Catchment influence on nitrate and dissolved organic matter in Alaskan streams across a latitudinal gradient
Abstract
Spatial patterns in carbon (C) and nitrogen (N) cycles of high-latitude catchments have been linked to climate and permafrost and used to infer potential changes in biogeochemical cycles under climate warming. However, inconsistent spatial patterns across regions indicate that factors in addition to permafrost and regional climate may shape responses of C and N cycles to climate change. In this paper, we hypothesized that physical attributes of catchments modify responses of C and N cycles to climate and permafrost. We measured dissolved organic C (DOC) and nitrate (NO3¯) concentrations, and composition of dissolved organic matter (DOM) in 21 streams spanning boreal to arctic Alaska, and assessed permafrost, topography, and attributes of soils and vegetation as predictors of stream chemistry. Multiple regression analyses indicated that catchment slope is a primary driver, with lower DOC and higher NO3¯ concentration in streams draining steeper catchments, respectively. Depth of the active layer explained additional variation in concentration of DOC and NO3¯. Vegetation type explained regional variation in concentration and composition of DOM, which was characterized by optical methods. Composition of DOM was further correlated with attributes of soils, including moisture, temperature, and thickness of the organic layer. Finally, regional patterns of DOC and NO3¯more »
- Authors:
-
- Univ. of Alaska, Fairbanks, AK (United States). Inst. of Arctic Biology. Dept. of Biology and Wildlife
- Nevada State College, Henderson, NV (United States). Dept. of Physical and Life Sciences
- Univ. of Alaska, Fairbanks, AK (United States). Inst. of Arctic Biology
- Western Univ., London, ON (Canada). Dept. of Biology
- Oak Ridge National Lab. (ORNL), Oak Ridge, TN (United States). Climate Change Science Inst.
- Publication Date:
- Research Org.:
- Univ. of Alaska, Fairbanks, AK (United States); Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States)
- Sponsoring Org.:
- USDOE; National Science Foundation (NSF)
- Contributing Org.:
- Nevada State College, Henderson, NV (United States); Western Univ., London, ON (Canada)
- OSTI Identifier:
- 1352809
- Grant/Contract Number:
- AC05-00OR22725; OPP-0817056
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Journal of Geophysical Research. Biogeosciences
- Additional Journal Information:
- Journal Volume: 121; Journal Issue: 2; Journal ID: ISSN 2169-8953
- Publisher:
- American Geophysical Union
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 59 BASIC BIOLOGICAL SCIENCES; 54 ENVIRONMENTAL SCIENCES; 37 INORGANIC, ORGANIC, PHYSICAL, AND ANALYTICAL CHEMISTRY; arctic tundra; boreal forest; catchment; dissolved organic carbon; nitrate; permafrost
Citation Formats
Harms, Tamara K., Edmonds, Jennifer W., Genet, Hélène, Creed, Irena F., Aldred, David, Balser, Andrew, and Jones, Jeremy B. Catchment influence on nitrate and dissolved organic matter in Alaskan streams across a latitudinal gradient. United States: N. p., 2016.
Web. doi:10.1002/2015JG003201.
Harms, Tamara K., Edmonds, Jennifer W., Genet, Hélène, Creed, Irena F., Aldred, David, Balser, Andrew, & Jones, Jeremy B. Catchment influence on nitrate and dissolved organic matter in Alaskan streams across a latitudinal gradient. United States. https://doi.org/10.1002/2015JG003201
Harms, Tamara K., Edmonds, Jennifer W., Genet, Hélène, Creed, Irena F., Aldred, David, Balser, Andrew, and Jones, Jeremy B. Sun .
"Catchment influence on nitrate and dissolved organic matter in Alaskan streams across a latitudinal gradient". United States. https://doi.org/10.1002/2015JG003201. https://www.osti.gov/servlets/purl/1352809.
@article{osti_1352809,
title = {Catchment influence on nitrate and dissolved organic matter in Alaskan streams across a latitudinal gradient},
author = {Harms, Tamara K. and Edmonds, Jennifer W. and Genet, Hélène and Creed, Irena F. and Aldred, David and Balser, Andrew and Jones, Jeremy B.},
abstractNote = {Spatial patterns in carbon (C) and nitrogen (N) cycles of high-latitude catchments have been linked to climate and permafrost and used to infer potential changes in biogeochemical cycles under climate warming. However, inconsistent spatial patterns across regions indicate that factors in addition to permafrost and regional climate may shape responses of C and N cycles to climate change. In this paper, we hypothesized that physical attributes of catchments modify responses of C and N cycles to climate and permafrost. We measured dissolved organic C (DOC) and nitrate (NO3¯) concentrations, and composition of dissolved organic matter (DOM) in 21 streams spanning boreal to arctic Alaska, and assessed permafrost, topography, and attributes of soils and vegetation as predictors of stream chemistry. Multiple regression analyses indicated that catchment slope is a primary driver, with lower DOC and higher NO3¯ concentration in streams draining steeper catchments, respectively. Depth of the active layer explained additional variation in concentration of DOC and NO3¯. Vegetation type explained regional variation in concentration and composition of DOM, which was characterized by optical methods. Composition of DOM was further correlated with attributes of soils, including moisture, temperature, and thickness of the organic layer. Finally, regional patterns of DOC and NO3¯ concentrations in boreal to arctic Alaska were driven primarily by catchment topography and modified by permafrost, whereas composition of DOM was driven by attributes of soils and vegetation, suggesting that predicting changes to C and N cycling from permafrost-influenced regions should consider catchment setting in addition to dynamics of climate and permafrost.},
doi = {10.1002/2015JG003201},
journal = {Journal of Geophysical Research. Biogeosciences},
number = 2,
volume = 121,
place = {United States},
year = {Sun Jan 10 00:00:00 EST 2016},
month = {Sun Jan 10 00:00:00 EST 2016}
}
Web of Science
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Assessing inter-annual and seasonal patterns of DOC and DOM quality across a complex alpine
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- Hydrology and Earth System Sciences