Laboratory for Earth Surface Processes, College of Urban and Environmental Sciences, Peking University , Beijing 100871, China.
Environ Sci Technol. 2013;47(21):12148-55. doi: 10.1021/es401732e. Epub 2013 Oct 7.
Soil organic matter (SOM) in a peat soil, humic acid, and humin and their precursors (i.e., cellulose and lignin) were treated at high temperature (250 and 400 °C) with high pressure in a sealed platinum reaction kittle to simulate the influence of diagenesis on their composition and structure, and impact of the simulated diagenesis on sorption behaviors of hydrophobic organic compounds (HOCs) (i.e., naphthalene and 1-naphthol) by these samples was investigated. High temperature and pressure treatment greatly influenced chemical composition and physical properties of the original samples and their sorption for both naphthalene and 1-naphthol. Sorption of naphthalene by all samples was jointly regulated by hydrophobic and π-π interactions with their alkyl and aromatic carbon moieties, which was derived from the positive correlation between total hydrophobic carbon content of all sorbents and their organic carbon content-normalized sorption coefficients (Koc) for this compound (p = 0.075). However, sorption of 1-naphthol by the tested sorbents was governed by hydrogen bonding with their O-containing polar functionalities, as derived from the positive correlation between Koc values of 1-Naph and their polarity index ((O+N)/C). Difference in sorption mechanisms of naphthalene and 1-naphthol by the original and treated samples noted the great influence of chemical composition of sorbates on their interaction and essential roles of specific interactions (e.g., hydrogen bonding) in sorption of polar compound (i.e., 1-naphthol) to these sorbents. Surface area (SA) and porosity data of sorbents obtained from N2 sorption-desorption isotherms at 77 K showed that new SA and pores were created during the diagenetic process of all original samples, which provided substantial sorption sites and thus enhanced sorption of naphthalene and 1-naphthol. Among all tested samples, physicochemical properties of cellulose were most strongly affected by the simulated diagenetic process, and impact of such a process on its sorption intensity for the tested compounds was the most significant. The characterization data of the treated sorbents showed that the high temperature and pressure treatment similarly simulated the naturally occurring diagenesis of SOMs and their precursors, which is a first attempt. These findings are valuable for better understanding of the sorption behaviors of HOCs to SOM and its precursors as affected by diagenesis, which in turn is critical for elucidating the transport and fate of HOCs in the environment.
土壤有机质(SOM)、腐殖酸、腐殖质及其前体(即纤维素和木质素)在密封的白金反应罐中,在高温(250 和 400°C)和高压下处理,以模拟成岩作用对其组成和结构的影响,以及模拟成岩作用对疏水性有机化合物(HOCs)(即萘和 1-萘酚)在这些样品上吸附行为的影响。高温高压处理极大地影响了原始样品的化学组成和物理性质,以及它们对萘和 1-萘酚的吸附。所有样品对萘的吸附均受疏水性和π-π相互作用的共同调节,这与所有吸附剂的总疏水性碳含量与其有机碳归一化吸附系数(Koc)之间的正相关关系有关(p=0.075)。然而,测试吸附剂对 1-萘酚的吸附是由其含 O 极性官能团的氢键决定的,这是由 Koc 值与极性指数((O+N)/C)之间的正相关关系得出的。原始和处理样品对萘和 1-萘酚吸附机制的差异表明,吸附质的化学组成对其相互作用有很大影响,氢键等特定相互作用在这些吸附剂对极性化合物(即 1-萘酚)的吸附中起着重要作用。从 77 K 下氮气吸附-解吸等温线获得的吸附剂的表面积(SA)和孔隙率数据表明,所有原始样品的成岩过程中都产生了新的 SA 和孔隙,这为吸附提供了大量的吸附位,从而增强了萘和 1-萘酚的吸附。在所有测试的样品中,纤维素的物理化学性质受模拟成岩过程的影响最大,而该过程对其对测试化合物的吸附强度的影响也最大。处理后的吸附剂的表征数据表明,高温高压处理同样模拟了 SOM 和其前体的自然成岩作用,这是首次尝试。这些发现对于更好地理解 HOCs 与 SOM 和其前体的吸附行为受成岩作用的影响是有价值的,这对于阐明 HOCs 在环境中的迁移和归宿至关重要。