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leolaw
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How come the Earth is negatively charged?
from http://nofc.cfs.nrcan.gc.ca/science/research/lightning_e.htmlWhat is the Earth's charge?
The Earth is electrically charged and acts as a spherical capacitor. The Earth has a net negative charge of about a million coulombs, while an equal and positive charge resides in the atmosphere.
The electrical resistivity of the atmosphere decreases with height to an altitude of about 48 kilometres (km), where the resistivity becomes more-or-less constant. This region is known as the electrosphere. There is about a 300 000 volt (V) potential difference between the Earth's surface and the electrosphere, which gives an average electric field strength of about 6 V/metre (m) throughout the atmosphere. Near the surface, the fine-weather electric field strength is about 100 V/m.
Earth's negative charge refers to the presence of a large number of negatively charged particles, such as electrons, on its surface and in its atmosphere.
The main cause of Earth's negative charge is the continuous bombardment of the planet by high-energy particles from the sun, known as solar wind. These particles strip electrons from atoms in Earth's upper atmosphere, creating a negative charge.
The negative charge on Earth can have a variety of effects, including influencing weather patterns, creating electric fields in the atmosphere, and contributing to the formation of lightning and other electrical phenomena.
Scientists use a variety of instruments, such as satellites, ground-based sensors, and weather balloons, to study Earth's negative charge. They also conduct experiments in controlled environments to better understand the processes that contribute to the planet's negative charge.
While there has been some research on harnessing the energy from lightning strikes, it is currently not possible to directly harness Earth's negative charge for energy. However, understanding the processes that create and maintain the planet's negative charge can help us develop more efficient and sustainable energy sources in the future.