Starting with a hypothesis and then collecting evidence to support that we have the ability to reverse polarization of electrons with terabytes of adhesions to neutrons’ with an electrical charge that the state of existence changes. Oh we have suspected that but never really had much success speeding up the impact of atoms, molecules with constant neutron pounding but not to the point where atoms collide. They simply reverse polarization, even simpler is to take two of the same fields in a magnet. The repel from each other.
How to accomplish this on a large scale is the tricky part but not impossible with critical thinking, not experimental data. Analysis and concepts form the heart of the work concentrates on principles: it states the lessons learned from previous attempts.
We can take an optical terabyte drive and suspend it within a reversed polarization field and it will never crash. Being able to do so now allows us to fully concentrate on how to repel a huge object carrying a cargo of several humans to outer space within seconds. ( it does not cost much at all)
Sweet dreams are made of geomagnetic activity. Most geophysicists agree that the main component of Earth’s magnetic field is generated by convection currents in the molten iron of the planet’s core. This dipole field — which defines the Earth’s magnetic poles — have reversed polarity tens of thousands of times in the past. We know this because ancient field configurations are “frozen” into the rocks, as magnetic particles align with field lines. Various theories have been put forward to explain the reversal mechanism but they are usually highly complex, where random variations in the flow of the liquid core are the main triggers. A geomagnetic field reversal takes approximately 10, 000 years — a very short period on a geological timescale — during which time, the field drops to approximately 10 percent of its normal intensity. In previous models, fluctuations in the flow of molten iron “switch off” the main dipole component and then regenerate it with the opposite polarity. But I have found a way to speed it up.
I can explain it all if you have about three days.
Koz