Relay-Version: version B 2.10 5/3/83; site utzoo.UUCP Path: utzoo!mnetor!seismo!rochester!cornell!batcomputer!lorraine From: lorraine@batcomputer.tn.cornell.edu (Peter Lorraine) Newsgroups: sci.electronics,sci.physics Subject: Re: resistance of earth ground Message-ID: <1571@batcomputer.tn.cornell.edu> Date: Tue, 30-Jun-87 11:40:20 EDT Article-I.D.: batcompu.1571 Posted: Tue Jun 30 11:40:20 1987 Date-Received: Wed, 1-Jul-87 07:16:21 EDT References: <1315@cullvax.UUCP> Reply-To: lorraine@tcgould.tn.cornell.edu (Peter Lorraine) Organization: Cornell Theory Center, Cornell University, Ithaca NY Lines: 18 Keywords: potential differences, thunderstorms Summary: origins of large potential differences Xref: mnetor sci.electronics:880 sci.physics:1803 In a reply to the original question about the resistivity of the earth someone mentioned that enormous potentials exist across continental distances. What is the mechanism that generates these potentials? Is there a return current balancing the generation mechanism? I've heard that your typical (whatever a high school geography teacher meant 10 or so years back) lightning flash carries several coulombs. The electrostatic energy in a capacitor is 0.5CV**2. How much energy does the earth churn out each day moving charge around? As long as my mind wanders, can anyone think of a way to collect some of this energy? How about sticking superconducting rods from the ground up two or so miles and collecting current on a continuous basis? This is probably not very practical for some fairly obvious reason (other than the engineering ones :). Thank you, Peter Lorraine (lorraine @ tcgould.tn.cornell.edu)