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Organic phosphorus mineralization characteristics in sediments from the coastal salt marshes of a Chinese delta under simulated tidal cycles

机译:模拟潮汐作用下中国三角洲沿海盐沼沉积物中有机磷的矿化特征

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Purpose Sediment organic phosphorus (OP) mineralization plays an important role in phosphorus cycling in coastal salt marshes. However, information on OP mineralization characteristics in sediments under tidal cycles is limited.Materials and methods Sediment cores were collected from salt marshes which were exposed to tidal cycles. A laboratory manipulation experiment was conducted under simulated tidal flooding cycles. After the completion of each incubation experiment, the inorganic phosphorus (IP) and OP fractions were analyzed and net phosphorus mineralization rates were calculated to investigate the sediment OP mineralization process. Sediment microbial characteristic and chemical properties were determined to identify factors that affect the mineralization of OP in the Yellow River Delta.Results and discussion During the first 2 days of incubation, the tidal cycles significantly increased the microbial biomass in the sediments, which accelerated the assimilation of IP by microorganisms and the transformation of IP into OP in their bodies, thereby causing a significant increase in OP in the sediments. After 2 days of incubation, the mineralization and immobilization of OP entered the adaptation stage and gradually reached the dynamic balance of various phosphorus fractions in sediments. The path analysis showed that microbial biomass phosphorus and carbon (MBP and MBC) and the activity of alkaline phosphatase (AKP) are the direct factors influencing OP mineralization in sediments. The indirect effects of soil organic matter (SOM), water content (WC), exchangeable aluminum (Al-0), and exchangeable iron (Fe-0) on net phosphorus mineralization rate were relatively high.Conclusions In the laboratory experiments, we showed that the recovery of tidal cycles caused a fluctuation in OP mineralization and immobilization in sediments, which reached equilibrium over time. The tidal effect was conducive to maintaining the stability of phosphorus in sediments of coastal salt marshes. The findings of this study can contribute to protecting water quality and improving primary productivity in coastal salt marshes by regulating the tidal cycles and the key environmental factors (e.g., SOM, WC, Al-0, and Fe-0) influencing OP mineralization.
机译:目的沉积物有机磷(OP)的矿化作用在沿海盐沼的磷循环中起着重要作用。然而,有关潮汐作用下沉积物中OP矿化特征的信息是有限的。材料和方法从暴露于潮汐作用下的盐沼中收集沉积岩心。在模拟潮汐洪水周期下进行了实验室操作实验。在完成每个温育实验后,分析无机磷(IP)和OP组分,并计算净磷矿化率以研究沉积物OP矿化过程。测定和确定沉积物的微生物特征和化学性质,以识别影响黄河三角洲OP矿化的因素。结果与讨论在孵化的前两天,潮汐周期显着增加了沉积物中的微生物生物量,从而加速了同化作用。微生物对IP的吸收以及IP在其体内转化为OP的方式,从而导致沉积物中OP的显着增加。孵育2天后,OP的矿化和固定化进入适应阶段,并逐渐达到沉积物中各种磷组分的动态平衡。路径分析表明,微生物生物量中的磷和碳(MBP和MBC)以及碱性磷酸酶(AKP)的活性是影响沉积物中OP矿化的直接因素。土壤有机质(SOM),水分(WC),可交换铝(Al-0)和可交换铁(Fe-0)对净磷矿化速率的间接影响相对较高。结论在实验室实验中,我们证明了潮汐循环的恢复引起沉积物中OP矿化和固定化的波动,并随时间达到平衡。潮汐作用有利于维持沿海盐沼沉积物中磷的稳定性。这项研究的发现可通过调节潮汐周期和影响OP矿化的关键环境因素(例如SOM,WC,Al-0和Fe-0)来帮助保护沿海盐沼的水质和提高初级生产力。

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