several problems the standard model does not:</p><p>&#183; If planets fission from the Sun due to overspin while the proto-Sun is still accreting, this more easily explains how 98% of the Solar system’s angular momentum ended up in the planets;</p><p>&#183; It solves the mystery of the dominance of prograde rotation for these original planets since they would have shared in the Sun’s prograde rotation at the outset;</p><p>&#183; It also explains coplanar and circular orbits;</p><p>&#183; It is the only model that explains the twinning of planets (and moons) and difference of planet pairs because after each planet pair is formed in this way, it will be some time before the Sun and extended cloud reach another overspin condition.</p><p>The outstanding issues of the Solar fission are:</p><p>&#183; It is usually objected that tidal friction between a proto-planet and a gaseous parent, such as the proto-Sun, ought to be negligible because the gaseous parent can reshape itself so that any tidal bulge has no lag or lead, and therefore transfers no angular momentum to the proto-planet;</p><p>&#183; There would exist no energy source to allow for planetary explosions.</p><p>Neither L. Jacot nor T. Van Flandern proposed an origin for the Sun itself. It seems that they followed the standard Nebular hypothesis of the formation of the Sun. In our Model, we concentrated on furthering the Solar fission theory [<xref ref-type="bibr" rid="scirp.112406-ref10">10</xref>].</p></sec><sec id="s2"><title>2. Angular Momentum Problem</title><p>Angular Momentum Problem is one of the most critical problem in Standard Cosmology that must be solved. Standard Cosmology does not explain how Galaxies and Extrasolar systems obtained their enormous orbital angular momenta. Any theory of evolution of the Universe that is not consistent with the Law of Conservation of Angular Momentum should be promptly ruled out. To the best of our knowledge, WUM is the only cosmological model in existence that is consistent with this Fundamental Law.</p><p>The outstanding issues of SS are:</p><p>&#183; The rotational momentum of the Sun is smaller than Jupiter’s, Saturn’s, Uranus’s, and Neptune’s orbital momentum. Evolutionary theory cannot account for this. This strange distribution was the primary cause of the downfall of the Nebular hypothesis;</p><p>&#183; There is no possible means by which the angular momentum from the Sun could be transferred to the planets.</p><p>There is another problem in the Standard Cosmology—Orbital Angular Momentum problem [<xref ref-type="bibr" rid="scirp.112406-ref11">11</xref>] [<xref ref-type="bibr" rid="scirp.112406-ref12">12</xref>]:</p><p>&#183; SS has an orbital momentum L o r b S S calculated based on the distance of 26.4 kly from the galactic Centre and orbital speed of about 220 km/s: L o r b S S = 1.1 &#215; 10 56   J ⋅ s , which far exceeds the rotational angular momentum: L r o t S S = 3.2 &#215; 10 43   J ⋅ s ;</p><p>&#183; Milky Way (MW) galaxy is gravitationally bounded with the Local Supercluster and has an orbital angular momentum L o r b M W calculated based on the distance of 65 million light-years from Local Supercluster and orbital speed of about 400 km/s [<xref ref-type="bibr" rid="scirp.112406-ref13">13</xref>]: L o r b M W = 2.5 &#215; 10 71   J ⋅ s , which far exceeds the rotational angular momentum of MW [<xref ref-type="bibr" rid="scirp.112406-ref14">14</xref>]: L r o t M W ≈ 1 &#215; 10 67   J ⋅ s ;</p><p>&#183; How did MW and SS obtain their substantial orbital angular momenta?</p><p>In frames of WUM, we calculated rotational and orbital angular momentum of all gravitationally-rounded Macroobjects in SS, from Mimas, a small moon of Saturn ( R M = 198   km , M M = 3.75 &#215; 10 19     kg ) to the Sun itself ( R S = 7 &#215; 10 5     km , M S = 2 &#215; 10 30     kg ) and found that orbital momenta of most satellites are indeed substantially smaller than the rotational momenta of their prime objects, with three exceptions [<xref ref-type="bibr" rid="scirp.112406-ref11">11</xref>]:</p><p>&#183; The Sun accounts for about 0.3% of the total rotational angular momentum of SS while about 60% is attributed to Jupiter;</p><p>&#183; The rotational momentum of the Earth is substantially smaller than Moon’s orbital momentum;</p><p>&#183; The rotational momentum of Pluto is considerably smaller than Charon’s orbital momentum.</p><p>In our opinion, there is the only one mechanism that can provide angular momenta to Macroobjects—Rotational Fission of overspinning (surface speed at equator exceeding escape velocity) Prime Objects. From the point of view of Fission model, the Prime Object is transferring some of its rotational angular momentum to orbital and rotational momenta of satellites. It follows that the rotational momentum of the prime object should exceed the orbital momentum of its satellite.</p><p>In frames of WUM, Prime Objects are Dark Matter (DM) Cores of Superclusters, which must accumulate tremendous rotational angular momenta before the Birth of the Luminous World. It means that it must be some long enough time in the history of the World, which we named “Dark Epoch” [<xref ref-type="bibr" rid="scirp.112406-ref12">12</xref>]. To be consistent with the Law of Conservation of Angular Momentum we developed a New Cosmology of the World:</p><p>&#183; WUM introduces Dark Epoch (spanning from the Beginning of the World for 0.45 billion years) when only DM Macroobjects (MOs) existed, and Luminous Epoch (ever since for 13.77 billion years) when Luminous MOs emerged due to the Rotational Fission of Overspinning DM Superclusters’ Cores and self-annihilation of Dark Matter Particles (DMPs);</p><p>&#183; Proposed Weak Interaction between DMPs provides the integrity of DM Cores, which are 3D fluid balls with a high viscosity and act as solid-state objects;</p><p>&#183; The main objects of the World are overspinning DM Cores of Superclusters, which accumulated tremendous rotational angular momenta