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Changes in dissolved organic matter quality in a peatland and forest headwater stream as a function of seasonality and hydrologic conditions

机译:泥炭地和森林源流中溶解性有机质的变化随季节和水文条件的变化

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Peatlands and peaty riparian zones are major sources of dissolved organic matter?(DOM), but are poorly understood in terms of export dynamics and controls thereof. Thereby quality of DOM affects function and behavior of DOM in aquatic ecosystems, but DOM quality can also help to track DOM sources and their export dynamics under specific hydrologic preconditions. The objective of this study was to elucidate controls on temporal variability in DOM concentration and quality in stream water draining a bog and a forested peaty riparian zone, particularly considering drought and storm flow events. DOM quality was monitored using spectrofluorometric indices for aromaticity?(SUVAsub254/sub), apparent molecular size?(iS/isubR/sub) and precursor organic material?(FI), as well as PARAFAC modeling of excitation emission matrices?(EEMs). brbr Indices for DOM quality exhibited major changes due to different hydrologic conditions, but patterns were also dependent on season. Stream water at the forested site with mineral, peaty soils generally exhibited higher variability in DOM concentrations and quality compared to the outflow of an ombrotrophic bog, where DOM was less susceptible to changes in hydrologic conditions. During snowmelt and spring events, near-surface protein-like DOM pools were exported. A microbial DOM fraction originating from groundwater and deep peat layers was increasing during drought, while a strongly microbially altered DOM fraction was also exported by discharge events with dry preconditions at the forested site. This might be due to accelerated microbial activity in the peaty riparian zone of the forested site under these preconditions. Our study demonstrated that DOM export dynamics are not only a passive mixing of different hydrological sources, but monitoring studies have to consider that DOM quality depends on hydrologic preconditions and season. Moreover, the forested peaty riparian zone generated the most variability in headwater DOM quantity and quality, as could be tracked by the used spectrofluorometric indices.
机译:泥炭地和河岸带是溶解性有机物(DOM)的主要来源,但在出口动态及其控制方面知之甚少。因此,DOM的质量会影响DOM在水生生态系统中的功能和行为,但是DOM的质量还可以帮助跟踪特定水文条件下的DOM来源及其出口动态。这项研究的目的是阐明对排泄沼泽和林木的河岸带的溪流中DOM浓度和质量的时间变化的控制,特别是考虑到干旱和暴风雨事件。使用分光荧光指数监测DOM质量,以测定芳香度?(SUVA 254 ),表观分子大小( S R )和前体有机物质? FI),以及激发发射矩阵(EEM)的PARAFAC建模。 DOM质量指标由于水文条件不同而发生了重大变化,但模式也取决于季节。与矿物营养丰富的沼泽的流出相比,DOM较不易受到水文条件变化的影响,与矿物养成的土壤相比,林地中的溪流水在DOM浓度和质量方面通常表现出更高的变异性。在融雪和春季事件期间,出口了近表面的类蛋白质DOM池。在干旱期间,源自地下水和深层泥炭层的微生物DOM含量在增加,而在森林地带,由于干旱条件下的排放事件,微生物产生的DOM含量也发生了强烈变化。在这些前提下,这可能是由于森林站点的豆类河岸带微生物活动加快所致。我们的研究表明,DOM出口动态不仅是不同水文资源的被动混合,而且监测研究还必须考虑DOM质量取决于水文前提和季节。而且,如使用的荧光分光光度指数所跟踪的那样,林木的河岸带产生的水源DOM数量和质量变化最大。

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