Sutton Rebecca, Sposito Garrison
Department of Environmental Science, Policy and Management, University of California, Berkeley 94720-3114, USA.
Environ Sci Technol. 2005 Dec 1;39(23):9009-15. doi: 10.1021/es050778q.
A critical examination of published data obtained primarily from recent nuclear magnetic resonance spectroscopy, X-ray absorption near-edge structure spectroscopy, electrospray ionization-mass spectrometry, and pyrolysis studies reveals an evolving new view of the molecular structure of soil humic substances. According to the new view, humic substances are collections of diverse, relatively low molecular mass components forming dynamic associations stabilized by hydrophobic interactions and hydrogen bonds. These associations are capable of organizing into micellar structures in suitable aqueous environments. Humic components display contrasting molecular motional behavior and may be spatially segregated on a scale of nanometers. Within this new structural context, these components comprise any molecules intimately associated with a humic substance, such that they cannot be separated effectively by chemical or physical methods. Thus biomolecules strongly bound within humic fractions are by definition humic components, a conclusion that necessarily calls into question key biogeochemical pathways traditionally thought to be required for the formation of humic substances. Further research is needed to elucidate the intermolecular interactions that link humic components into supramolecular associations and to establish the pathways by which these associations emerge from the degradation of organic litter.
对主要从近期核磁共振光谱、X射线吸收近边结构光谱、电喷雾电离质谱和热解研究中获得的已发表数据进行批判性审视,揭示了土壤腐殖质分子结构的一种不断演变的新观点。根据这一新观点,腐殖质是由多种相对低分子量成分组成的集合体,这些成分通过疏水相互作用和氢键形成动态缔合。在合适的水环境中,这些缔合能够组织成胶束结构。腐殖质成分表现出不同的分子运动行为,并且可能在纳米尺度上发生空间分离。在这种新的结构背景下,这些成分包括与腐殖质紧密相关的任何分子,以至于它们不能通过化学或物理方法有效分离。因此,按照定义,紧密结合在腐殖质组分中的生物分子就是腐殖质成分,这一结论必然对传统上认为是腐殖质形成所必需的关键生物地球化学途径提出质疑。需要进一步研究以阐明将腐殖质成分连接成超分子缔合的分子间相互作用,并确定这些缔合从有机凋落物降解中产生的途径。