during Dark Epoch and transferred it to DM Cores of Galaxies during their Rotational Fission. The experimental observations of galaxies in the universe showed that most of them are disk galaxies: about 60% are ellipticals and about 20% are spirals [<xref ref-type="bibr" rid="scirp.112406-ref13">13</xref>]. These results speak in favor of the developed Rotational Fission mechanism;</p><p>&#183; Size, mass, density, composition, L o r b and L r o t of satellite cores depend on local density fluctuations at the edge of the overspinning prime DM cores and cohesion of the outer shell. Consequently, the diversity of satellite cores has a clear explanation;</p><p>&#183; Dark Matter Core of MW was born 13.77 billion years ago as the result of the Rotational Fission of the Local Supercluster DM Core;</p><p>&#183; DM Cores of Extrasolar systems, planets and moons were born as the result of the repeating Rotational Fissions of MW DM Core in different times (4.57 billion years ago for SS);</p><p>&#183; Macrostructures of the World form from the top (superclusters) down to galaxies, extrasolar systems, planets, and moons.</p><p>Based on the developed New Cosmology, we performed a detailed analysis of the angular momenta of all gravitationally-rounded Macroobjects in SS and found that [<xref ref-type="bibr" rid="scirp.112406-ref11">11</xref>]:</p><p>&#183; The overspinning DM Core of MW could produce DM core of the Sun with the substantial orbital angular momenta of SS;</p><p>&#183; The overspinning DM Core of the Sun could produce DM cores of all planets, which could produce DM cores of all moons, including the Moon of the Earth;</p><p>The Pluto-Charon pair is definitely a binary system. Charon was not generated by Pluto’s DM core; instead, they are two Macroobjects that happened to be bounded together by gravity.</p></sec><sec id="s3"><title>3. Sun</title><p>Internal Structure. According to the standard Solar model, the Sun has:</p><p>&#183; Core that extends from the center to about 20% - 25% of the solar radius, contains 34% of the Sun’s mass with density ρ max = 1.5 &#215; 10 5 kg / m 3 and ρ min = 2 &#215; 10 4 kg / m 3 . It produces all of Sun’s energy;</p><p>&#183; Radiative zone from the Core to about 70% of the solar radius with density ρ max = 2 &#215; 10 4 kg / m 3 and ρ min = 2 &#215; 10 2 kg / m 3 in which convection does not occur and energy transfer occurs by means of radiation;</p><p>&#183; Core and Radiative zone contain practically all Sun’s mass [<xref ref-type="bibr" rid="scirp.112406-ref14">14</xref>]. In our view, they are parts of DM Core of the Sun.</p><p>The large power output of the Sun is mainly due to the huge size and density of its Core (compared to the Earth), with only a fairly small amount of power being generated per cubic meter. Theoretical models of the Sun’s interior indicate a maximum power density of approximately 276.5 W⁄m<sup>3</sup> at the center of the Core [<xref ref-type="bibr" rid="scirp.112406-ref15">15</xref>] (see <xref ref-type="table" rid="table1">Table 1</xref>), which is about the same power density inside a compost pile [<xref ref-type="bibr" rid="scirp.112406-ref16">16</xref>] and closer approximates reptile metabolism than a thermonuclear bomb.</p><p>Solar Core Rotation. E. Fossat, et al. found that Solar Core rotates 3.8 &#177; 0.1 faster than the surrounding envelope [<xref ref-type="bibr" rid="scirp.112406-ref17">17</xref>]. The fact that the Solar Core rotates faster than surrounding envelope, despite high viscosity of the internal medium, is intriguing. WUM explains this phenomenon through the absorption of DMPs by Solar Core over time τ . DMPs supply not only additional mass ( ∝ τ 3 / 2 ), but also additional angular momentum ( ∝ τ 2 ). DM Core irradiates products of DMPs self-annihilation, which carry away excessive angular momentum. The Solar Wind is the result of this mechanism [<xref ref-type="bibr" rid="scirp.112406-ref12">12</xref>].</p><p>Evolution of the Sun. By 1950s, stellar astrophysicists had worked out the physical principles governing the structure and evolution of stars [<xref ref-type="bibr" rid="scirp.112406-ref18">18</xref>]. According</p><table-wrap id="table1" ><label><xref ref-type="table" rid="table1">Table 1</xref></label><caption><title> Computer Model of the Sun at 4.5 Billion Years. Adapted from [<xref ref-type="bibr" rid="scirp.112406-ref15">15</xref>]</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >Radius, Rel. to R<sub>ʘ</sub></th><th align="center" valign="middle" >Radius &#215; 10<sup>9</sup> m</th><th align="center" valign="middle" >Temperature &#215; 10<sup>6</sup> K</th><th align="center" valign="middle" >Luminosity, %</th><th align="center" valign="middle" >Fusion Rate, W⁄kg</th><th align="center" valign="middle" >Fusion Power Density, W⁄m<sup>3</sup></th></tr></thead><tr><td align="center" valign="middle" >0</td><td align="center" valign="middle" >0.00</td><td align="center" valign="middle" >15.7</td><td align="center" valign="middle" >0</td><td align="center" valign="middle" >0.0175</td><td align="center" valign="middle" >276.5</td></tr><tr><td align="center" valign="middle" >0.09</td><td align="center" valign="middle" >0.06</td><td align="center" valign="middle" >13.8</td><td align="center" valign="middle" >33</td><td align="center" valign="middle" >0.010</td><td align="center" valign="middle" >103.0</td></tr><tr><td align="center" valign="middle" >0.12</td><td align="center" valign="middle" >0.08</td><td align="center" valign="middle" >12.8</td><td align="center" valign="middle" >55</td><td align="center" valign="middle" >0.0068</td><td align="center" valign="middle" >56.4</td></tr><tr><td align="center" valign="middle" >0.14</td><td align="center" valign="middle" >0.10</td><td align="center" valign="middle" >11.3</td><td align="center" valign="middle" >79</td><td align="center" valign="middle" >0.0033</td><td align="center" valign="middle" >19.5</td></tr><tr><td align="center" valign="middle" >0.19</td><td