Institute of Hydrobiology and Aquatic Ecosystem Management, University of Natural Resources and Life Sciences, Gregor-Mendel-Straße 33, 1180 Vienna, Austria; WasserCluster Lunz, Dr. Kupelwieser-Promenade 5, 3293 Lunz am See, Austria.
WasserCluster Lunz, Dr. Kupelwieser-Promenade 5, 3293 Lunz am See, Austria; Institute of Hydrobiology, Chinese Academy of Sciences, Wuhan 430072, China.
Sci Total Environ. 2020 Jun 15;721:137620. doi: 10.1016/j.scitotenv.2020.137620. Epub 2020 Feb 29.
Transport and transformation of inorganic nutrients are influenced by abiotic-biotic interactions and determine downstream water quality. Macrophytes play an important role in these complex ecological interactions. The role of macrophytes was studied in three reaches of the groundwater-fed, oligotrophic River Fischa with different macrophyte coverage and biomass. This was done by measuring metabolism and calculating changes in nutrient loading and concentrations, which were determined via an upstream-downstream mass balance approach. As the dominant autotrophs, we expected macrophytes (i) to have a direct effect by uptake and release, and (ii) an indirect effect by slowing down flow, which results in changed sedimentation patterns and altered conditions for heterotrophic microbial organisms implicating higher turnover and uptake rates. The seasonal development of macrophytes in 2017 had a strong impact on gross primary production, but not on ecosystem respiration. Increase in macrophyte biomass led to higher GPP (max. 5.4 g Omd). ER was highest in autumn in the reach with intermediate macrophyte biomass (max. 10.1 g Omd). We observed that the autotrophic uptake of phosphorus accounted for 80-145% of the P-PO-flux and concluded that P-uptake by macrophytes from the sediment is an important source of phosphate for macrophytes in the river. By accumulating fine sediment, macrophytes are improving the availability of phosphate for their own long-term development. N-NO, represented >99% of the nitrogen flux. N-NO net uptake was higher in the reaches with more macrophytes (0.84 vs. 0.12 g md), but in average only 21% of the net uptake could be related to autotrophic nitrogen uptake in the reach with high macrophyte biomass. Dissimilatory uptake by heterotrophic organisms, most probably denitrification, were of high relevance. Macrophytes supported microbial uptake and release by improving conditions and slowing down flow. In the River Fischa, an oligotrophic river with low variability of environmental parameters, macrophytes greatly affected nutrient uptake by direct and indirect pathways.
无机养分的迁移和转化受到非生物-生物相互作用的影响,并决定了下游的水质。大型水生植物在这些复杂的生态相互作用中发挥着重要作用。本研究以富营养化程度低、地下水补给的菲沙河的三个河段为研究对象,探讨了不同大型水生植物覆盖度和生物量条件下大型水生植物的作用。通过测量新陈代谢并通过上下游物质平衡方法计算营养负荷和浓度的变化来进行研究。作为主要的自养生物,我们预计大型水生植物(i)通过吸收和释放产生直接影响,(ii)通过减缓水流产生间接影响,这会导致沉积模式发生变化,改变异养微生物的条件,从而导致更高的周转率和吸收速率。2017 年大型水生植物的季节性发展对总初级生产力有很大影响,但对生态系统呼吸没有影响。大型水生植物生物量的增加导致更高的 GPP(最大值为 5.4 g Omd)。在中型大型水生植物生物量的河段中,秋季 ER 最高(最大值为 10.1 g Omd)。我们观察到,磷的自养吸收占 P-PO 通量的 80-145%,并得出结论,从沉积物中吸收磷是河流中大型水生植物磷的重要来源。通过积累细沉积物,大型水生植物提高了自身长期发展所需的磷酸盐可用性。N-NO 占氮通量的>99%。有更多大型水生植物的河段的 N-NO 净吸收量更高(0.84 与 0.12 g md),但在高大型水生植物生物量的河段中,仅有 21%的净吸收量可归因于自养氮吸收。异养生物的异化吸收,很可能是反硝化作用,具有重要意义。大型水生植物通过改善条件和减缓水流来支持微生物的吸收和释放。在菲沙河这条富营养化程度低、环境参数变化小的河流中,大型水生植物通过直接和间接途径极大地影响了养分的吸收。