Flushing of distal hillslopes as an alternative source of stream dissolved organic carbon in a headwater catchment

TitleFlushing of distal hillslopes as an alternative source of stream dissolved organic carbon in a headwater catchment
Publication TypeJournal Article
Year of Publication2015
AuthorsGannon, JP, Bailey, SW, McGuire, KJ, Shanley, JB
JournalWater Resources Research
Volume51
Issue10
Pagination8114 - 8128
Date Published2015/10/01/
ISBN Number1944-7973
Keywords0486 Soils/pedology, 1804 Catchment, 1860 Streamflow, 1879 Watershed, dissolved organic carbon, hillslope hydrology, Hubbard Brook, hydropedological units, hydropedology, stream chemistry
Abstract

We investigated potential source areas of dissolved organic carbon (DOC) in headwater streams by examining DOC concentrations in lysimeter, shallow well, and stream water samples from a reference catchment at the Hubbard Brook Experimental Forest. These observations were then compared to high-frequency temporal variations in fluorescent dissolved organic matter (FDOM) at the catchment outlet and the predicted spatial extent of shallow groundwater in soils throughout the catchment. While near-stream soils are generally considered a DOC source in forested catchments, DOC concentrations in near-stream groundwater were low (mean = 2.4 mg/L, standard error = 0.6 mg/L), less than hillslope groundwater farther from the channel (mean = 5.7 mg/L, standard error = 0.4 mg/L). Furthermore, water tables in near-stream soils did not rise into the carbon-rich upper B or O horizons even during events. In contrast, soils below bedrock outcrops near channel heads where lateral soil formation processes dominate had much higher DOC concentrations. Soils immediately downslope of bedrock areas had thick eluvial horizons indicative of leaching of organic materials, Fe, and Al and had similarly high DOC concentrations in groundwater (mean = 14.5 mg/L, standard error = 0.8 mg/L). Flow from bedrock outcrops partially covered by organic soil horizons produced the highest groundwater DOC concentrations (mean = 20.0 mg/L, standard error = 4.6 mg/L) measured in the catchment. Correspondingly, stream water in channel heads sourced in part by shallow soils and bedrock outcrops had the highest stream DOC concentrations measured in the catchment. Variation in FDOM concentrations at the catchment outlet followed water table fluctuations in shallow to bedrock soils near channel heads. We show that shallow hillslope soils receiving runoff from organic matter-covered bedrock outcrops may be a major source of DOC in headwater catchments in forested mountainous regions where catchments have exposed or shallow bedrock near channel heads.

URLhttp://onlinelibrary.wiley.com/doi/10.1002/2015WR016927/abstract
Short TitleWater Resour. Res.