align="center" valign="middle" >0.13</td><td align="center" valign="middle" >10.1</td><td align="center" valign="middle" >91</td><td align="center" valign="middle" >0.0016</td><td align="center" valign="middle" >6.9</td></tr><tr><td align="center" valign="middle" >0.22</td><td align="center" valign="middle" >0.15</td><td align="center" valign="middle" >9.0</td><td align="center" valign="middle" >97</td><td align="center" valign="middle" >0.0007</td><td align="center" valign="middle" >2.2</td></tr><tr><td align="center" valign="middle" >0.24</td><td align="center" valign="middle" >0.17</td><td align="center" valign="middle" >8.1</td><td align="center" valign="middle" >99</td><td align="center" valign="middle" >0.0003</td><td align="center" valign="middle" >0.67</td></tr><tr><td align="center" valign="middle" >0.29</td><td align="center" valign="middle" >0.20</td><td align="center" valign="middle" >7.1</td><td align="center" valign="middle" >100</td><td align="center" valign="middle" >0.00006</td><td align="center" valign="middle" >0.09</td></tr><tr><td align="center" valign="middle" >0.46</td><td align="center" valign="middle" >0.32</td><td align="center" valign="middle" >3.9</td><td align="center" valign="middle" >100</td><td align="center" valign="middle" >0</td><td align="center" valign="middle" >0</td></tr><tr><td align="center" valign="middle" >0.69</td><td align="center" valign="middle" >0.48</td><td align="center" valign="middle" >1.73</td><td align="center" valign="middle" >100</td><td align="center" valign="middle" >0</td><td align="center" valign="middle" >0</td></tr><tr><td align="center" valign="middle" >0.89</td><td align="center" valign="middle" >0.62</td><td align="center" valign="middle" >0.66</td><td align="center" valign="middle" >100</td><td align="center" valign="middle" >0</td><td align="center" valign="middle" >0</td></tr></tbody></table></table-wrap><p>to these principles, the Sun’s luminosity had to change over time, with the young Sun being about 30% less luminous than today [<xref ref-type="bibr" rid="scirp.112406-ref19">19</xref>] [<xref ref-type="bibr" rid="scirp.112406-ref20">20</xref>] [<xref ref-type="bibr" rid="scirp.112406-ref21">21</xref>] [<xref ref-type="bibr" rid="scirp.112406-ref22">22</xref>]. The long-term evolution of the bolometric solar luminosity L ( τ ) as a function of cosmological time τ can be approximated by a simple linear law: L ( τ ) ∝ τ [<xref ref-type="bibr" rid="scirp.112406-ref18">18</xref>].</p><p>One of the consequences of WUM holds that all stars were fainter in the past. As their cores absorb new DMPs, size of MO cores R M O and their luminosity L M O are increasing in time: R M O ∝ τ 1 / 2 and L M O ∝ R M O 2 ∝ τ , respectively. Taking the age of the World: A W ≅ 14.2   Byr and the age of SS: A S S ≅ 4.6   Byr , it is easy to find that the young Suns’ output was 67% of what it is today. Literature commonly refers to the value of 70% [<xref ref-type="bibr" rid="scirp.112406-ref21">21</xref>]. This result supports the developed model of the structure and evolution of the Sun [<xref ref-type="bibr" rid="scirp.112406-ref18">18</xref>].</p><p>Solar Flare is a sudden flash of increased brightness on the Sun, usually observed near its surface and in close proximity to a sunspot group. Powerful flares are often, but not always, accompanied by a coronal mass ejection. The maximum total energy of a bolometric fluence that was observed in 2012 is: 6 &#215; 10<sup>25</sup> J [<xref ref-type="bibr" rid="scirp.112406-ref23">23</xref>]. During the impulsive stage of Solar flares, radio waves, hard x-rays, and gamma rays with energy above 100 GeV are emitted (one photon had an energy as high as 467.7 GeV) [<xref ref-type="bibr" rid="scirp.112406-ref24">24</xref>].</p><p>Coronal Mass Ejection is a significant release of plasma from the solar corona. They often follow solar flares and are normally present during a solar prominence eruption. Coronal mass ejections are often associated with other forms of solar activity, but a broadly accepted theoretical understanding of these relationships has not been established. Coronal Mass Ejections most often originate from active regions on the Sun’s surface, such as groupings of sunspots associated with frequent flares.</p><p>In WUM, Solar Flares and Coronal Mass Ejections are the result of the activity of DM Core of the Sun. They can be explained by the Sun’s DM Core eruptions of DMPs and their subsequent self-annihilation. As the result, radio waves and gamma rays are observed together with mass ejections of ordinary particles originated by the self-annihilation of DMPs. It is worth noting that the self-annihilation of DMPs depends on the density squared. It is in good agreement with Fusion Power Density distribution inside of the Sun considering drop of density from 1.5 &#215; 10<sup>5</sup> kg⁄m<sup>3</sup> at the Centre to 2 &#215; 10<sup>2</sup> kg⁄m<sup>3</sup> at the edge of DM core.</p></sec><sec id="s4"><title>4. Earth</title><p>Internal Structure. Information about the Earth’s structure mostly comes from the analysis of seismic waves. According to the standard model, the Earth has the following layers: an outer silicate solid Crust, solid Mantle, a liquid Outer core, and a solid Inner core. The Inner core is believed to be composed of an iron-nickel alloy with some other elements. The temperature at the Inner core’s surface is estimated to be approximately 5700 K. The liquid Outer core surrounds the Inner core and is believed to be composed of iron mixed with nickel and trace amounts of lighter elements.</p><p>Although seismic waves propagate through the core as if it was solid, the measurements cannot distinguish between a perfectly solid material from an extremely viscous one. Some scientists have therefore considered whether there may be slow convection in the Inner Core as is believed to exist in the Mantle. That could be an explanation for the anisotropy detected in seismic studies. In 2009, B. Buffett estimated the viscosity of the Inner core at 10<sup>18</sup> kg∙m<sup>−1</sup>∙s<sup>−1</sup> [<xref ref-type="bibr" rid="scirp.112406-ref25">25</xref>].