January 24, 2008
Characterization of Natural Organic Matter in an Ultra-Oligotrophic Lake
T. Schäfer1, V. Chanudet2,3, F. Claret4, and M. Filella2
1Institut für Nukleare Entsorgung (INE), Forschungszentrum Karlsruhe, Germany;
2Department of Inorganic, Analytical, and Applied Chemistry, University of Geneva, Switzerland;
3Institute F.-A. Forel, University of Geneva, Switzerland;
4BRGM, Environment and Process Division, Orleans, France
| ||||||
|
Low-nutrient, or oligotrophic, alpine lakes showing very small quantities of natural organic matter (NOM) have attracted increased interest over the past few years as they are sensitive indicators for a wide variety of anthropogenic stressors including climate changes. We have used a combination of microscopic and spectroscopic tools to investigate the role of mineral colloids and organic macromolecules in Lake Brienz (Switzerland) and its tributaries, the Aare and Lütschine Rivers in creating and/or maintaining severe oligotrophic conditions. Evidence gleaned from transmission electron microscopy (TEM), scanning transmission x-ray microscopy (STXM), and ultra-Fourier transform infrared spectroscopy (µFTIR) shows that NOM sorption onto inorganic settling particles mainly causes the elimination of NOM in the lake (estimated to be 25% from mass balances).
Combining spectromicroscopic methods with NOM measurements using the classical MBTH (3-methyl-2 benzothiazolinone hydrochloride) method for carbohydrate determination and a new voltammetric method for the determination of refractory organic matter (ROM) made it possible, for the first time, to quantify the types, functionalities, sources, and fate of submicron NOM present in an ultra-oligotrophic lake (Lake Brienz, Switzerland) and its two tributaries, the Aare and Lütschine rivers (Figure 1).
NOM concentrations remained extremely low throughout the year (<1 mg C•L-1) with carbohydrate concentrations of 0.06–0.43 mg C•L-1 in the lake and 0.06–0.25 mg C•L-1 in the two tributary rivers. Pedogenic ROM is a major source of organic material in Lake Brienz with concentrations in the lake of 0.1–0.2 mg C•L-1. Melting snow was responsible for about 32% of the lake's annual ROM input. The concentration of all types of NOM is at its lowest after lake mixing. One box mass balance calculations showed that about 25% of ROM was lost within the lake that is not accounted for by lake flushing.
Principal component (PCA) and cluster analysis of C1s STXM data of a lake water sample (1 m depth) revealed spectroscopically different regions with a cluster (Figure 2, yellow region) showing a general high optical density (spectra not shown) and no spectral features typically for purely inorganic minerals. Cluster 1 (Figure 2, red region) has a high absorption at the potassium L2,3-edge (orthose, biotite or illite minerals), but relatively weak absorption on the carbon edge (optical density OD ~0.05). Finally, higher amounts of organic structures (OD ~0.12) can be found (Figure 2, green region), either surrounding these inorganic phases as submicron colloidal structures/coatings or as separate submicrometer sized particles. The organics of cluster 1 show a relatively high aliphatic/aromatic ratio with lower amounts of oxygen-containing functional groups, whereas the areas of cluster 2 are highly enriched in carboxyl/carbonyl-type groups. The cluster analysis and high-resolution C1s ratio images (Figure 3) show that inorganic phases are coated by ROM, thus leading to a change in surface charge and therefore influencing colloid/particulate stability.
All organics found in a Lake Brienz sample taken at 100 m depth showed an association to potassium-rich minerals and very
comparable organic functionality to the mineral-associated organic matter of the surface waters. This suggests that sedimentation
of organic material, particularly via the association with K-rich mineral phases, is one of the major organic removal processes
in the lake, thus supporting conclusions from the mass balance study. Almost pure organic material with high amounts of
oxygen-containing functional groups and poor aromatic content, as found in surface waters, could not be detected in deeper zones.
Taken the cluster spectra found for the Aare and Lütschine rivers as target spectra, correlation maps of organic spectral
similarities for the Lake Brienz samples were calculated. 
FTIR analyses are in general good agreement with the C1s results,
although the size of the particles/colloids investigated does not overlap due to the different resolution of the techniques used.
Interestingly, the correlation maps of both methods show that the aggregate structures are built of colloidal/particulate material
with spectral signatures from both tributaries at both sampling depths.
 | |
|
 | |
|
 | |
|
Overall, the results prove that STXM and FTIR are suitable to characterize colloidal
and particulate organic material and its functionality in very low organic carbon systems (< 0.2 mg C•L-1 ROM) and help
to significantly increase the process understanding of carbon cycling in these low nutrient environments.
BEAMLINES
X1A, U10B
FUNDING
Regional government of the Canton Bern
Kraftwerke Oberhasli (KWO)
Bundesamt für Umwelt (BAFU)
Lake Brienz shoreline communities
PUBLICATIONS
Schäfer, T., Chanudet, V., Claret, F., and Filella, M., "Spectromicroscopy Mapping of Colloidal/Particulate Organic Matter in Lake Brienz, Switzerland,"
Environmental Science & Technology, 41, 7864-7869 (2007).
Chanudet, V. and Filella, M., "Submicron organic matter in a peri-alpine, ultra-oligotrophic lake," Organic Geochemistry, 38, 1146-1160 (2007).
FOR MORE INFORMATION
Thorsten Schäfer
Institut für Nukleare Entsorgung (INE) / Institut for Nuclear Waste Disposal (INE)
Forschungszentrum Karlsruhe / Research Center Karlsruhe
Germany
Email: schaefer@ine.fzk.de
Montserrat Filella
Department of Inorganic, Analytical and Applied Chemistry
University of Geneva
Switzerland
Email: montserrat.filella@cabe.unige.ch