Transformation of Dissolved Organic Matter in Aquatic Landscapes

A special issue of Water (ISSN 2073-4441). This special issue belongs to the section "Water Quality and Contamination".

Deadline for manuscript submissions: closed (31 December 2020) | Viewed by 13296

Special Issue Editors


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Guest Editor
University of Lausanne, Lausanne, Switzerland
Interests: dissolved organic matter; transport versus transformation; biogeochemistry; fluvial networks; microbial metabolism; aquatic continuum

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Guest Editor
Helmholtz-Centre for Environmental Research - UFZ
Interests: human impacts on dissolved organic matter sources, fate, and on fluvial macronutrient processing; fluvial ecosystem ecology; fluvial ecosystem concepts

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Guest Editor
1 USGS - Water Mission Area, Boulder, CO, USA;
2 Laboratoire des Sciences du Climat et l'Environnement (LSCE), CNRS-UMR 8212, France
Interests: biodegradation; reactivity; degradation models; dissolved organic carbon; land to ocean continuum

Special Issue Information

Dear Colleagues,

Dissolved organic matter (DOM) is a heterogeneous mixture of organic compounds varying in size and chemical structure that originate from a high diversity of sources, such as soil organic matter, terrestrial and aquatic plants, phytoplankton, bacteria, and fungi. DOM is not only transported in aquatic ecosystems but also subjected to transformation through processes such as flocculation, bio- and photodegradation that interact together and determine the biogeochemical and ecological functioning of aquatic ecosystems from local to global scales. Despite the importance of DOM transformation in the aquatic landscape, major gaps or uncertainties remain on how DOM transformation varies across the aquatic continuum (from headwaters to oceans) as well as regarding the relative importance of external factors versus intrinsic properties of DOM on its fate. This Special Issue welcomes contributions from field, experimental, and modeling studies that address the controls on DOM transformation along spatial and temporal dimensions and help to reshape the thinking of DOM reactivity in aquatic ecosystems.

Dr. Thibault Lambert
Dr. Daniel Graeber
Dr. Núria Catalán
Guest Editors

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Keywords

  • Dissolved organic matter
  • Degradation
  • Transformation
  • Reactivity
  • Aquatic ecosystems.

Published Papers (4 papers)