</p><p>In our view, the Inner core, Outer core, and Lower mantle are the parts of the Earth’s liquid DM core, which have different viscosities from extremely high values for the Inner core going down to a 660-km boundary between the Lower mantle and Upper mantle with Crust. The main characteristics of the Earth’s layers are presented in <xref ref-type="table" rid="table2">Table 2</xref>.</p><p>Let us take a look at the structure of the Earth:</p><p>&#183; An Inner core and an Outer core that extend from the Centre to about 55% of the Earth radius with density ρ max = 1.3 &#215; 10 4 kg / m 3 and ρ min = 9.9 &#215; 10 3 kg / m 3 ;</p><p>&#183; Lower mantle, spanning from the Outer core to about 90% of the Earth</p><table-wrap id="table2" ><label><xref ref-type="table" rid="table2">Table 2</xref></label><caption><title> Density and mass of Earth’s layers. Adapted from [<xref ref-type="bibr" rid="scirp.112406-ref26">26</xref>]</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >Depth, km</th><th align="center" valign="middle" >Component Layer</th><th align="center" valign="middle" >Outer Radius, Rel. to Earth Radius</th><th align="center" valign="middle" >Density, kg⁄m<sup>3</sup> &#215;10<sup>3</sup></th><th align="center" valign="middle" >Mass, kg &#215; 10<sup>22</sup></th><th align="center" valign="middle" >Mass, Rel. to Earth Mass</th></tr></thead><tr><td align="center" valign="middle" >0</td><td align="center" valign="middle" >Atmosphere</td><td align="center" valign="middle" ></td><td align="center" valign="middle" >0.0012</td><td align="center" valign="middle" >0.0005</td><td align="center" valign="middle" >0.0000008</td></tr><tr><td align="center" valign="middle" >0 - 11</td><td align="center" valign="middle" >Oceans</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >1.02 - 1.05</td><td align="center" valign="middle" >0.14</td><td align="center" valign="middle" >0.0002</td></tr><tr><td align="center" valign="middle" >0 - 35</td><td align="center" valign="middle" >Crust</td><td align="center" valign="middle" >1</td><td align="center" valign="middle" >2.2 - 2.9</td><td align="center" valign="middle" >4</td><td align="center" valign="middle" >0.007</td></tr><tr><td align="center" valign="middle" >35 - 660</td><td align="center" valign="middle" >Upper Mantle</td><td align="center" valign="middle" >0.99</td><td align="center" valign="middle" >3.4 - 4.4</td><td align="center" valign="middle" >112</td><td align="center" valign="middle" >0.19</td></tr><tr><td align="center" valign="middle" >660 - 2900</td><td align="center" valign="middle" >Lower Mantle</td><td align="center" valign="middle" >0.9</td><td align="center" valign="middle" >3.4 - 5.6</td><td align="center" valign="middle" >265</td><td align="center" valign="middle" >0.44</td></tr><tr><td align="center" valign="middle" >2900 - 5100</td><td align="center" valign="middle" >Outer Core</td><td align="center" valign="middle" >0.55</td><td align="center" valign="middle" >9.9 - 12.2</td><td align="center" valign="middle" >183</td><td align="center" valign="middle" >0.31</td></tr><tr><td align="center" valign="middle" >5100 - 6400</td><td align="center" valign="middle" >Inner Core</td><td align="center" valign="middle" >0.2</td><td align="center" valign="middle" >12.8 - 13.1</td><td align="center" valign="middle" >12</td><td align="center" valign="middle" >0.02</td></tr></tbody></table></table-wrap><p>radius (below 660 km) with density ρ max = 5.6 &#215; 10 3 kg / m 3 and ρ min = 3.4 &#215; 10 3 kg / m 3 ;</p><p>&#183; Upper mantle, spanning from the Lower mantle to about 99% of the Earth radius (below 35 km) with density ρ max = 4.4 &#215; 10 3 kg / m 3 and ρ min = 3.4 &#215; 10 3 kg / m 3 ;</p><p>&#183; Inner core, Outer core, and Lower mantle contain most of the Earth’s mass [<xref ref-type="bibr" rid="scirp.112406-ref27">27</xref>].</p><p>Very little is known about the Lower mantle apart from that there is a seismicity cutoff-660 (660-km discontinuity): ρ min = 3.4 &#215; 10 3 kg / m 3 for the Lower mantle is less than ρ max = 4.4 &#215; 10 3 kg / m 3 for the Upper mantle. In our view, Lower mantle is the part of the Earth’s DM core.</p><p>W. Wu, S. Ni, and J. Irving investigated scattered seismic waves traveling inside the Earth to constrain the roughness of the Earth’s 660-km boundary [<xref ref-type="bibr" rid="scirp.112406-ref28">28</xref>]. The researchers were surprised by just how rough that boundary is—rougher than the surface layer that we all live on. The roughness was not equally distributed, either; just as the Crust’s surface has smooth ocean floors and massive mountains, the 660-km boundary has rough areas and smooth patches [<xref ref-type="bibr" rid="scirp.112406-ref29">29</xref>].</p><p>X. Markenscoff in the paper “Volume collapse” instabilities in deep-focus earthquakes: a shear source nucleated and driven by pressure” explains “the mystery of the long-standing observations in deep-focus earthquakes (400 - 700 km) by symmetry-breaking instabilities in high-pressure phase transformation, which produce the counterintuitive phenomenon of “volume collapse” producing only shear radiation, with little, or no, volumetric component, even under conditions of full isotropy” [<xref ref-type="bibr" rid="scirp.112406-ref30">30</xref>].</p><p>According to WUM, the 660-km boundary is a boundary between Earth’s DM core and Upper mantle with Crust, which were produced by DM core during 4.57 billion years [<xref ref-type="bibr" rid="scirp.112406-ref11">11</xref>]. The deep-focus earthquakes are connected with random mass ejections of DM core happening at the 660-km boundary.