An Electrical Crevasse Detector. John C. Cook Geophysics, Vol. 21, No. 4, 1956, p. 1055–70, 9 figs. (1957)

the V.S. Army sponsored several efforts to find a suitable method of detecting crevasses, and the only promising one was that developed by Mr. Cook at the Southwest Research Institute (" a as).The latest form of the detector, whose early development is described in the above article, is being used by thl: Americans on a snow vehicle in the Antarctic.Long interconnected booms extend forwa rd in front of the vehicle and slide four large spherical sectors of polished m etal across the snow surface.The .. pherical sectors are electrodes making good contact with the snow, two feed in an audio-frequen..:y current and the potential across the other pair is continuously recorded inside the vehicle.If the input is kept constant, the measured potential is a function of the effective impedance (mainly capacitance according to the author) of the underlying snow and ice.Hence any anomaly in the snow, su ch as the air void of a crevasse or a change in the density and structure of the snow, produces a change in the output voltage.The m ethod is similar, as the author indicates, to some of the methods of electrical surveying of the ground, but its development and application for snow surveying is novel.With a snow surface there is the considerable advantage of being able to slide the electrodes across the surfaces to obtain a continuous record of the background variation and thus of picking out the crevasse anomalies more readily.An approximate theoretical solution is given of the voltages and currents for a system of four hemispherical electrodes equally spaced in a line on the snow surface.The snow or ice is considered to be a dielectric and there is no crevasse.The solution is very approximate, as the author states, for the input needed to produce a given output was several times greater in practice than the theory predicts.Perhaps the dielectric constant is in error.The first field trials were made in the summer of 1955 on the Greenland Ice Sheet.Both stationary and mobile tests were carried out, using sheet metal sledges 4 ft.(1'2 m.) square as electrodes.The stationary test on melting snow used an input of 200 volts and l ' 5 milliamps.at 400 cycles per sec.and gave a signal of 0'5 volt with an electrode spacing of 35 feet (II m.).Over 250 miles (400 km.) were traversed at speeds from 2 to 20 miles (3 to 30 km.) per hour.using a "weasel" as one electrode.The electrode spacing was 20 ft.(6 m.).Several traces of the output against distance are illustrated, and the crevasse anomalies are well defined.Output profiles were reproducible, known crevasses 4 to 20 ft.(1'2 to 6 m.) wide were revealed and others were found.Attempts were then made to obtain the optimum conditions for detection.Several hundred traverses were made of selected crevasses with electrodes in different arrays and spacings and at different electrical frequencies.Electrode spacings of 7 to 180 ft.(2'1 to 55 m.) were used successfully.The shortest spread giving good discrimination between the crevasse anomaly and background variations had unequal spacings of 20 , 40 ~"1 d 20 ft.(6, 12 and 6 m.) between the four electrodes.For short spacings, electrodes in a line moving broadside on to a crevasse gave double the anomaly of the electrodes moving in line across the crevasse.The best frequency on wet snow was 200 cycles per sec.but on dry snow 60 cycles per sec.or less was best.The best anomalies were obtained at sub-freezing temperatures, but dry snow produced frictional "noise" amounting to 0'2 volt at 20 miles (30 km.) per hour.A small portable headphone detector for use with a skier was also tried out.The skier is the leading electrode and the other three electrodes are towed behind.The skier might be used to safeguard a heavier vehicle following him, but not himself.