Parikh Sanjai J, Chorover Jon, Burgos William D
Department of Soil, Water and Environmental Science, The University of Arizona, 429 Shantz Building, Tucson, AZ 85721, USA.
J Contam Hydrol. 2004 Aug;72(1-4):1-22. doi: 10.1016/j.jconhyd.2003.10.004.
Experiments were conducted to compare the sorption and desorption of phenanthrene and its primary degradation product, 1-hydroxy-2-naphthoic acid (HNA), in estuarine sediment, humic acid (HA) and humin. Ionic composition, ionic strength (0.4 M) and pH (7.6) were employed to mimic native estuarine pore water at the sediment-water interface. Sorption to whole sediment and organic matter (OM) fractions was significantly lower for HNA than for phenanthrene. Whereas HNA did not sorb to HA, uptake to sediment and humin was observed, suggesting that HNA does not bind directly to OM. Phenanthrene uptake was characterized by hysteretic behavior and exhibited slow desorption. In contrast, HNA initially was more readily desorbed from sediment and humic fractions, but a significant fraction was not recovered in repeated desorption runs. The lower sorption of HNA reflects its greater polarity and water solubility, but the consistent retention of a non-desorbing fraction suggests strong binding and/or chemical transformation reactions may be important. It was postulated that abiotic transformation of HNA may occur in estuarine sediments, in part due to the presence of redox active minerals (Fe(III) and Mn(IV) oxides). The presence of Fe and Mn solids in the estuarine sediment was verified by sequential extraction and studies were then conducted to investigate the transformation of HNA in the presence of synthetic goethite (alpha-FeOOH) and birnessite (delta-MnO2) as model solids. Reaction with birnessite led to transformation of all HNA in solution within 24 h and resulted in the formation of partial oxidation products (POPs). Following reaction with goethite, HNA was present in solution and POPs were observed in the weakly bound fraction. This study indicates that degradation products of polycyclic aromatic hydrocarbons (PAHs) may have distinctly different sorption affinities and reactivities toward environmental surfaces than their parent compounds.
开展了实验,以比较菲及其主要降解产物1-羟基-2-萘甲酸(HNA)在河口沉积物、腐殖酸(HA)和腐殖质中的吸附和解吸情况。采用离子组成、离子强度(0.4M)和pH值(7.6)来模拟沉积物-水界面处的天然河口孔隙水。HNA在整个沉积物和有机物质(OM)组分上的吸附显著低于菲。HNA不吸附于HA,但观察到其在沉积物和腐殖质上的吸附,这表明HNA不直接与OM结合。菲的吸附具有滞后行为,且解吸缓慢。相比之下,HNA最初更容易从沉积物和腐殖质组分上解吸,但在重复解吸过程中,有相当一部分未被回收。HNA较低的吸附反映了其较高的极性和水溶性,但非解吸部分的持续保留表明强结合和/或化学反应可能很重要。据推测,HNA的非生物转化可能发生在河口沉积物中,部分原因是存在氧化还原活性矿物(Fe(III)和Mn(IV)氧化物)。通过顺序提取验证了河口沉积物中Fe和Mn固体的存在,然后进行研究以调查在作为模型固体的合成针铁矿(α-FeOOH)和水钠锰矿(δ-MnO2)存在下HNA的转化。与水钠锰矿反应导致溶液中所有HNA在24小时内转化,并形成部分氧化产物(POPs)。与针铁矿反应后,HNA存在于溶液中,且在弱结合部分观察到POPs。本研究表明,多环芳烃(PAHs)的降解产物与其母体化合物相比,对环境表面可能具有明显不同的吸附亲和力和反应活性。