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中国海河沉积物中的磷形态及其释放

Phosphorus fractions and its release in the sediments of Haihe River, China.

作者信息

Sun Shujuan, Huang Suiliang, Sun Xueming, Wen Wei

机构信息

Numerical Simulation Group for Water Environment, College of Environmental Science and Engineering, Nankai University, Tianjin 300071, China.

出版信息

J Environ Sci (China). 2009;21(3):291-5. doi: 10.1016/s1001-0742(08)62266-4.

Abstract

The amounts and forms of phosphorus (P) in surface sediments of Haihe River, Tianjin, North China, were examined using a sequential chemical extraction procedure. Five fractions of sedimentary P, including loosely sorbed P (NH4Cl-P), redox-sensitive P (BD-P), metal oxide bound P (NaOH-P), calcium bound P (HCl-P), and residual P (Res-P) (organic and refractory P), were separately quantified. The results indicated that the contents of different P fractions in the sediments varied greatly. The total P (TP) contents ranged from 968 to 2017 mg/kg. Phosphorus contents in NH4Cl-P, BD-P, NaOH-P, and HCl-P ranged from 6.7 to 26.6 mg/kg, 54.5 to 90.2 mg/kg, 185.2 to 382.5 mg/kg, and 252.3 to 425.5 mg/kg, respectively, which represented 1.2%-3.2%, 7.7%-13%, 33.3%-48.9%, and 36.2%-54.2% of the sedimentary inorganic P, respectively. For all the sediment samples, the rank order of P-fractions was Res-P > HCl-P > NaOH-P > BD-P > NH4Cl-P. The highly positive relationship between the amounts of P released from the sediments and those in the NH4Cl-P and BD-P fractions, indicated that NH4Cl-P and BD-P were the main fractions that can release P easily.

摘要

采用连续化学提取法对中国北方天津市海河表层沉积物中的磷(P)含量及形态进行了研究。分别对沉积物中5种形态的磷进行了定量分析,包括松散吸附态磷(NH4Cl-P)、氧化还原敏感态磷(BD-P)、金属氧化物结合态磷(NaOH-P)、钙结合态磷(HCl-P)和残余态磷(Res-P)(有机磷和难分解磷)。结果表明,沉积物中不同形态磷的含量差异很大。总磷(TP)含量范围为968至2017mg/kg。NH4Cl-P、BD-P、NaOH-P和HCl-P中的磷含量分别为6.7至26.6mg/kg、54.5至90.2mg/kg、185.2至382.5mg/kg和252.3至425.5mg/kg,分别占沉积物无机磷的1.2%-3.2%、7.7%-13%、33.3%-48.9%和36.2%-54.2%。对于所有沉积物样品,磷形态的排序为Res-P>HCl-P>NaOH-P>BD-P>NH4Cl-P。沉积物释放的磷量与NH4Cl-P和BD-P形态磷含量之间存在高度正相关关系,表明NH4Cl-P和BD-P是易于释放磷的主要形态。

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