VERFAHREN ZUM ORTEN VON OBJEKTEN IN FORM VON GASAUSTRITTEN AN DER ERDOBERFLÄCHE

摘要

Method wherein multiple thermograms are recorded in a localization phase at different predefined times over a long time period. The thermograms are subtracted from each other on a pixel by pixel basis. A location or locations with the lowest differential temperature values is determined and a multitude of differential themograms stored. The locations in the different thermograms are compared to see if there is any correspondence. If there is significant local correspondence of lowest differential temperature values these are classed as first grade discovery locations, while those with no correspondence are classed as second grade.