徐程, 杨斌, 莫小荣, 宁志铭, 黄海方. 茅尾海入海河口区表层沉积物磷形态特征研究[J]. 海洋环境科学, 2021, 40(2): 250-257. DOI: 10.12111/j.mes.20200080
引用本文: 徐程, 杨斌, 莫小荣, 宁志铭, 黄海方. 茅尾海入海河口区表层沉积物磷形态特征研究[J]. 海洋环境科学, 2021, 40(2): 250-257. DOI: 10.12111/j.mes.20200080
XU Cheng, YANG Bin, MO Xiao-rong, NING Zhi-ming, HUANG Hai-fang. Forms and characteristics of phosphorus in surface sediment from estuary areas in the Maowei sea[J]. Chinese Journal of MARINE ENVIRONMENTAL SCIENCE, 2021, 40(2): 250-257. DOI: 10.12111/j.mes.20200080
Citation: XU Cheng, YANG Bin, MO Xiao-rong, NING Zhi-ming, HUANG Hai-fang. Forms and characteristics of phosphorus in surface sediment from estuary areas in the Maowei sea[J]. Chinese Journal of MARINE ENVIRONMENTAL SCIENCE, 2021, 40(2): 250-257. DOI: 10.12111/j.mes.20200080

茅尾海入海河口区表层沉积物磷形态特征研究

Forms and characteristics of phosphorus in surface sediment from estuary areas in the Maowei sea

  • 摘要: 以茅尾海两个主要入海河口区表层沉积物为研究对象,采用改进后的连续提取法(SEDEX)对15个采样点沉积物中磷的组分、含量、分布及其影响因素进行研究,探讨了磷的生物有效性。结果表明,无机磷(IP)是茅岭江和钦江入海河口区表层沉积物中总磷(TP)的主要存在形式,平均分别占TP的64.4%和65.9%,有机磷(OP)均占较小的比例。IP均以铁结合态磷(Fe-P)为主要赋存形态,平均分别占TP的31.2%和28.1%,原生碎屑磷(De-P)、自生磷灰石磷(Ca-P)和可交换态磷(Ex-P)平均占TP比例依次递减。河流输入、沉积物粒度和沉积环境是影响茅尾海入海河口区表层沉积物中不同形态磷含量及分布的主要因素。磷生物有效性分析表明,茅岭江、钦江入海河口区表层沉积物中生物可利用磷(BAP)含量分别为2.95~22.52 μmol/g和2.67~13.83 μmol/g,平均占TP的73.9%和68.8%,呈现较强的释磷潜力。

     

    Abstract: Surface sediments from fifteen stations were sampled along the Maolingjiang river estuary (MRE) and Qinjiang river estuary (QRE) areas in the Maowei sea, and analyzed using an improved sequential extraction (SEDEX) method to evaluate the abundance, distribution and potential bioavailable forms of P. Results showed that inorganic P (IP) was the dominant P form, which averagely accounted for 64.4% and 65.9% of total P (TP) pool in surface sediments along the MRE and QRE areas, respectively. Ferric (Fe) bound P (Fe-P) was the dominant IP specie, accounting for 31.2% and 28.1% of sedimentary TP pool, respectively along the MRE and QRE areas. The proportions of other IP species such as the detrital apatite P (De-P), authigenic P (Ca-P) and exchangeable P (Ex-P) were relatively low in surface sediments. Riverine inputs, sediment grain size and sedimentary environment played influential roles on the concentration and distribution of different P forms in the study area. The concentrations of potential bioavailable P (BAP) were 2.95~22.52 μmol/g and 2.67~13.83 μmol/g, respectively, and averagely accounted for 73.9% and 68.8% of TP pool in surface sediments along the MRE and QRE areas, respectively. Thus, surface sediments deposited along the estuarine areas in the Maowei sea show a higher potential for P release into the overlying water.

     

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