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Effect of nutrient loading on biogeochemical processes in tropical tidal creeks

机译:营养盐负荷对热带潮汐小溪生物地球化学过程的影响

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The effect of increased nutrient loads on biogeochemical processes in macrotidal, mangrove-lined creeks was studied in tropical Darwin Harbour, Australia. This study uses an integrative approach involving multiple benthic and pelagic processes as measures of ecosystem function, and provides a comparison of these processes in three tidal creeks receiving different loads of treated sewage effluent. There were significant differences in process rates between Buffalo Creek (BC) (hypereutrophic), which receives the largest sewage loads; Myrmidon Creek (MC) (oligotrophic–mesotrophic) which receives smaller sewage inputs; and Reference Creek (RC) (oligotrophic) which is comparatively pristine. Benthic nutrient fluxes and denitrification were more than an order of magnitude higher and lower, respectively, in BC and denitrification efficiency (DE) was <10%. Pelagic primary production rates were also much higher in BC but respiration exceeded primary production resulting in severe drawdown of O2 concentrations at night. Hypoxic conditions released oxide-bound phosphorus and inhibited coupled nitrification–denitrification, enhancing benthic nitrogen and phosphorus fluxes, leading to a build-up of excess nutrients in the water column. Poor water quality in BC was exacerbated by limited tidal flushing imposed by a narrow meandering channel and sandbar across the mouth. In contrast to BC, the effect of the sewage load in MC was confined to the water column, and the impact was temporary and highly localized. This is attributed to the effective flushing of the sewage plume with each tidal cycle. Denitrification rates in MC and RC were high (up to 6.83 mmol N m−2 day−1) and DE was approximately 90%. This study has identified denitrification, benthic nutrient fluxes and pelagic primary production as the biogeochemical processes most affected by nutrient loading in these tidal creek systems. Physical process play a key role and the combined influence of nutrient loading and poor tidal flushing can have serious consequences for ecosystem functioning.
机译:在澳大利亚热带达尔文港,研究了养分负荷增加对红树林衬里的巨潮小河生物地球化学过程的影响。这项研究采用了涉及多个底栖和浮游过程的综合方法作为生态系统功能的度量,并提供了在三个潮汐小溪中这些过程的比较,这些小溪接受了不同负荷的处理污水。 Buffalo Creek(BC)(营养过剩)之间的处理速率存在显着差异,该区域的污水负荷最大。 Myrmidon Creek(MC)(贫营养—中营养),其污水输入量较小;以及相对原始的Reference Creek(RC)(营养不足)。在卑诗省,底栖养分通量和反硝化分别高出和低出一个数量级,反硝化效率(DE)<10%。卑诗省中上层的初级生产力也高得多,但呼吸超过初级生产力,导致夜间O 2 浓度严重下降。缺氧条件释放了结合氧化物的磷,并抑制了硝化-反硝化作用,增加了底栖氮和磷通量,导致水柱中养分过多。狭窄的蜿蜒曲折河道和穿过河口的沙洲限制了潮汐冲刷,使卑诗省水质恶化。与不列颠哥伦比亚省相反,MC中污水负荷的影响仅限于水柱,并且影响是暂时的且高度局部化。这归因于每个潮汐周期都有效冲洗了污水羽流。 MC和RC的反硝化率很高(高达6.83 mmol N m -2 天 -1 ),DE约为90%。这项研究已经确定反硝化作用,底栖营养通量和浮游初级生产是这些潮汐小溪系统中受营养物负荷影响最大的生物地球化学过程。物理过程起着关键作用,养分含量和潮汐冲刷不良的综合影响可能对生态系统功能产生严重影响。

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