Geological Faculty, Moscow State University, Leninskie Gory 1, 119234, Moscow, Russia.
Geological Faculty, Moscow State University, Leninskie Gory 1, 119234, Moscow, Russia; Scientific Geoinformation Center of Russian Academy of Sciences, New Arbat 11/1, 119019, Moscow, Russia.
Chemosphere. 2020 Jul;250:126216. doi: 10.1016/j.chemosphere.2020.126216. Epub 2020 Feb 14.
Photodegradation of dissolved organic matter (DOM) is highly important in humic waters of peatland regions, yet the coupling between organic and organo-mineral colloids, trace metals and bioavailability of photodegraded products is poorly known. Here we studied photo-destruction of organo-mineral colloids induced by UV-irradiation of sterile-filtered mire water. We revealed two simultaneously occurring processes of transformation of DOM and trace elements speciation: (i) disintegration of high molecular weight organo-mineral colloids into lower molecular weight (<1 kDa) DOM and metal complexes and (ii) formation of particulate (>0.22 μm) aggregates of metals and organic matter. Over 26 days of UV-irradiation, up to 20% of dissolved organic carbon from peat waters was transformed into CO. In addition to transformation of organic compounds, sizeable change in speciation and size fractionation of many trace metals such as Fe, Pb, Cd, Co, Zn, Cu, V, La, Ni and Cr occurred. Although short-term (1 day) UV-irradiation of mire water stimulated growth of cultivable Pseudomonas sp. bacterium, the long-term exposure (26 days) of organic substrate had a negative effect on bacterial development. Therefore, while sizeable transformation of the organic and metal colloidal load of peat water may occur over first 10 days of UV-irradiation, the enhanced bioavailability of UV-treated substrate is achieved after first day of exposure. The present study demonstrates the importance of even short-term UV-irradiation on colloidal transformation and potential bioavailability of humic waters from temperate mires and highlights the need for more detailed study of coupled metal-organic matter transformation induced by sunlight exposure of mire waters.
在泥炭地地区的腐殖质水中,溶解性有机质(DOM)的光降解非常重要,但有机和有机-矿物胶体、痕量金属以及光降解产物的生物可利用性之间的耦合关系知之甚少。在这里,我们研究了无菌过滤的沼泽水经紫外线辐照诱导的有机-矿物胶体光降解。我们揭示了 DOM 和痕量元素形态同时发生的两个转化过程:(i)高分子量有机-矿物胶体分解成低分子量(<1 kDa)DOM 和金属络合物,(ii)金属和有机物形成颗粒(>0.22 µm)聚集体。在 26 天的紫外线辐照下,来自泥炭水的溶解有机碳中有高达 20%转化为 CO。除了有机化合物的转化外,许多痕量金属如 Fe、Pb、Cd、Co、Zn、Cu、V、La、Ni 和 Cr 的形态和大小分级也发生了相当大的变化。尽管沼泽水的短期(1 天)紫外线辐照刺激了可培养假单胞菌的生长,但长期(26 天)暴露于有机基质对细菌的发展有负面影响。因此,虽然在紫外线辐照的前 10 天内,泥炭水中的有机和金属胶体负荷可能会发生大量转化,但在暴露于紫外线后的第一天,处理后的基质的生物利用度会提高。本研究表明,即使是短期的紫外线辐照对温带泥炭地腐殖质水中胶体转化和潜在生物可利用性也很重要,并强调需要更详细地研究阳光照射对泥炭水引起的金属-有机物质耦合转化。