John About fifteen years ago I went to a non-classified briefing about a land version of a gravity gradiometer. The Defense Mapping Agency had it. It was in a Winabago of some sort and had three disks that rotated at a fairly low rpm, a few Hz at most. The disks were less than a meter in diameter. The disks had two accelerometers on them. The acceleration as a function of position of the two accelerometers was reccorded and some sort of auto-correlation or FFT was done to get the direction and magnitude of the gradient. It was cute. Tom Schmitt tschmitt@.............. ----- Original Message ----- From: John HernlundTo: Sent: Saturday, April 29, 2000 10:58 PM Subject: Re: Article on gravimeters > > George Bush > > George, > There was a horribly written article about an incredibly interesting > subject a few years back in Scientific American. Even though the article did > not belong in the magazine, you might be interested in reading it. It was > about a gravity gradiometer that had been designed to help submarines "see" > the topography on the ocean floor and avoid collision with sea mounts. They > needed a passive method to see the ocean floor so that they would not be > detected. Supposedly this thing worked great (too bad all the data they > collected is classified). Anyways, the company that made it was allowed to > contract its use out to some geophysical concerns, such as finding oil and > natural gas resevoirs. The company takes a huge amount of money, throws this > thing in a boat and drives around for a while. They take the data, reduce it, > and then sell portions of it for commercial use. Nobody is allowed to buy > one of these instruments, or use one for themselves. This is the reason it > did not belong in the magazine: it was really an ad for the company. The > exact technology is still classified, so it is like a magical black box. > > Anyways, this device produces higher resolution images for finding density > anomalies than seismic methods, and does not require a whole lot of fancy > deployment except for position tracking and recording instruments, and so is a > lot easier to use than seismic arrays. I found this hard to believe when I > first heard it, but then again I was only used to absolute vertical gravity > measurements. So I had to find out about it a little further. > > The gravity gradient is the change in the gravity for each direction (down, > east, north) within a given distance and with respect to each direction. So > the downward component of gravity changes differently in the down, east and > west directions, and likewise for the east and north components of gravity. > This makes nine different combinations of gradients that can be examined. One > of those nine components can tell you an awful lot more than an absolute > gravity measurement, so just imagine having nine of them. Well, it turns out > that some of the components are equal, and the total number of unique > components is reduced to six. For example, the change in the down component > of gravity with respect to north is equal to the change in the north component > of gravity with respect to the down direction. In addition, the three terms > where the component changes in each of its directions is regulated by the fact > that a gravitational field is divergenceless, which means these three > gradients must sum to 0. So that makes five unique components, from which the > other four can be determined. All nine components are referred to as the > "gravity gradient tensor." > > This machine is supposed to have rotatiing parts and sensors inside some > kind of black spherical shell. It is very mysterious, and I would love to see > inside one some day. I am sure everyone else would be interested too... I > guess I would have to hijack one of their ships or something if I wanted to > get it, but that won't happen any time soon. Perhaps the PSN could mount an > expedition, and the media would try and figure out if PSN stood for some kind > of terrorist organization or something. > > Anyhow, enjoy! > > John Hernlund > E-mail: hernlund@....... > WWW: http://www.public.asu.edu/~hernlund/ > > **************************************************************************** ** > > __________________________________________________________ > > Public Seismic Network Mailing List (PSN-L) > > To leave this list email PSN-L-REQUEST@.............. with > the body of the message (first line only): unsubscribe > See http://www.seismicnet.com/maillist.html for more information. __________________________________________________________ Public Seismic Network Mailing List (PSN-L)
Larry Cochrane <cochrane@..............>