</p><p>Random Variations of Earth’s Rotational Speed. G. Jones and K. Bikos in the paper “Earth Is in a Hurry in 2020” wrote [<xref ref-type="bibr" rid="scirp.112406-ref31">31</xref>]:</p><p>“When highly accurate atomic clocks were developed, they showed that the length of a mean solar day can vary by milliseconds. These differences are obtained by measuring the Earth’s rotation with respect to distant astronomical objects”. It turned out that the variations of the daylength throughout 2020 were in the range 86400 − 1.46   ms + 1.62   ms   s . The speed of the Earth’s rotation varies constantly because of the complex motion of its molten core, oceans and atmosphere, plus other effects (see <xref ref-type="fig" rid="fig1">Figure 1</xref>. Adapted from [<xref ref-type="bibr" rid="scirp.112406-ref31">31</xref>] ).</p><p>In frames of WUM, random variations of the Earth’s rotational speed on a daily basis can be explained by variations in an activity of the Earth’s DM core. As the result of DMPs self-annihilation, random mass ejections are happening. During a time of high DM core activity, the Earth’s rotational speed is lower (long days) due to increase of their moment of inertia. When random mass ejections are less frequent, the Earth’s moment of inertia is decreasing, we observe</p><p>short days.</p><p>Let us analyze the proposed mechanism. The relative change of the daylength throughout 2020 was about 2 &#215; 10<sup>−8</sup>. Hence, the relative change of the Earth’s moment of inertia must be about 2 &#215; 10<sup>−8</sup>. If a layer of a mass m at radius of r will shift on h, the relative change of the Earth’s moment of inertia will be about</p><p>m M r R h R ~ 10 − 8 , where M and R are the mass and radius of the Earth, respectively. In case of the Atmosphere (see <xref ref-type="table" rid="table2">Table 2</xref>): m M ~ 10 − 6 , r ~ R , and h R ~ 10 − 2 . It means that h ~ 64   km . In case of the Oceans: m M ~ 10 − 4 , r ~ R , and h R ~ 10 − 4 . It means that h ~ 0.64   km . In case of the boundary Lower mantle—Upper mantle: m M ~ 10 − 5 , r ~ R , and h R ~ 10 − 3 . It means that h ~ 6.4   km .</p><p>The estimated values of the masses and shifts show:</p><p>&#183; There is no way to explain the random variations of the speed of the Earth’s rotation by the complex motion of oceans and atmosphere as it was supposed in [<xref ref-type="bibr" rid="scirp.112406-ref31">31</xref>];</p><p>&#183; They can be explained by random mass ejections of the Lower mantle’s layer.</p><p>Internal Heating. The analysis of the Sun’s heat for planets in SS yields the effective temperature of Earth of 255 K [<xref ref-type="bibr" rid="scirp.112406-ref32">32</xref>]. The actual mean surface temperature of Earth is 288 K [<xref ref-type="bibr" rid="scirp.112406-ref33">33</xref>]. The higher actual temperature of the Earth is due to the heat generated internally by the planet itself. According to the standard model, the Earth’s internal heat is produced mostly through the radioactive decay. The major heat-producing isotopes within Earth are K-40, U-238, and Th-232. The mean global heat loss from Earth is 44.2 &#177; 1.0 TW [<xref ref-type="bibr" rid="scirp.112406-ref34">34</xref>]. The Earth’s Uranium has been thought to be produced in one or more supernovae over 6 billion years ago.</p><p>Radiogenic decay can be estimated from the flux of geoneutrinos that are emitted during radioactive decay. The KamLAND Collaboration combined precise measurements of the geoneutrino flux from the Kamioka Liquid-Scintillator Antineutrino Detector, Japan, with existing measurements from the Borexino detector, Italy. They found that decay of U-238 and Th-232 together contribute about 20 TW to the total heat flux from the Earth to space. The neutrinos emitted from the decay of K-40 contribute 4 TW. Based on the observations the KamLAND Collaboration made a conclusion that “heat from radioactive decay contributes about half of Earth’s total heat flux” [<xref ref-type="bibr" rid="scirp.112406-ref35">35</xref>].</p><p>Plutonium-244 with half-life of 80 million years is not produced in significant quantities by the nuclear fuel cycle, because it needs very high neutron flux environments. Any Plutonium-244 present in the Earth’s Crust should have decayed by now. Nevertheless, D. C. Hoffman, et al. in 1971 obtained the first indication of Pu-244 present existence in Nature [<xref ref-type="bibr" rid="scirp.112406-ref36">36</xref>].</p><p>In WUM, all chemical products of the Earth including isotopes K-40, U-238, Th-232, and Pu-244, are produced within the Earth as the result of the DMPs self-annihilation with the rest energy 1.3 TeV (compare to proton rest energy 938 MeV) [<xref ref-type="bibr" rid="scirp.112406-ref11">11</xref>]. They arrive in the Crust of the Earth due to convection currents in the mantle carrying heat and isotopes from the interior to the planet’s surface [<xref ref-type="bibr" rid="scirp.112406-ref37">37</xref>]. According to WUM, the 660-km boundary is a boundary between Dark Matter Reactor and Upper mantle with Crust, which were produced by Dark Matter Reactor during 4.57 billion years and are, in fact, “Homemade” [<xref ref-type="bibr" rid="scirp.112406-ref11">11</xref>].</p><p>As a conclusion, the internal heating of all gravitationally-rounded Macroobjects of SS is due to DMPs self-annihilation in their DM cores made up of DMPs (1.3 TeV). The amount of energy produced due to this process is sufficiently high to heat up the Macroobjects. New DMPs freely penetrate through the entire Macroobjects’ envelope, get absorbed into the DM cores, and continuously support DMPs self-annihilation.</p><p>Faint Young Sun paradox: with the young Sun’s output at only 70 percent of its current output (see Subsection Evolution of the Sun), the early Earth would be expected to be completely frozen, but the early Earth seems to have had liquid water. The issue was raised by astronomers C. Sagan and G. Mullen in 1972 [<xref ref-type="bibr" rid="scirp.112406-ref38">38</xref>]. An unresolved question is how a climate suitable for life was maintained on Earth over the long timescale despite the variable solar output and wide range of terrestrial conditions [<xref ref-type="bibr" rid="scirp.112406-ref39">39</xref>]. Proposed resolutions of this paradox have taken into account greenhouse effects, changes to planetary albedo, astrophysical influences, or combinations of these suggestions.