The Relationship of the Processes in the Rhizosphere of CommonReed Phragmites australis, (CAV.) TRIN. ex STEUDEL to Water Fluctuation key words: water level fluctuation, reed stand, ETS-activity, inorganic nutrients, soil water.
AbstractIntermittent Lake Cerknica is characterised by extreme water level fluctuations. It is neither a lake, nor a terrestrial ecosystem. The decomposition processes in the rhizosphere of extended reed stands are essential for the entire ecosystem. The influence of intermittent water regime on the microbial activity and availability of nutrients in the rhizosphere in a terrestrial reed stand was investigated. The measurements revealed a relatively high soil water content, that was not related to underground water table. Mineralization processes in a soil profile were estimated by measuring microbial activity as electron transport system (ETS) activity and by nutrients in soil water. The microbial activity was determined in the whole depth profile. The highest ETS activity of a soil was 0. . The values were not related to underground water table. All forms of nutrients were constantly present, showing no correlation with the soil water content. ANOVA revealed significant decrease of nitrate with depth, but not for nitrite, ammonium and ortho-phosphate.
IntroductionThe intermittent Lake Cerknica is characterised by extreme water level fluctuations. A part of the year the area is flooded, but from time to time, usually in summer, it becomes dry. The lake is the locus typicus for intermittent lakes and poljes (karst fields). Wetting and drying occurs seasonally, depending on precipitation. The exchanging of dry and wet periods influences the dynamics of biota and the process of mineralisation (URBANC-BERČIČ and GABERŠČIK, 2001). Common reed (Phragmites australis) is a dominant wetland species in the area. With respect to the water regime three types of reed stands were distinguished: terrestrial, land-water interface, and littoral stands. Stands exhibited significant differences in primary productivity parameters (GABERŠČIK et al., 2000), in the composition and depth of the soil layer, and in the variations of water regime (URBANC-BERČIČ and GABERŠČIK, 2001; URBANC-BERČIČ and GABERŠČIK, in press). Variations of water regime are fundamental for the nutrient cycling in the sediment (BROCK, 1986;BOULTON and BROCK, 1999). Most chemical features depending on aerobic and anaerobic conditions are highly variable. A presence of oxygen in a soil increases the microbial activity and the mineralization rate at the beginning of drying. Later on drying can cause considerable impact on sediment properties by affecting mineral phases and by killing up to 76% of the microbial biomass (QUI and MCCOMB, 1995). These changes reduce the capacity of the sediment to adsorb nutrients, such Internat. Rev. Hydrobiol.