The Gamma Isotope Mapping System (GIMS) has two main components. The first component is a stainless steel sled that is towed on the seafloor by a survey vessel. The second component is the shipboard electronics. The sled houses a gamma radiation detector and battery pack. As the sled is towed along the seafloor at approximately 3 knots, the detector measures the natural gamma radioactivity of the surface sediment. The signal from the detector is sent by armored cable to the ship. The gamma signal is received and processed by a spectrometer mounted in the electronics package. The gamma radiation data, along with time, latitude, longitude, and water depth is logged automatically at 60 second intervals on a computer diskette. During the survey, two- and three-dimensional maps are created with the collected data. These maps show the differences in the sediment seafloor lithology. This data can be used in the location of surface mineral deposits on the seafloor or to track sediment distribution as a result of disposal activities during dredging operations from near-shore environments. Since the results are obtained during the survey, additional studies can proceed immediately after the GIMS survey allowing for a more economical merging of various studies. INTRODUCTION Due to the vast regions of the unknown marine environment, a method for rapidly exploring and mapping the surface lithology would be very useful to geologists and environmentalists. In addition to this, the ability to have the final results displayed in two- and three-dimensional maps immediately after the region is covered would be extremely helpful. The gamma detection sled was originally developed during the early 1970's for mineral exploration (Noakes et al, 1974). It was tested off the Georgia-South Carolina coast in an exploration effort to locate phosphate deposits (Harding & Noakes, 1976). Several anomalous areas were detected during the offshore exploration efforts. Sampling of the anomalies indicated that these areas consisted of heavy mineral sands and phosphatic material. The general design of the sled performed extremely well with little damage due to the abrasive nature of the seafloor. The system proved it's capabilities to detect changes in the bottom lithology during the testing in the 1970's with the location of heavy minerals and phosphatic deposits. This led to the possibility of using the gamma sled for tracking and mapping the changes in the seafloor lithology; not for minerals, but for environmental purposes. The Environmental Protection Agency (EPA) monitors all of the Ocean Dredged Material Disposal Sites (ODMDS) located directly offshore the coastal regions of the United States. In the past, the primary methods used to monitor the sites were sediment traps, box coring devices, biological sampling, and diver collected samples. All of these methods required considerable amounts of time and manpower to survey one ODMDS which can cover an average of 52 km2. Data collected over a long period of time are no longer representative of the current condition due to the effects of ocean currents and storms.

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Characteristic x rays have been produced for a variety of samples by bombardment with protons in the energy range from 75 keV to 5 MeV. The experiments were performed with two accelerators. For the low-energy studies (less than 150 keV), a Cockcroft-Walton accelerator was used. The higher-energy studies were done with a 5 MV Van de Graaff. The x rays were measured with high-resolution Si(Li) and Ge(Li) detectors. Yields for the cross section of characteristic K- and L-shell ionizations were measured for titanium, vanadium, chromium, manganeses iron, cobalt, nickel, copper, silver, gold, bismuth, and uranium. The experimental cross-sections have been compared to the theoretical predictions of the Born approximation for an interaction of this type.Trace element analysis by 4-MeV proton bombardment of samples in the 10-12 gm range has also been performed. Some comments with regard to analysis with these sensitivities will be made.

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