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Distribution of Geochemical Fractions of Phosphorus in Surface Sediment in Daya Bay China

机译:大亚湾表层沉积物中磷的地球化学组成分布

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摘要

Surface sediment samples were collected from 19 sites throughout Daya Bay, China, to study the concentrations, and spatial distributions of different fractions of phosphorus through sequential extraction methods. Like many coastal and marine areas, De-P was the dominant form of P, contributing 47.5% of TP, followed by O-P, contributing 25.5% of TP. Ex-P and Fe-P contribute the lowest to TP. The concentration of sedimentary TP ranged from 290.3~525.1 µg/g, with the average of 395.3 µg/g, which was a similar range to other estuaries and coastal areas. Based on the spatial distribution, Pearson correlation and Principal component analysis, different fractions of phosphorus showed different spatial distributions due to different sources. The molar ratio of organic carbon to phosphorus (TOC/O-P) ranged from 199 to 609, with the average of 413, which was much higher than the Redfield ratio, suggesting terrestrial sources of organic matter in Daya Bay surface sediment. The average bioavailable phosphorus was 149.6 µg/g and contributed 37.8% (24.6~56.0%) of TP, indicating that the surface sediments of Day Bay act as an important internal source of P.
机译:从中国大亚湾的19个站点收集了地表沉积物样本,以通过顺序提取方法研究磷的不同部分的浓度和空间分布。像许多沿海和海洋地区一样,De-P是P的主要形式,占TP的47.5%,其次是O-P,占TP的25.5%。 Ex-P和Fe-P对TP的贡献最低。沉积物TP的浓度范围为290.3〜525.1 µg / g,平均浓度为395.3 µg / g,与其他河口和沿海地区相似。基于空间分布,Pearson相关性和主成分分析,由于来源不同,不同比例的磷表现出不同的空间分布。有机碳与磷的摩尔比(TOC / O-P)为199至609,平均为413,远高于Redfield的比值,表明大亚湾表层沉积物中有机物的陆源。平均生物利用磷为149.6 µg / g,占TP的37.8%(24.6%至56.0%),表明Day Bay的表层沉积物是磷的重要内部来源。

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