This thesis is the result of a four year work on investigations regarding the use of nuclear measurement techniques for subsea fluid characterization. This thesis consists of a total of five papers, an introductory part with a detailed background and motivation of the current work as well as a presentation of the main results of the current work.In 2003, research on the SOFA (Subsea Online Fluid Analyzer) concept was initiated by the Christian Michelsen Research AS in cooperation with the Department of Physics and Technology at the University of Bergen. The ultimate goal of the SOFA concept is to be able to characterize all of the components that may be found in a subsea hydrocarbon multiphase flow through utilizing multi-modality measurements. It also includes a module based on gamma-ray dual modality densitometry (DMD) for the characterization of produced water samples. The first part of the work presented in this thesis focuses on further improvements of the DMD measurement setup employed in the SOFA concept. This was done through experimental and Monte Carlo (MC) investigations of the feasibility of utilizing gas-filled Geiger-Müller (GM) counters for the detection of transmitted and scattered gamma-rays.The DMD measurements alone are, however, not sufficiently sensitive to provide useful compositional information on produced water samples unless these are combined with other measurement modalities such as ultrasound and electrical conductivity measurements. The second part of the thesis, therefore, focuses on the experimental and MC work conducted in order to study the feasibility of applying the PGNAA (Prompt Gamma-ray Neutron Activation Analysis) method in conjunction with the MCLLS (Monte Carlo Library Least-Squares) approach for the characterization of produced water samples. It would not have been possible to accomplish this work without very much appreciated help from people who have shown a great deal of interest, and provided a great deal of help. First of all, I would like to thank my supervisors Prof.