...The atmosphere is not a perfect insulator, but has the property of conducting a very small amount of electricity. On a clear, windless day, the ground is negatively charged, and positive charges are distributed in the upper atmosphere, resulting in a vertical distribution of electric potential in the atmosphere, higher at the top and lower at the bottom. This is called the "atmospheric electric field," and the electric current (3× 10-13 A per m2) that flows from the upper layers to the ground is called the "air-ground current." The atmosphere is very weak but has electrical conductivity because charged particles called "atmospheric ions" exist in the atmosphere and move according to the electric potential difference. ... *Some of the terminology explanations that mention "air-ground current" are listed below. Source | Heibonsha World Encyclopedia 2nd Edition | Information |
…また大気は完全な絶縁体ではなく,ごくわずかであるが電流を通す性質をもち,晴天無風のとき,地表は負に帯電し,上層の大気中には正電荷が分布し,大気中では垂直に,上方が高く下方が低い電位の分布が生じている。これを〈大気電界〉とよび,このため上層から地表に向かって流れる電流(1m2当り3×10-13A)を〈空地電流〉という。大気が非常に微弱であるが導電率をもつのは,〈大気イオン〉とよばれる荷電粒子が大気中に存在し,電位差に応じて移動するためである。… ※「空地電流」について言及している用語解説の一部を掲載しています。 出典|株式会社平凡社世界大百科事典 第2版について | 情報 |
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