Centre for Ecology and Hydrology, Wallingford, Oxfordshire, OX10 8BB, UK.
Environ Sci Technol. 2010 Feb 1;44(3):908-14. doi: 10.1021/es902706r.
Diffusive equilibration in thin films was used to study the cycling of phosphorus and nitrogen at the sediment-water interface in situ and with minimal disturbance to redox conditions. Soluble reactive phosphate (SRP), nitrate, nitrite, ammonium, sulfate, iron, and manganese profiles were measured in a rural stream, 12 m upstream, adjacent to, and 8 m downstream of a septic tank discharge. Sewage fungus adjacent to the discharge resulted in anoxic conditions directly above the sediment. SRP and ammonium increased with depth through the fungus layer to environmentally significant concentrations (440 and 1800 microM, respectively) due to release at the sediment surface. This compared to only 0.8 microM of SRP and 2.0 microM of ammonium in the water column upstream of the discharge. Concomitant removal of ammonium, nitrite and nitrate within 0.5 cm below the fungus-water interface provided evidence for anaerobic ammonium oxidation (anammox). "Hotspots" of porewater SRP (up to 350 microM) at the downstream site demonstrated potential in-stream storage of the elevated P concentrations from the effluent. These results provide direct in situ evidence of phosphorus and nitrogen release from river-bed sediments under anoxic conditions created by sewage-fungus, and highlight the wider importance of redox conditions and rural point sources on in-stream nutrient cycling.
采用薄膜扩散平衡法原位研究了磷和氮在沉积物-水界面的循环过程,同时最小化对氧化还原条件的干扰。在一条农村溪流中测量了可溶解性反应磷(SRP)、硝酸盐、亚硝酸盐、铵、硫酸盐、铁和锰的分布情况,该溪流位于 12 米上游、紧邻污水处理池排放口处以及 8 米下游处。排放口附近的污水真菌导致沉积物上方出现缺氧条件。由于在沉积物表面释放,SRP 和铵在真菌层中随着深度的增加而增加,达到环境显著浓度(分别为 440 和 1800μM)。相比之下,在排放口上游的水柱状中,SRP 仅为 0.8μM,铵为 2.0μM。在真菌-水界面以下 0.5 厘米处同时去除铵、亚硝酸盐和硝酸盐,为厌氧氨氧化(anammox)提供了证据。在下游位置,底泥中孔穴水的 SRP 出现高达 350μM 的“热点”,表明从污水中流出的高浓度磷有在河流中存储的潜力。这些结果提供了直接的原位证据,证明在由污水真菌产生的缺氧条件下,河流沉积物中的磷和氮会释放出来,并强调了氧化还原条件和农村点源对河流中营养物质循环的更广泛重要性。