Large amounts of DU material has been released to the environment in Kosovo and Kuwait due to the use of depleted uranium (DU) ammunition during the 1991 Gulf war and the 1999 Balkan conflict. Following the impact of metallic DU penetrators on solid targets, DU particles are dispersed and ignited, and uranium in the particles is oxidized. Following inhalation or ingestion of DU particles, the amount of DU that is absorbed into the blood and distributed to tissues and organs will largely depend on the particle size distribution and associated weathering rates (solubility) both in the respiratory system as well as the GI tract. Particle weathering rates are related to particle characteristics such as specific surface area, size distribution, elemental composition, U oxidation states and crystallographic structure.In order to improve the basis for health impact assessments related to contamination of DU in Ceja Mountains, Kosovo and Al Doha, Um Al Kwaty as well as Manageesh Oil fields in Kuwait, DU particles originating from these sites have been isolated and characterised in detail using advanced analytical techniques. Information on particle size, surface structure and surface elemental distribution were obtained by means of electron microscopy, whereas elemental distribution, oxidation state and crystallographic structure of U were determined using synchrotron radiation (SR) based x-ray microscopic techniques. Inductively Coupled Plasma Mass Spectrometry (ICP-MS) and Accelerator Mass Spectrometry (AMS) were employed to obtain U isotope ratios for source identification purposes.Characteristics of DU particles in soil/sand from Kosovo and Kuwait contaminated during the Balkan conflict and Gulf war varied significantly depending on the release scenario. Atom ratios ( 236 U/ 235 U) obtained from ICP-MS and AMS varied between individual particles, but demonstrated that U in the DU-particles originated from reprocessed fuel. The bright yellow, highly oxidised DU particles associated with a fire in a DU ammunition storage facility showed a wide particle size distribution; from submicron to several O.C. LIND ET AL. 58 hundred micrometers. Furthermore, the micro-XRD signals closely resembled those of schoepite, dehydrated schoepite and metaschoepite. DU in sand samples contaminated with these particles is expected to dissolve quite rapidly in biological fluids. In contrast, the potential mobility of smaller and less oxidised DU particles, originating from the corrosion of DU penetrators or collected in tanks hit by DU ammunition should be significantly lower. The presence of respiratory DU particles where U is more oxidised than UO 2 , and exhibiting high weathering rates, reflects that DU particles are potentially more bioavailable than natural uranium. Thus, environmental or health impact assessments for areas affected by DU ammunitions should take into account oxidation states, their corresponding weathering rates and the subsequent mobilisation of U from oxidized DU particles.