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Bacterially mediated removal of phosphorus and cycling of nitrate and sulfate in the waste stream of a 'zero-discharge' recirculating mariculture system

机译:在“零排放”再循环海水养殖系统的废物流中细菌介导的磷的去除和硝酸盐和硫酸盐的循环

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摘要

Simultaneous removal of nitrogen and phosphorus by microbial biofilters has been used in a variety of water treatment systems including treatment systems in aquaculture. In this study, phosphorus, nitrate and sulfate cycling in the anaerobic loop of a zero-discharge, recirculating mariculture system was investigated using detailed geochemical measurements in the sludge layer of the digestion basin. High concentrations of nitrate and sulfate, circulating in the overlying water (∼15 mM), were removed by microbial respiration in the sludge resulting in a sulfide accumulation of up to 3 mM. Modelling of the observed S and O isotopic ratios in the surface sludge suggested that, with time, major respiration processes shifted from heterotrophic nitrate and sulfate reduction to autotrophic nitrate reduction. The much higher inorganic P content of the sludge relative to the fish feces is attributed to conversion of organic P to authigenic apatite. This conclusion is supported by: (a) X-ray diffraction analyses, which pointed to an accumulation of a calcium phosphate mineral phase that was different from P phases found in the feces, (b) the calculation that the pore waters of the sludge were highly oversaturated with respect to hydroxyapatite (saturation index = 4.87) and (c) there was a decrease in phosphate (and in the Ca/Na molar ratio) in the pore waters simultaneous with an increase in ammonia showing there had to be an additional P removal process at the same time as the heterotrophic breakdown of organic matter.
机译:通过微生物生物滤池同时去除氮和磷已用于包括水产养殖处理系统在内的各种水处理系统中。在这项研究中,使用详细的地球化学测量值对消化池污泥层中的零排放循环海水养殖系统的厌氧回路中的磷,硝酸盐和硫酸盐循环进行了研究。在上层水中循环的高浓度硝酸盐和硫酸盐(约15 mM)通过污泥中的微生物呼吸作用被去除,导致硫化物积累高达3 mM。对表面污泥中观察到的S和O同位素比率的建模表明,随着时间的流逝,主要的呼吸过程从异养硝酸盐和硫酸盐还原转变为自养硝酸盐还原。相对于鱼粪而言,污泥中无机磷的含量高得多,这归因于有机磷向自生磷灰石的转化。该结论得到以下方面的支持:(a)X射线衍射分析,表明与粪便中发现的P相不同的磷酸钙矿物相的积累,(b)计算出污泥的孔隙水为相对于羟基磷灰石而言,过饱和度很高(饱和指数= 4.87),并且(c)孔隙水中的磷酸盐(以及Ca / Na摩尔比)降低,同时氨水增加,这表明必须添加额外的P去除过程同时进行有机物的异养分解。

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