Distribution Characteristics and Factors Controlling Different Phosphorus Fractions in the Soils and Sediments of an Inland Lagoon

Kun Yuan, Rui Wang, Bo He, Guowei Fu, Yanwei Song, Lixin Pei, Shichao Fan, Fangyi Gao
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Abstract

Lagoons, significant coastal wetlands, stand out for their vital role in the cycles and transformations of phosphorus. However, the relationship between the spatial distributions of various phosphorus forms in the soil and sediments of lagoon areas remains unclear. This study investigated the phosphorus fractions and distribution patterns in the soil and sediments from Shimei Inland Sea, Hainan Province, China, and identified the factors controlling phosphorus distribution and its relationship with lagoon eutrophication. The results revealed significant enrichment of inorganic phosphorus (IP) in the Shimei Inland Sea (64.1–679.0 mg/kg) and offshore areas (56–627.2 mg/kg), while organic phosphorus (OP) was relatively concentrated in land (60–744.3 mg/kg), suggesting that the productivity of the terrestrial ecosystem controlled the OP content and IP formed from the mineralization of OP was more likely to leach into the water and combine with minerals. Total phosphorus (TP) content was negatively affected by pH, and organic matter, cation exchange capacity and iron/aluminum oxides showed significant positive correlations with TP content. These findings highlighted the coupled impact of soil and sediment physicochemical properties on phosphorus enrichment and transformation, providing theoretical support for the ecological restoration of ecosystems in tropical coastal wetlands.
内陆泻湖土壤和沉积物中不同磷组分的分布特征和控制因素
泻湖是重要的沿海湿地,在磷的循环和转化中发挥着重要作用。然而,潟湖地区土壤和沉积物中各种形态的磷的空间分布关系仍不清楚。本研究调查了中国海南省石梅内海土壤和沉积物中磷的组分和分布模式,确定了控制磷分布的因素及其与环礁湖富营养化的关系。结果表明,无机磷(IP)在石梅内海(64.1-679.0 mg/kg)和近海区域(56-627.2 mg/kg)明显富集,而有机磷(OP)则相对集中在陆地(60-744.3 mg/kg),这表明陆地生态系统的生产力控制着OP的含量,由OP矿化形成的IP更容易渗入水中并与矿物质结合。总磷(TP)含量受 pH 值的负面影响,而有机质、阳离子交换容量和铁/铝氧化物与 TP 含量呈显著正相关。这些发现强调了土壤和沉积物物理化学特性对磷富集和转化的耦合影响,为热带沿海湿地生态系统的生态恢复提供了理论支持。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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