Recalculating the Mass of Earth The Bipartite Nature of Mass and the Recovery of Atomic Mass from Dodecahedral Quanta
This paper proposes a bipartite ontology of mass within an Info-Magneto-Electrostatic framework, arguing that the Earth's catalogued mass conceals distinct inert (Mahatva) and interactive (Gurutva) components derived from a viscous celestial plenum and dodecahedral quanta, thereby reinterpreting gravity as a plenum vortex pressure gradient rather than an intrinsic property of matter.
Original paper licensed under CC BY 4.0 (https://creativecommons.org/licenses/by/4.0/). This is an AI-generated explanation of the paper below. It is not written or endorsed by the authors. For technical accuracy, refer to the original paper. Read full disclaimer
The Great Cosmic Scale: Why Weighing the Earth is Trickier Than It Looks
Imagine trying to weigh a giant, spinning basketball that you can't touch, can't lift, and is floating in a vast, invisible ocean. That is essentially what scientists have been trying to do for centuries: figure out exactly how heavy the Earth is. In the world of physics, this falls under the study of gravity and mass. For a long time, we've treated mass as a single, simple thing: the amount of "stuff" inside an object. We also treat gravity as a mysterious pull that objects exert on each other across empty space. But here's the catch: to weigh the Earth, scientists have to use a specific number called Newton's gravitational constant (G). The problem is, nobody can agree on what that number actually is. It's like trying to bake a cake using a cup that keeps changing size every time you measure it. Because of this, the standard number we have for Earth's weight might be a bit fuzzy, and it might be hiding a deeper secret about what gravity actually is.
This paper, written by Dr. Satinder Singh Malik, asks a bold question: What if the Earth doesn't have just one mass, but two? And what if gravity isn't a pull at all, but a push? The author suggests that space isn't empty; it's filled with a real, fluid-like substance (called a "plenum") that acts like a cosmic ocean. In this view, the Earth isn't just sitting there; it's spinning inside a whirlpool of this invisible fluid. The paper argues that the "weight" we feel is actually the pressure of this fluid pushing on us, and the "mass" we calculate is a mix-up of two different things: the heavy, solid core of the planet and the thin, interactive skin that touches the fluid. By separating these two, the author recalculates the Earth's mass and suggests it's actually about 20% lighter than the textbooks say, while also explaining why the planet spins the way it does.
The Two Faces of the Earth: A Tale of Two Masses
So, how does this new way of looking at things work? Dr. Malik proposes that the Earth has a "bipartite" nature, meaning it has two distinct parts that play different roles. Think of the Earth like a heavy, dense bowling ball (the core) wrapped in a very thin, sticky layer of bubblegum (the surface).
1. The Heavy Core (Mahatva)
The first mass is the "inert nucleonic mass," or what the paper calls Mahatva. This is the actual, dense "stuff" of the Earth—the rocks, the iron core, the dirt. It's the heavy bowling ball. The paper calculates this mass to be 4.765 × 10²⁴ kg. This is about 20% less than the famous number you see in textbooks (5.972 × 10²⁴ kg). Why the difference? The author argues that the textbook number includes an "inflation" caused by the Earth's own gravity squeezing the planet tighter than it naturally wants to be. If you could take the Earth out of its own gravity and let it relax to a normal pressure, it would be lighter. This is the true amount of substance the planet contains.
2. The Sticky Skin (Gurutva)
The second mass is the "interactive cohesive mass," or Gurutva. This is the thin bubblegum layer. In this theory, gravity doesn't pull on the heavy core; it only grabs onto the outer electron clouds of the atoms, which act like a skin. This skin interacts with the invisible "ocean" of space (the plenum). The paper calculates this mass to be incredibly small: 9.59 × 10⁹ kg. That's tiny compared to the core! It's the only part of the Earth that the cosmic ocean actually "grips" to create what we feel as weight.
Gravity is a Push, Not a Pull
The most playful part of this theory is how it explains gravity. Usually, we think of gravity as a magnet pulling things down. But Dr. Malik suggests it's more like a crowd of people pushing you toward the center of a room. Imagine the Earth is a spinning fan in a pool of water. As it spins, it creates a whirlpool. The water (the plenum) swirls around the fan. If you drop a leaf into this whirlpool, the water doesn't "pull" the leaf; the water pressure pushes the leaf inward toward the center of the swirl.
In this paper, the "plenum" is a real, viscous fluid that fills all of space. Its density is numerically identical to a known electrical constant (the permittivity of free space), suggesting that electricity and gravity are two sides of the same coin. The Earth spins, dragging this fluid with it, creating a vortex. The "weight" you feel on a scale is just the pressure of this swirling fluid pushing down on your electron-skin.
The Mystery of the Spin: Who is the Driver?
Here is where the story gets even more interesting. The paper looks at the Earth's rotation (its spin). If the Earth were just a dead rock spinning in a fluid, the fluid's drag would eventually slow it down, and it would spin backward (retrograde) or very slowly. But the Earth spins fast and forward.
The author calculates that the Earth's spin is actually being driven by an external force: the Sun's magnetic field. It's like a cosmic motor. The Sun's magnetic field sweeps past the Earth, and this interaction pushes the Earth's core, keeping it spinning against the drag of the fluid. The paper calculates a "rotational inertia" of 1.41 × 10¹³ kg, which is the tiny amount of spin the local fluid could support on its own. The fact that the Earth spins much faster than this suggests that the Sun is constantly "refueling" the Earth's spin. This explains why the Earth hasn't stopped spinning over billions of years; it's an open machine, not a closed one.
The Quantum Puzzle: Why Two Masses?
To prove that mass really has two parts, the author dives down to the quantum level, looking at atoms. They use a geometric model where space is made of tiny, 12-sided shapes (rhombic dodecahedra) packed together like a honeycomb. They try to count how many of these "cells" make up a hydrogen atom.
When they try to count only the heavy nucleus (the proton), the math fails; the atom comes out too light. But when they count the proton as the heavy core and the electron as the light, interactive skin, the math works perfectly. The atom's mass is recovered exactly as an integer count of these space-cells. This suggests that mass is fundamentally "bipartite" (two-part) all the way down to the smallest scale: a heavy core and a light, interactive boundary.
What This Means for Us
The paper concludes that the single number we use for Earth's mass is a "conflation"—a messy mix-up of these two different physical realities, contaminated by a constant (G) that we can't measure precisely. By separating them, we get a clearer picture:
- The Earth is lighter in substance than we thought (4.765 × 10²⁴ kg).
- Gravity is a pressure gradient from a fluid ocean, not a pull.
- The Earth is an open system, constantly driven by the Sun's magnetism.
The author is careful to note that this is a speculative framework. It fits the data we have (like the orbits of satellites and the Moon) without needing the mysterious constant G, but it challenges our deepest assumptions about what space and mass are. It suggests that if we could measure the Earth without using the "broken cup" of Newton's constant, we would find a planet that is lighter, gripped only at its surface, and kept spinning by its star. The paper invites scientists to test these ideas, perhaps by looking for tiny differences in how light travels vertically versus horizontally, or by checking if the gravitational constant changes as the Earth's day length fluctuates. Until then, the Earth remains a mystery, spinning in a fluid sea, with a mass that might be two things at once.
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