</p><p>In frames of WUM, the Upper mantle with Crust are due to DM core activity: the self-annihilation of DMPs in the DM core. As a result of this activity, a thickness of the Upper mantle with Crust is growing in time: the early Earth had a smaller thickness than it is in the present time. Hence, the temperature of the Earth’s surface was higher than its calculated temperature based on the Sun’s output at that time.</p><p>Expanding Earth hypothesis asserts that the position and relative movement of continents is at least partially due to the volume of Earth increasing. In 1888 I. O. Yarkovsky suggested that some sort of aether is absorbed within Earth and transformed into new chemical elements, forcing the celestial bodies to expand. The theses of O.C. Hilgenberg (1933, 1974) and N. Tesla (1935) were based on absorption and transformation of aether-energy into normal matter. In spite of the recognition of plate tectonics in the 1970s, scientific consensus has rejected any significant expansion or contraction of Earth [<xref ref-type="bibr" rid="scirp.112406-ref40">40</xref>].</p><p>In WUM, the Earth’s DM core absorbs new DMPs, and its size is increasing in time ∝ τ 1 / 2 . Hence, there is an expansion of DM core, and its surface (the Upper mantle with Crust) is likewise expanding. Due to DMPs self-annihilation, new chemical elements are created inside of the Upper mantle with Crust. As the result, the relative movement of continents is happening. The Medium of the World with DMPs are, in fact, some sort of aether proposed by Yarkovsky, Hilgenberg, and Tesla.</p></sec><sec id="s5"><title>5. Mars</title><p>NASA’s InSight mission landed on Mars on 26 November 2018. It aims to determine the interior structure, composition and thermal state of Mars, as well as constrain present-day seismicity and impact cratering rates. Such information is key to understanding the differentiation and subsequent thermal evolution of Mars. InSight lander learns Mars interior by monitoring “marsquakes” with magnitude not larger than around 4 on the Richter scale. Mars is just the third celestial body to have its core directly measured with seismic data, following Earth in the early 1900s and the Moon in 2011.</p><p>Mars is seismically active, with InSight recording over 450 marsquakes and related events in 2019 [<xref ref-type="bibr" rid="scirp.112406-ref41">41</xref>] [<xref ref-type="bibr" rid="scirp.112406-ref42">42</xref>]. In March 2021, NASA reported, based on measurements of over 500 Marsquakes that the core of Mars is liquid and has a radius of about 1830 km, more than half the radius of Mars and about half the size of the Earth’s core. This is significantly larger than models predicted, suggesting a core of lighter elements [<xref ref-type="bibr" rid="scirp.112406-ref43">43</xref>]. Average retrieved core density is 6 &#215; 10<sup>3</sup> kg⁄m<sup>3</sup>.</p><p>NASA researchers found that seismic waves must be bouncing off a boundary of ~1550 km beneath the surface: the dividing line between Mars’s solid mantle and its liquid core. The mantle between the crust and core has a single rocky layer. It is thinner than Earth’s and has a different composition which suggests that “two planets arose from different materials when they formed”. ETH Zurich geophysicist and study co-author A. Khan told that “this might be the simple explanation why we do not see plate tectonics on Mars”.</p><p>The crust of Mars 48 &#177; 24 km thick is likely highly enriched in radioactive elements that help to heat this layer at the expense of the interior. The crust is far more enriched with radioactive, heat-producing elements by a factor of 13 to 21 relative to the mantle beneath. This enrichment is greater than suggested by gamma-ray surface mapping and has a moderate-to-elevated surface heat flow. These results could help explain why its volcanoes show up at where they do despite the planet’s lack of global plate tectonics [<xref ref-type="bibr" rid="scirp.112406-ref44">44</xref>].</p><p>Analysis of the obtained experimental results show that:</p><p>&#183; Internal structure of the Mars is close enough to the structure of the Earth:</p><p>- Radius of Mars core relative to Mars radius is 0.54 (for Earth this ratio is 0.55);</p><p>- Relative thickness of the Mars mantle is 0.46 (for Earth this ratio is 0.45);</p><p>&#183; Composition of the Mars layers is significantly different from the composition of the Earth layers;</p><p>&#183; Average Mars core density 6 &#215; 10<sup>3</sup> kg⁄m<sup>3</sup> is significantly less than the average Earth core density 12 &#215; 10<sup>3</sup> kg⁄m<sup>3</sup>;</p><p>&#183; Seismic waves are bouncing off a boundary between Mars’s solid mantle and its liquid core. What is the cause of them?</p><p>&#183; Mars crust is far more enriched with radioactive, heat-producing elements by a factor of 13 to 21 relative to the mantle beneath. Where did they come from?</p><p>In frames of WUM, these questions can be answered the following way:</p><p>&#183; Seismic waves are generated by random mass ejections of the Mars DM core like deep-focus earthquakes, which are connected with random mass ejections of the Earth DM core happening at the 660-km boundary;</p><p>&#183; Mars crust is far more enriched with radioactive, heat-producing elements, which are produced within the Mars DM core as the result of DMPs self-annihilation. They arrive to the crust of Mars due to convection currents in the mantle carrying isotopes from the interior to the planet’s surface;</p><p>&#183; Significantly smaller Mars core density is important because the self-annihilation of DMPs depends on the density squared. It explains why the actual mean Mars surface temperature of 215 K is slightly higher than an effective temperature of 210 K due to the Sun’s heat [<xref ref-type="bibr" rid="scirp.112406-ref45">45</xref>]. At the same time, the actual mean Earth surface temperature of 288 K [<xref ref-type="bibr" rid="scirp.112406-ref33">33</xref>] is significantly higher than an effective temperature of 255 K due to the Sun’s heat [<xref ref-type="bibr" rid="scirp.112406-ref32">32</xref>].