THE MALTA COSMOLOGY TEMPLATE

Chapter 05 - Darkmatter

PARTS

Darkmatter Selfproofs

SELFPROOF 0503 – UNDUE DENSITY OF MERCURY

• Mercury's density is the second highest in the Solar System at 5.427 g/cm³, only slightly less than Earth's density of 5.515 g/cm³. If the effect of gravitational compression were to be factored out from both planets, the materials of which Mercury is made would be denser than those of Earth, with an uncompressed density of 5.3 g/cm³ versus Earth's 4.4 g/cm³. Mercury's density can be used to infer details of its inner structure. Although Earth's high density results appreciably from gravitational compression, particularly at the core, Mercury is much smaller and its inner regions are not as compressed. Therefore, for it to have such a high density, its core must be large and rich in iron. (Wikipedia 04 June 2013)

• 0502-02:     That many blackholes are within the gravitonospheric gravitonstreams of larger objects.

• Quarks are small blackholes:  see Chapter 7 (Electrons) and Chapter 8 (Nucleons).
• Quarks consist of a gravitoncore, a gravitonocean, and a gravitonosphere.
• Electrons consist of two quarks, one axial and one centrifugal.
• Nucleons consist of three quarks of two different types, axial and centrifugal.   
• Atoms consist of nucleons and electrons in combination.
• Thus atoms consist of a core of blackholes surrounded by a gravitonosphere.
• Atoms, when solidbonded to others of their ilk, are held together by gravity and held apart by their gravitonospheres.

• The planet Mercury is a blackhole composite consisting of a core of solidbonded atoms
• Solidbonded atoms abide by the one percent rule. 
• Per the one percent rule, the atom core of planet Mercury consists of 1% gravitoncore and 99% gravitonocean/gravitonosphere. 

• The orbit of Mercury is within the Sun's gravitonospheric disc.
• The gravitonospheric disc is a dense and fast moving gravitonstream rising from the Sun's equator.
• Being in the gravitonospheric disk has three consequences:  

• CONSEQUENCE 1:     Some of the gravitons of the gravitonospheric disc strike the gravitoncores of Mercury's atoms and exchange spinspeed, thus pushing Mercury outward and precessing its orbit (see Selfproof 0502).  

• CONSEQUENCE 2:     Some of the gravitons of the gravitonospheric disc strike the gravitons in the gravitonospheres of Mercury's atoms, exchanging spinspeed and thus differentially raising both the vergence velocity and the escape velocity of the atom gravitonospheres.

• The additional gravitons understabilise the atom's gravitonosphere because the vergence velocity increases more than the escape velocity. 
• Increasing vergence velocity more than escape velocity means that the atom gravitonospheres differentially lose more energy than mass as they restabilise.
• Differentially losing more energy than mass reduces the rejectivity of the atom's gravitonospheres.
• Reducing the rejectivity of the atom gravitonospheres allows the atoms to close up.
• Closing up the solidbonded atoms increases the number of atoms in a given area.
• Increasing the number of atoms in a given area equates to increasing Mercury's density. 

• CONSEQUENCE 3:     Some of the gravitons of the gravitonospheric disc pass right through Mercury without striking anything and thus the only effect they have on the planet is gravitational:  the graviton's gravitypull moves from one side of the planet to the other. This effect shows in the planets precession.