A b s t r a c t. Stress responses of spring rape to soil hypoxia were investigated during 8-days flooding. Soil air-filled porosity decreased from 25-30% to 0%, oxygen diffusion rate -from 2.6-3.5 to 0.34 µmol O 2 m -2 s -1, and redox potential -from 460 to 150 mV within few hours. Alcohol dehydrogenase activity in roots increased up to 7-fold after one day of flooding and then decreased to 170% of control. Superoxide dismutase activity in roots increased by 27% during first 3 days and then dropped to 60% of control; in the leaves superoxide dismutase activity increased in average by 44%. Ascorbate peroxidase activity in leaves increased by 37% during first 3 days and then decreased to control value. Glutathione reductase activity increased by 45% in roots of flooded plants but did not change in leaves. Proline concentration in leaves increased up to 4-fold on the 3d day of flooding and then decreased to control value. Thus soil flooding induces increase of alcohol dehydrogenase activity and subsequent increase of superoxide dismutase and glutathione reductase activities in roots while the leaves display a few days increase of free proline concentration and ascorbate peroxidase activity, and a long-term increase of superoxide dismutase activity.K e y w o r d s: spring rape, flooding, oxygen diffusion rate, redox potential, enzyme activity INTRODUCTION Soil flooding changes subsurface plant gas exchange. The low diffusion rate of oxygen in water-filled pore space of the soil results in limitation of oxygen availability for plant roots and soil microorganisms and leads to a switch of aerobic metabolism of plant roots into less efficient anaerobic fermentation, causing a fast depletion of carbohydrate reserves. Hypoxic conditions in soil cause also a decrease of Eh (Balakhnina et al., 2009(Balakhnina et al., , 2010 Gliñski and Stêpniewski, 1985;Bailey-Serres and Voesenek, 2008). This, in turn, stimulates evolution of carbon dioxide, molecular hydrogen, hydrogen sulphide, ethylene, and methane and accumulation in the soil of reduced phytotoxins (Fe 2+ , Mn 2+ , sulfide and, at high concentrations, ammonium) which can have a negative impact on plants, causing, among others, growth retardation, reduction in leaf size, wilting of shoots and necrosis (Lucassen et al., 2002; Smith and Restal, 2006). Plant adaptation to soil hypoxia includes series of interconnected reactions directed to survival during the periods of hypoxic and anoxic conditions and to the homeostasis maintenance. Anatomical and morphological changes help to provide oxygen to the plant tissues (Colmer, 2003;Pederson et al., 2009;Vartapetian et al., 2003).In connection with the specificity of the effect of hypoxia on plants, of special interest are compensatory changes connected with transformations of respiration pathways. Under oxygen deficiency most plants exhibit intensification of glycolysis accompanied with accumulation of lactate and ethanol (Rocha et al., 2010). Under prolonged and deep hypoxic stress the formation of ethanol prevails. Pr...