Experimental Verification of Anomalous Forces on Shielded Symmetrical Capacitors

Elio B Porcelli,Omar R Alves,Victo S Filho

doi:10.5539/apr.v12n2p33

Abstract

In this work, we measured the magnitude of forces raised from the operation of symmetrical capacitor devices working in high electric potentials. Our experimental measurements were realized with basis on an improved setup which aimed significant reduction of ionic wind by means of an efficient shield. We observed small variations of the device inertia within an accurate range and we confirmed with good accuracy that the experimental results can be explained by a generalized quantum entanglement hypothesis which provides us a theoretical model for a macroscopic dipole force raised by the myriad of microscopic dipoles constituting the capacitor. The new results corroborated the positive results of previous experiments and also indicate the validity of our theoretical forecast.

Highlights

1.1 Outline of the PhenomenonIt is well known since 1928 (Brown, 1928, 1965; Williams, 1983) that an anomalous phenomenon involving weight variation measurements occurs in experiments in which parallel plate capacitor devices are subjected to high voltage
We present an experimental investigation of the existence and magnitude of anomalous forces on shielded symmetrical capacitors, operating in high voltage
Our experimental measurements indicated the presence of small but persistent weight losses or an upward force acting on the capacitor in the scale of mgf for different values of the high voltage applied on the capacitors

Summary

Introduction

It is well known since 1928 (Brown, 1928, 1965; Williams, 1983) that an anomalous phenomenon involving weight variation measurements occurs in experiments in which parallel plate capacitor devices are subjected to high voltage. Other experiments described in Refs (Buehler, 2004; Musha, 2008; Musha, 2014) showed that insulating materials around the capacitor devices could not eliminate such forces They could not be explained from the electromagnetic interaction or fields of the Earth due to the inconsistency with the magnitude of the upward force

Methods

Results

Conclusion