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Research

20 pages, 1273 KiB  
Article
Available Dissolved Organic Carbon Alters Uptake and Recycling of Phosphorus and Nitrogen from River Sediments
by Marc Stutter, Daniel Graeber and Gabriele Weigelhofer
Water 2020, 12(12), 3321; https://doi.org/10.3390/w12123321 - 26 Nov 2020
Cited by 10 | Viewed by 2570
Abstract
Concurrent with nutrient pollution, agriculture has significantly impacted the quantity, composition, and bioavailability of catchment-derived dissolved organic carbon (DOC) in stream ecosystems. Based on the stoichiometric theory, we tested the hypothesis that bioavailable DOC will stimulate the heterotrophic uptake of soluble reactive P [...] Read more.
Concurrent with nutrient pollution, agriculture has significantly impacted the quantity, composition, and bioavailability of catchment-derived dissolved organic carbon (DOC) in stream ecosystems. Based on the stoichiometric theory, we tested the hypothesis that bioavailable DOC will stimulate the heterotrophic uptake of soluble reactive P (SRP) and inorganic nitrogen in stream sediments. In a simplified laboratory column flow-through study, we exposed stream sediments to additions of glucose, nitrate, and phosphate alone and in combination (+C, +NP, +CNP), and calculated gross and net changes in DOC and nutrients via a mass balance approach. Our results show that glucose-C increased nutrient uptake, but also that NP additions resulted in the enhanced consumption of both native and added organic C. The effects of C addition were stronger on N than P uptake, presumably because labile C stimulated both assimilation and denitrification, while part of the P uptake was due to adsorption. Internal cycling affected net nutrient uptake due to losses of dissolved organically-complexed P and N (DOP and DON). Overall, our study shows that increases in the stoichiometric availability of organic carbon can stimulate N and P sequestration in nutrient-polluted stream sediments. Future studies are required to assess the effects of complex organic carbon sources on nutrient uptake in stream sediments under different environmental conditions, and whether these stoichiometric relations are relevant for ecosystem management. Full article
(This article belongs to the Special Issue Transformation of Dissolved Organic Matter in Aquatic Landscapes)
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19 pages, 1823 KiB  
Article
Dissolved Organic Matter Quality and Biofilm Composition Affect Microbial Organic Matter Uptake in Stream Flumes
by Gabriele Weigelhofer, Tania Sosa Jirón, Tz-Ching Yeh, Gertraud Steniczka and Matthias Pucher
Water 2020, 12(11), 3246; https://doi.org/10.3390/w12113246 - 19 Nov 2020
Cited by 12 | Viewed by 3023
Abstract
Agriculture delivers significant amounts of dissolved organic matter (DOM) to streams, thereby changing the composition and biodegradability of the aquatic DOM. This study focuses on the interactive effects of DOM quality and biofilm composition on the degradation of DOM in a laboratory flume [...] Read more.
Agriculture delivers significant amounts of dissolved organic matter (DOM) to streams, thereby changing the composition and biodegradability of the aquatic DOM. This study focuses on the interactive effects of DOM quality and biofilm composition on the degradation of DOM in a laboratory flume experiment. Half of the flumes were exposed to light to stimulate algal growth, the other half was shaded. Leachates of deciduous leaves, maize leaves, and cow dung were added to the flumes in a single pulse and changes of DOC (dissolved organic carbon) and nutrient concentrations, DOM composition (absorbance and fluorescence data), chlorophyll-a concentrations, bacterial abundances, and enzymatic activities were recorded over a week. DOM was taken up with rates of 50, 109, and 136 µg DOC L−1 h−1 for dung, leaf, and maize leachates, respectively, in the light flumes and 37, 80, and 170 µg DOC L−1 h−1 in the dark flumes. DOC uptake correlated strongly with initial SRP (soluble reactive phosphorus) and DOC concentrations, but barely with DOM components and indices. Algae mostly stimulated the microbial DOC uptake, but the effects differed among differently aged biofilms. We developed a conceptual model of intrinsic (DOM quality) and external (environmental) controlling factors on DOM degradation, with the microbial community acting as biotic filter. Full article
(This article belongs to the Special Issue Transformation of Dissolved Organic Matter in Aquatic Landscapes)
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15 pages, 2166 KiB  
Article
Influence of Dissolved Organic Matter Sources on In-Stream Net Dissolved Organic Carbon Uptake in a Mediterranean Stream
by Anna Lupon, Núria Catalán, Eugènia Martí and Susana Bernal
Water 2020, 12(6), 1722; https://doi.org/10.3390/w12061722 - 17 Jun 2020
Cited by 6 | Viewed by 3200
Abstract
Studies exploring how different sources of dissolved organic matter (DOM) influence in-stream dissolved organic carbon (DOC) uptake at the ecosystem scale are scarce in the literature. To fill this knowledge gap, we examined the relationship between DOM sources and in-stream net DOC uptake [...] Read more.
Studies exploring how different sources of dissolved organic matter (DOM) influence in-stream dissolved organic carbon (DOC) uptake at the ecosystem scale are scarce in the literature. To fill this knowledge gap, we examined the relationship between DOM sources and in-stream net DOC uptake (UDOC) in a sub-humid Mediterranean stream. We considered four reach-scale scenarios occurring under natural conditions that differed in predominant DOM sources (groundwater, leaf litter, and/or upstream water). Results showed that groundwater inputs favored in-stream net DOC uptake, while leaf litter inputs promoted in-stream net DOC release. However, there was no clear effect of DOM source mixing on the magnitude of UDOC. Further, the variability in UDOC within and among scenarios was mostly explained by stream DOC concentration, suggesting that DOC availability limits microbial activity in this stream. DOM composition became a controlling factor of UDOC variability only during the leaf litter period, when stream DOC concentration was the highest. Together, these results suggest that the capacity of headwater forested streams to process DOC is closely tied to the availability of different DOM sources and how they vary over time and along the river network. Full article
(This article belongs to the Special Issue Transformation of Dissolved Organic Matter in Aquatic Landscapes)
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22 pages, 1598 KiB  
Article
Short-Term Effects of Fertilization on Dissolved Organic Matter in Soil Leachate
by Alexandra Tiefenbacher, Gabriele Weigelhofer, Andreas Klik, Matthias Pucher, Jakob Santner, Walter Wenzel, Alexander Eder and Peter Strauss
Water 2020, 12(6), 1617; https://doi.org/10.3390/w12061617 - 05 Jun 2020
Cited by 18 | Viewed by 3732
Abstract
Besides the importance of dissolved organic matter (DOM) in soil biogeochemical processes, there is still a debate on how agricultural intensification affects the leaching of terrestrial DOM into adjacent aquatic ecosystems. In order to close this linkage, we conducted a short-term (45 day) [...] Read more.
Besides the importance of dissolved organic matter (DOM) in soil biogeochemical processes, there is still a debate on how agricultural intensification affects the leaching of terrestrial DOM into adjacent aquatic ecosystems. In order to close this linkage, we conducted a short-term (45 day) lysimeter experiment with silt loam and sandy loam undisturbed/intact soil cores. Mineral (calcium ammonium nitrate) or organic (pig slurry) fertilizer was applied on the soil surface with a concentration equivalent to 130 kg N ha−1. On average, amounts of leached DOC over 45 days ranged between 20.4 mg (silt loam, mineral fertilizer) and 34.4 mg (sandy loam, organic fertilizer). Both, mineral and organic fertilization of a silt loam reduced concentration of dissolved organic carbon (DOC) in the leachate and shifted its composition towards a microbial-like signature (BIX) with a higher aromaticity (Fi) and a lower molecular size (E2:E3). However, in sandy loam only mineral fertilization affected organic matter leaching. There, lowered DOC concentrations with a smaller molecular size (E2:E3) could be detected. The overall effect of fertilization on DOC leaching and DOM composition was interrelated with soil texture and limited to first 12 days. Our results highlight the need for management measures, which prevent or reduce fast flow paths leading soil water directly into aquatic systems, such as surface flow, fast subsurface flow, or drainage water. Full article
(This article belongs to the Special Issue Transformation of Dissolved Organic Matter in Aquatic Landscapes)
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