</p></sec><sec id="s6"><title>6. The Moon</title><p>The Moon is a differentiated body, being composed of a geochemically distinct crust, mantle, and planetary core. Based on geophysical techniques, the crust is estimated to be on average about 50 km thick. Moonquakes have been found to occur deep within the mantle of the Moon about 1000 km below the surface. Several lines of evidence imply that the lunar core is small, with a radius of about 350 km or less. The size of the lunar core is only about 20% the size of the Moon itself, in contrast to about 50% as is the case for most other terrestrial bodies. The composition of the lunar core is not well constrained, but most believe that it is composed of metallic iron alloy with a small amount of sulfur and nickel [<xref ref-type="bibr" rid="scirp.112406-ref46">46</xref>].</p><p>In 2010, a reanalysis of the old Apollo seismic data on the deep moonquakes using modern processing methods confirmed that the Moon has an iron rich core with a radius of 330 &#177; 20 km. The same reanalysis established that the solid Inner core made of pure iron has a radius of 240 &#177; 10 km. The core is surrounded by the partially (10 to 30%) melted layer of the Lower mantle with a radius of 480 &#177; 20 km (thickness ~150 km). These results imply that 40% of the core by volume has solidified. The density of the liquid outer core is about 5 &#215; 10<sup>3</sup> kg⁄m<sup>3</sup>. The temperature in the core is probably about 1600 - 1700 K [<xref ref-type="bibr" rid="scirp.112406-ref47">47</xref>].</p><p>In 2019, a reanalysis of nearly 50 years of data collected from the Lunar Laser Ranging experiment with lunar gravity field data from the GRAIL mission, shows that for a relaxed lunar fluid core with non-hydrostatic lithospheres, the core-mantle boundary has a radius 381 &#177; 12 km [<xref ref-type="bibr" rid="scirp.112406-ref48">48</xref>].</p><p>In WUM, the internal structure of the Moon can be explained the same way as it was done for the Earth and Mars. It is worth noting that the DM core of the Moon is much less than DM core of the Earth. This result is in good agreement with the proposed in our Model mechanism of the Moon creation: DM Core of the Moon was born as the result of the Rotational Fission of the Earth DM Core 4.57 billion years ago.</p></sec><sec id="s7"><title>7. Planets and Moons</title><p>Jupiter radiates more heat than it receives from the Sun [<xref ref-type="bibr" rid="scirp.112406-ref49">49</xref>]. Giant planets like Jupiter are hundreds of degrees warmer than current temperature models predict. Until now, the extremely warm temperatures observed in Jupiter’s atmosphere (about 970 C [<xref ref-type="bibr" rid="scirp.112406-ref50">50</xref>] ) have been difficult to explain, due to lack of a known heat source [<xref ref-type="bibr" rid="scirp.112406-ref11">11</xref>]. T. Guillot, et al. found that a deep interior of Jupiter rotates nearly as a rigid body, with differential rotation decreasing by at least an order of magnitude compared to the atmosphere [<xref ref-type="bibr" rid="scirp.112406-ref51">51</xref>].</p><p>Saturn radiates 2.5 times more energy than it receives from the Sun [<xref ref-type="bibr" rid="scirp.112406-ref52">52</xref>]. Despite consisting mostly of hydrogen and helium, most of Saturn’s mass is not in the gas phase, because hydrogen becomes a non-ideal liquid when the density is above 10 kg⁄m<sup>3</sup>, which is reached at a radius containing 99.9% of Saturn’s mass. The temperature, pressure, and density inside Saturn all rise steadily toward the core, which causes hydrogen to be a metal in the deeper layers [<xref ref-type="bibr" rid="scirp.112406-ref53">53</xref>].</p><p>Standard planetary models suggest that the interior of Saturn is similar to that of Jupiter, having a small rocky core surrounded by hydrogen and helium, with trace amounts of various volatiles [<xref ref-type="bibr" rid="scirp.112406-ref54">54</xref>]. This core is similar in composition to Earth but is denser. In 2004, scientists estimated that the core must be 9 - 22 times the mass of the Earth [<xref ref-type="bibr" rid="scirp.112406-ref55">55</xref>] [<xref ref-type="bibr" rid="scirp.112406-ref56">56</xref>], which corresponds to a diameter of about 25,000 km [<xref ref-type="bibr" rid="scirp.112406-ref57">57</xref>]. This is surrounded by a thicker liquid metallic hydrogen layer, followed by a liquid layer of helium-saturated molecular hydrogen that gradually transitions to a gas with increasing altitude. The outermost layer spans 1000 km and consists of gas. Saturn has a hot interior, reaching 11,700˚C at its core.</p><p>C. R. Mankovich and J. Fuller in the paper “A diffuse core in Saturn revealed by ring seismology” compare structural models with gravity and seismic measurements to show that the data can only be explained by a diffuse, stably stratified core-envelope transition region in Saturn extending to approximately 60% of the planet’s radius and containing approximately 17 Earth masses of ice and rock [<xref ref-type="bibr" rid="scirp.112406-ref58">58</xref>].</p><p>Uranus radiates 1.1 times more energy than it receives from the Sun [<xref ref-type="bibr" rid="scirp.112406-ref59">59</xref>]; Neptune—2.6 times [<xref ref-type="bibr" rid="scirp.112406-ref60">60</xref>]. The most fascinating result was obtained for the smallest gravitationally-rounded Macroobject—Mimas with a mean density 1.15 &#215; 10<sup>3</sup> kg⁄m<sup>3</sup> and the temperature ≈ 64 K. <xref ref-type="fig" rid="fig2">Figure 2</xref> illustrates the unexpected and bizarre pattern of daytime temperatures found on it. It is worth noting that the self-annihilation of DMPs inside of the Mimas DM core is efficient with the core density about 10<sup>3</sup> kg⁄m<sup>3</sup>, and the Mimas temperature is significantly higher than the effective temperature calculated based on the heat it receives from the Sun.