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Phosphorus Fractions and Its Adsorption Thermodynamics onto Sediments from the Upper Reaches of the Yellow River, China

机译:中国黄河上游沉积物磷馏分及其吸附热力学

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The form distribution of phosphorus (P) in ten surface sediments from the upper reaches of the Yellow River, China, was studied using the sequential chemical extraction procedure--the standards, measurements and testing harmonized procedure. The equilibrium and thermodynamics of P adsorption onto sediments were evaluated. Five fractions of sedimentary P, including metal oxide bound P (NaOH-P), calcium bound P (HCl-P), inorganic P (IP), organic P (OP) and concentrated HCl P (total P, TP), were separately quantified. The results indicated that the contents of different P fractions in sediments varied greatly. The mean of TP content was 657.57 mg/kg, and averages of NaOH-P, OP, HCl-P and IP contents represented 4.03%, 8.85%, 82.10% and 88.69% of TP, respectively. HCl-P was the major component of IP and TP. The amount of potential bioavailable P was approximately estimated 12.88% of TP. The equilibrium data of P adsorption on different sediments fitted perfectly for Langmuir and Freundlich models. The adsorption amounts of P decreased with increasing temperature. The negative values of thermodynamic parameters ?G and ?H indicated the spontaneous and exothermic nature of the sorption.
机译:使用顺序化学提取程序研究了黄河上游10个表面沉积物中磷(P)的形式分布 - 标准,测量和检测协调程序。评估了P吸附到沉积物上的平衡和热力学。沉积P的五个部分,包括金属氧化物结合的p(NaOH-P),钙结合的P(HCl-P),无机P(IP),有机P(OP)和浓HCl P(总P,TP)分别是单独的量化。结果表明,沉积物中不同P部分的含量变化大大变化。 TP含量的平均值为657.57mg / kg,以及NaOH-P,OP,HCl-P和IP含量的平均分别表示为4.03%,8.85%,82.10%和88.69%的TP。 HCl-P是IP和TP的主要成分。潜在的生物可利用率p的量估计为TP的12.88%。不同沉积物对不同沉积物的平衡数据,适用于Langmuir和Freundlich模型。随着温度的增加,P的吸附量降低。热力学参数的负值?G和ΔH表示吸附的自发性和放热性质。

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