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Published on: October 29, 2016
Groundwater controls on colloidal transport in forest stream waters
N Gottselig1, J Sohrt2, D Uhlig3
1Institute of Crop Science and Resource Conservation, Soil Science and Soil Ecology, University of Bonn, Nussallee 13, 53115 Bonn, Germany.
Seasonal variations in natural nanoparticles (NNP) and fine colloids in stream water reveal their sources. Groundwater significantly contributes to streamflow year-round, influencing elemental composition.
Area of Science:
- Environmental Science
- Geochemistry
- Hydrology
Background:
- Biogeochemical changes in catchments are reflected in stream water composition.
- Natural nanoparticles (NNP; 1-100 nm) and fine colloids (<300 nm) play a role in element transport.
- Understanding seasonal dynamics of colloids is crucial for catchment science.
Purpose of the Study:
- To investigate seasonal variations in NNP and fine colloids in stream water.
- To determine the origin of NNP and fine colloids based on catchment inflow parameters.
- To assess the role of different water compartments in NNP and fine colloid composition.
Main Methods:
- Annual monitoring of elemental composition of NNP and fine colloids in stream water, precipitation, groundwater, and subsurface flow.
- Analysis of meteorological and hydrological parameters.
- Quantification of org C, Al, Si, P, Ca, Mn, and Fe using Asymmetric Flow Field Flow Fractionation (AF4).
Main Results:
- Colloid-bound elements constituted up to 55% of total element concentrations.
- Highest NNP and fine colloid loads were observed during winter.
- Groundwater was identified as a consistent source of colloidal Ca in stream water.
Conclusions:
- Different water compartments exhibit distinct NNP and fine colloid compositions.
- NNP and fine colloids serve as effective indicators for identifying stream colloid sources.
- This study highlights the under-explored significance of NNP and fine colloids in forest watersheds.
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