IntroductionSeveral phosphatases are involved in the hydrolysis of organic P compounds but the major role in the organic phosphorus mineralization process is attributed to the phosphomonoesterases. Acid phosphomonoesterase enzymes are the dominant group of enzymes involved in organic P mineralization in acidic soils [1]. These enzymes are produced mainly by plants and fungi and to a lesser degree by bacteria. The level of acid phosphomonoesterase secreted by plant roots has been shown to differ significantly between species, with N-fixing plants (legumes) secreting more phosphomonoesterase enzymes than cereals [2]. Plant available P (P AVAIL ) concentration also increases in soils underlying plantations of N-fixing trees [1], probably due to a higher P requirement by N-fixing plants [3]. The relationship between the available P concentration and phosphatase activity is usually very complex, since a positive, a negative or no relationship between these two parameters is possible [1,4]. There are studies which show that phosphatase activity is inversely proportional to the P AVAIL concentration [5], which confirms the thesis that the production and activity of soil phosphatases, especially the acid form, is connected with the demand of microorganisms and plants for P. Phosphatases are typical adaptive enzymes and their activity increases when plant available P concentration decreases. Kinetics studies indicate that orthophosphate ions, which are the product of the reaction conducted by the phosphatases, are competitive inhibitors of their activity in soil [6]. Other studies have found a significant positive correlation between phosphatase activity and available P concentration. Generally, a significant and positive relationship between phosphatase activity and P availability [7] is obtained in unfertilized soils or/ and those with a low content of nutrients, where P deficiency occurs. On the contrary, in soil where P fertilizers are applied and/ or in naturally fertile soil a significant but negative relationship between both of these parameters can be observed [4].It is a well known fact that trees can alter soil conditions, thus influencing ecological processes such as secondary succession and plant migration. Black alder [Alnus glutinosa (L.) Gaertn.] can have a great impact on its habitats and can form a symbiosis with Frankia and with ectomycorrhizal fungi. The actinobacteria provide the tree with N fixed from the atmosphere, whereas mycorrhizal fungi provide P and other nutrients [8], and on the other hand alders provide energy to microsymbionts [9]. Therefore, they play an important role
AbstractBlack alder, an N-fixing tree is considered to accelerate the availability of phosphorus in soils due to the increased production of phosphatase enzymes, which are responsible for the P release from the litter. Acid phosphatase activity plays a pivotal role in organic P mineralization in forest soils and in making P available to plants. In order to check whether Alnus glutinosa stimulates acid phosphomonoesterase (P...