The purpose of this thesis was to examine the practical application and research potential of magnetometry as a method in applied geophysics. The work connects theoretical foundations with an experimental analysis of magnetometer use, focusing on the acquisition and interpretation of relevant data. A magnetometer enables the detection of magnetic anomalies, which may indicate the presence of buried objects or subsurface structures and reveal their physical properties. The aim of the research was to assess the effectiveness of the device in locating metallic objects, analyze the influence of their chemical composition on the detected anomalies, and verify or disprove the stated hypothesis. Anomalies or deviations from baseline values, result from differences in the physical and chemical properties of the objects and their surroundings and are expressed as contrasts in the geomagnetic field. The magnetometer detects them only if the objects are within its detection range, as it records local changes caused by material interactions with the geomagnetic field.
The experiment was based on systematic measurements conducted within a designated area, where various metallic objects were randomly buried and subsequently detected using the Rover C4 magnetometer by OKM. The objective was to collect data, analyze it, and test the hypothesis. This allowed for the verification of physical principles and a deeper understanding of magnetic phenomena in a natural setting. The study opens opportunities for further research, methodological refinement, and the development of new practical approaches.
The results indicate that object detection was relatively unreliable, yet the anomalies observed corresponded to the material composition size and location of the buried items. Metallic objects produce diverse responses, which generally allow for differentiation, although this depends on environmental and technical measurement conditions. In conclusion, the findings from research partially confirm the hypothesis that the magnetometer is an effective tool for detecting buried metallic objects. The method proved useful for mapping subsurface structures in geoscience, archaeology, engineering, and environmental monitoring, and shows potential in treasure hunting—especially for gold—where the Rover C4 proved to be a highly effective instrument.
|