</p><p>S. Kamata, et al. report that “many icy Solar System bodies possess subsurface oceans. To maintain an ocean, Pluto needs to retain heat inside”. Kamata, et al. show that “the presence of a thin layer of gas hydrates at the base of the ice shell can explain both the long-term survival of the ocean and the maintenance of shell thickness contrasts. Gas hydrates act as a thermal insulator, preventing the ocean from completely freezing while keeping the ice shell cold and immobile. The most likely guest gas is methane” [<xref ref-type="bibr" rid="scirp.112406-ref62">62</xref>].</p><p>According to WUM, the internal heating of all gravitationally-rounded Macroobjects of the Solar system is due to DMPs self-annihilation in their cores made up of DMPs (1.3 TeV). The amount of energy produced due to this process is sufficiently high to heat up the Macroobjects.</p></sec><sec id="s8"><title>8. Dark Matter Reactors</title><p>The following facts support the existence of Dark Matter Cores in Macroobjects:</p><p>&#183; E. Fossat, et al. found that Solar Core rotates 3.8 &#177; 0.1 faster than the surrounding envelope;</p><p>&#183; J. Zhang, et al. concluded that the Earth’s inner core is rotating faster than its surface by about 0.3 - 0.5 degrees per year;</p><p>&#183; T. Guillot, et al. found that a deep interior of Jupiter rotates nearly as a rigid body, with differential rotation decreasing by at least an order of magnitude compared to the atmosphere;</p><p>&#183; W. Wu, S. Ni, and J. Irving were surprised by just how rough the Earth’s 660-km boundary is—rougher than the surface layer that we all live on;</p><p>&#183; The variations of the Earth daylength throughout 2020 were in the range 86400 − 1.46   ms + 1.62   ms     s ;</p><p>&#183; D. C. Hoffman, et al. in 1971 obtained the first indication of Pu-244 present existence in Nature;</p><p>&#183; Giant planets like Jupiter are hundreds of degrees warmer than current temperature models predict. Saturn radiates 2.5 times more energy than it receives from the Sun; Uranus—1.1 times; Neptune—2.6 times;</p><p>&#183; Many Icy Solar system bodies including Pluto possess subsurface oceans.</p><p>The radiuses of the DM cores of different Macroobjects of SS are presented in <xref ref-type="table" rid="table3">Table 3</xref>.</p><p>In WUM, Macroobjects’ cores are essentially Dark Matter Reactors fueled by DMPs. All chemical elements, compositions, radiations are Homemade and produced by Macroobjects themselves as the result of DMPs self-annihilation. The diversity of all gravitationally-rounded Macroobjects in the Solar system is explained by the differences in their DM cores (mass, size, density, composition). The DM Reactors at their cores (including Earth) are very efficient and provide enough energy for the internal heating and all their geological processes like volcanos, quakes, mountains’ formation through tectonic forces or volcanism, tectonic plates’ movements, etc. All gravitationally-rounded Macroobjects in hydrostatic equilibrium, down to Mimas in Solar system, prove the validity of WUM.</p></sec><sec id="s9"><title>9. Conclusion</title><p>WUM does not attempt to explain all available cosmological data, as that is an impossible feat for any one article. Nor does WUM pretend to have built an all-encompassing theory that can be accepted as is. The Model needs significant further elaboration, but in its present shape, it can already serve as a basis for a new Cosmology proposed by Paul Dirac in 1937. The Model should be developed into a well-elaborated theory by the entire physical community. In our view, great experimental results and observations achieved by Astronomy in the</p><table-wrap id="table3" ><label><xref ref-type="table" rid="table3">Table 3</xref></label><caption><title> The radius of the DM core of the different Macroobjects in the Solar system</title></caption><table><tbody><thead><tr><th align="center" valign="middle" >Macroobject</th><th align="center" valign="middle" >Sun</th><th align="center" valign="middle" >Saturn</th><th align="center" valign="middle" >Earth</th><th align="center" valign="middle" >Mars</th><th align="center" valign="middle" >Moon</th><th align="center" valign="middle" >Mimas</th></tr></thead><tr><td align="center" valign="middle" >Radius, km &#215; 10<sup>3</sup></td><td align="center" valign="middle" >487</td><td align="center" valign="middle" >34.9</td><td align="center" valign="middle" >3.52</td><td align="center" valign="middle" >1.83</td><td align="center" valign="middle" >0.381</td><td align="center" valign="middle" >&lt;0.2</td></tr></tbody></table></table-wrap><p>last decades should be analyzed through the prism of a New Paradigm—Hypersphere World-Universe Model [<xref ref-type="bibr" rid="scirp.112406-ref1">1</xref>]. Solar System became Experimental Laboratory for astrophysicists to check their theories!</p></sec><sec id="s10"><title>Acknowledgements</title><p>Special thanks to my son Ilya Netchitailo who helped me refine the Model and improve its understanding.</p></sec><sec id="s11"><title>Conflicts of Interest</title><p>The author declares no conflicts of interest regarding the publication of this paper.</p></sec><sec id="s12"><title>Cite this paper</title><p>Netchitailo, V.S. (2021) Solar System. Angular Momentum. Dark Matter Reactors. Journal of High Energy Physics, Gravitation and Cosmology, 7, 1353-1372. https://doi.org/10.4236/jhepgc.2021.74084</p></sec></body><back><ref-list><title>References</title><ref id="scirp.112406-ref1"><label>1</label><mixed-citation publication-type="other" xlink:type="simple">Netchitailo, V.S. 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