Institut für Geoökologie, Abteilung Umweltgeochemie, Technische Universität Braunschweig, Langer Kamp 19C, Braunschweig 38106, Germany.
Environ Sci Technol. 2022 Feb 15;56(4):2747-2759. doi: 10.1021/acs.est.1c04719. Epub 2022 Feb 1.
Peatlands of the Northern Hemisphere and Central European coniferous forests experience significant environmental change. The resultant browning of surface waters, that is, elevated concentrations of dissolved organic matter (DOM) and metals, is of interest in the context of the global C cycle, peatland and forest management, and water treatment. In an attempt to identify the causes of this process in the Harz Mountains (Central Germany), we studied the spatiotemporal variations in DOM molecular composition (thermally assisted hydrolysis and methylation combined with GC-MS) and metal concentrations in headwater stream samples. We found strong relationships between DOM and metals and seasonal variations in the DOM quality and tentatively DOM-metal binding mode: during summer base flow, DOM and metal concentrations are low, and all elements other than the alkali and alkaline earth metals (Ca, Mg, Sr, K, and Na) are positively correlated to DOM, whereas during spring and autumn (high discharge), only metals with strong affinity for DOM (Fe, As, Cu, Cr, Pb, and Ti), but not weakly binding ones (Al, Cd, La, Mn, Ni, Zn, and Zr), are correlated to DOM, indicative of selectivity in DOM-metal interactions. The products of polyphenols are the key ingredients of the DOM-metal complexes. We argue the importance of spruce lignin-derived vanillic acid moieties, which are involved in weak (all seasons) and strong, multidentate and/or colloidal, binding (spring and autumn) of metals. Considering the ongoing spruce forest dieback and climate change acceleration, it is tempting to conclude that spruce necromass and forest soils may release vast amounts of lignin-derived DOM and associated metals to headwater streams. This would have significant implications for forest soil C stocks and the management of connected drinking water reservoirs.
北半球泥炭地和中欧针叶林经历了显著的环境变化。地表水体的褐变,即溶解有机质(DOM)和金属浓度的升高,在全球碳循环、泥炭地和森林管理以及水处理等方面引起了关注。为了尝试在德国中部的哈尔茨山脉确定这一过程的原因,我们研究了源头溪流样本中 DOM 分子组成(热辅助水解和甲基化与 GC-MS 相结合)和金属浓度的时空变化。我们发现 DOM 和金属之间存在很强的关系,以及 DOM 质量的季节性变化和暂定的 DOM-金属结合模式:在夏季基流期间,DOM 和金属浓度较低,除碱金属和碱土金属(Ca、Mg、Sr、K 和 Na)以外的所有元素都与 DOM 呈正相关,而在春季和秋季(高流量)期间,只有对 DOM 具有强烈亲和力的金属(Fe、As、Cu、Cr、Pb 和 Ti),而不是对 DOM 亲和力较弱的金属(Al、Cd、La、Mn、Ni、Zn 和 Zr),与 DOM 相关,表明 DOM-金属相互作用具有选择性。多酚的产物是 DOM-金属配合物的关键成分。我们认为云杉木质素衍生的香草酸部分的重要性,它参与了金属的弱(所有季节)和强、多齿和/或胶体结合(春季和秋季)。考虑到云杉森林衰退和气候变化加速的持续进行,人们不禁要得出结论,云杉枯木和森林土壤可能会向源头溪流释放大量木质素衍生的 DOM 和相关金属。这将对森林土壤碳储量和相关饮用水水库的管理产生重大影响。