Sun Shujuan, Huang Suiliang, Sun Xueming, Wen Wei
Numerical Simulation Group for Water Environment, College of Environmental Science and Engineering, Nankai University, Tianjin 300071, China.
J Environ Sci (China). 2009;21(3):291-5. doi: 10.1016/s1001-0742(08)62266-4.
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.
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。