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Study on the Biotic Influence on Internal Phosphorus Release in the Sediment of Lake Xuanwu

机译:玄武湖沉积物中内磷释放的生物影响研究

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To uncover the biotic influence of the internal phosphorus release in the sediment of Lake Xuanwu, colony-counting method of flat-panel culture was used to analysis the amount and categories of phosphorus-degrading microorganism. The result showed that there were phosphorus-degrading microorganisms in the sediments of the Lake Xuanwu and most them were inorganic phosphorus-degrading microorganisms, the number was 5.25 × 104 cfu each gram sediment, while the organic phosphorus-degrading microorganism was few. The internal phosphorus release contrast experiments were done with the sediment with microorganism and without microorganism. The result showed that the microorganism absorbed more phosphorus but degraded few due to the aerobic interface of the sediment, so the microorganisms in the sediment inhibited the internal phosphorus release from the sediment. In Alkaline water condition, the internal phosphorus release more than in the neutral water condition, which infer that the chemical release process was that insoluble Ca3(PO4)2, Fe3(PO4)2 transformed into insoluble Ca(OH)2 and Fe(OH) 3 and resulted the PO43- dissolved into the overlying water.
机译:为了揭示宣武湖沉积物中内磷释放的生物影响,平板培养的殖民地计数方法分析磷降解微生物的量和类别。结果表明,玄武湖沉积物中存在磷脂微生物,大多数它们是无机磷降解微生物,该数量为5.25×104 CFU,每克沉积物,而有机磷降解微生物少。用微生物和没有微生物的沉积物进行内部磷释放对比实验。结果表明,由于沉积物的有氧界面,微生物吸收了更多的磷,但很少降解,因此沉积物中的微生物抑制了沉积物的内部磷释放。在碱性水状况中,内部磷释放比中性水状况更多,这次推断化学释放过程是不溶性CA3(PO4)2,Fe3(PO4)2转化为不溶性Ca(OH)2和Fe(OH )3并将PO43溶解在上覆水中。

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