Both saline and alkaline stresses involve osmotic stress and ion injury; however, alkaline stress involves the stress due to a high pH. The aim of this study was to evaluate the physiological responses of linseed seeds and seedlings to saline and alkaline stresses and to elucidate the adaptive mechanisms involved. Stresses were generated by exposure to neutral saline solutions of saline stress and alkaline stress for 7 days. The relative growth rate (RGR) and water content (WC) of linseed seedlings were scarcely affected by salinity stress, but significantly reduced by alkaline stress. Photosynthetic activity and pigment indices were hardly changed under saline stress but were inhibited by alkaline stress. This implies that alkaline stress may be mediated by Na + uptake and accumulation up to toxic levels, leading to a decrease in photosynthetic pigments and damage to the photosynthetic apparatus. Alkaline stress causes precipitation of phosphate and metal ions which causes a sharp decrease in ionic activity and in the concentrations of various other ions. The results indicated that carbohydrates and proline synthesis decreased osmotic potential, remedied the shortage of inorganic anions and maintained stability of the intracellular pH allowing the plant to cope with osmotic stress from a high Na + vacuolar concentrations. However, the contribution of betaine to osmotic adjustment was small in linseed seedlings. With increasing solution concentrations, the rate of germination of linseeds was more severely inhibited under alkaline stress than under saline stress.Key words: Alkaline stress, Linseed, Saline stress.Over the last 300 years, since the beginning of the industrial revolution, our unbridled exploitation of the world's natural resources has severely damaged its vegetation and has also resulted in worrying accumulations of industrial wastes and greenhouse gases. Together, these have upset many natural ecosystem balances and have created many global environmental and climatic problems, including rising sea and air temperatures, rising sea levels, increasing desertification, severe erosion and soil loss, soil salinization and damaging accumulations of soil nitrogen (Abrol et al., 1988;Richards, 1990;Rengasamy, 2002). With widespread use of low-grade water for irrigation, soil salinization has also come into especially sharp focus. Somewhat over 60% of the world's arable land is now affected by salinity to some degree and this inhibits crop growth and lowers productivity and can even kill crops (Allakhverdiev et al., 2000;Munns, 2002).In naturally saline/alkaline soils, the main salts responsible are NaCl, Na 2 SO 4 , NaHCO 3 and Na 2 CO 3 , so the predominant ions are Na2-and NO 3 - (Kawanabe and Zhu, 1991;Tanji, 2002). Based on the particular mix of salts present in the soil at any site, natural salt stress has been classified into neutral salt-stress, alkaline salt-stress and mixed salt-stress. Saline stress generally involves two stresses -osmotic stress and ion injury stress, whereas alkaline s...