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Influence of the biomass content in sediment on the sediment nutrient flux for a pulsed organic load

机译:脉冲有机负荷下沉积物中生物量的含量对沉积物养分通量的影响

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A laboratory study was carried out to investigate the influence of the biomass content in the sediment on the rate of diagenesis of particulate organic materials (POM) and the consequent sediment oxygen demand (SOD) and nutrient fluxes. Fish food pellets were loaded into the sediment to simulate a sudden POM input. Three types of sediments with different biomass contents were tested, including a raw marine sediment, the marine sediment after one month of cultivation and an artificial sediment of sand and clay without any biomass. There was little difference in organic flux from the three different sediments. However, compared to the artificial sediment, the marine sediments had much higher SOD and ammonia flux. A mathematical model also has been developed for the SOD dynamics and nutrient fluxes. Both the experimental and simulation results indicate the important role of the biomass in the sediment in POM diagenesis, SOD and nutrient fluxes.
机译:进行了一项实验室研究,以调查沉积物中生物量的含量对颗粒状有机物(POM)的成岩速率以及随之产生的沉积物需氧量(SOD)和养分通量的影响。将鱼粮颗粒装载到沉积物中,以模拟突然的POM输入。测试了三种具有不同生物量含量的沉积物,包括原始海洋沉积物,培养一个月后的海洋沉积物和不含任何生物量的沙子和粘土人工沉积物。来自三种不同沉积物的有机通量几乎没有差异。但是,与人工沉积物相比,海洋沉积物的SOD和氨通量要高得多。还为SOD动力学和养分通量开发了数学模型。实验和模拟结果均表明,生物质在底泥中对POM成岩作用,SOD和养分通量具有重要作用。

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