The significance of storms for the concentration and export of dissolved organic carbon from two Precambrian Shield catchments

Dissolved organic carbon (DOC) concentrations and DOC export arestudied during storms to examine the relationship between DOCconcentration and stream discharge and to assess the importance of stormson DOC export. Storms were monitored in seven subcatchments within twosmall watersheds (Harp 4--21 and Harp 3A) on the Precambrian Shield inCentral Ontario, Canada. Stream DOC concentrations increase during stormsby as much as 100% and 410% in Harp3A and Harp 4--21 respectively. The seasonal regression between DOC andstream discharge is significant in subcatchments without wetlands(r2 > 0.7) but is not significant in thetwo subcatchments with small wetland areas (r2 <0.06). On average, regressions based on weekly data yield accurate estimatesof DOC export but the variation in regressions among individual storms andthe small number of high DOC samples result in uncertainties of more than30% in DOC export. The period-weighted calculation ofDOC export from weekly data underestimates export by 14%and 22% in Harp 3A and Harp 4--21 respectively. Stormswere responsible for 57% to 68% of theDOC export in the autumn and 29% to 40%of the DOC export in the spring. A single large storm accounted for31% of the autumn DOC export in Harp 3A. The importanceof individual storms for DOC export and the variation in the relationshipbetween DOC and stream discharge among storms make it difficult to predictthe effects of climate change on DOC export and DOC concentrations.

[1]  J. Hewlett Factors affecting the response of small watersheds to precipitation in humid areas , 1967 .

[2]  W. McDowell,et al.  Autumnal Processing of Dissolved Organic Matter in a Small Woodland Stream Ecosystem , 1976 .

[3]  J. Zachara,et al.  ROLE OF SOLUBLE ORGANICS IN THE SOIL PROCESSES OF A PODZOL, CENTRAL CASCADES, WASHINGTON , 1978 .

[4]  Arthur H. Johnson,et al.  Estimating solute transport in streams from grab samples , 1979 .

[5]  J. A. Watts,et al.  Transport of organic carbon to the oceans by rivers of North America: a synthesis of existing data '' , 1982 .

[6]  Cathy M. Tate,et al.  The Effects of Watershed Disturbance on Dissolved Organic Carbon Dynamics of a Stream , 1983 .

[7]  K. N. Eshleman,et al.  The Role of Organic Acids in the Acid‐Base Status of Surface Waters at Bickford Watershed, Massachusetts , 1985 .

[8]  E. M. Thurman,et al.  Organic Geochemistry of Natural Waters , 1985, Developments in Biogeochemistry.

[9]  W. H. Dowell Kinetics and mechanisms of dissolved organic carbon retention in a headwater stream , 1985 .

[10]  E. S. Corbett,et al.  Comparison of Methods for Estimating Sulfate Export from a Forested Watershed , 1986 .

[11]  W. McDowell,et al.  Origin, Composition, and Flux of Dissolved Organic Carbon in the Hubbard Brook Valley , 1988 .

[12]  J. McCarthy,et al.  Mechanisms of dissolved organic carbon adsorption on soil , 1989 .

[13]  T. Moore,et al.  Dynamics of dissolved organic carbon in forested and disturbed catchments, Westland, New Zealand: 1. Maimai , 1989 .

[14]  C. Driscoll,et al.  The role of organic acids in the acidification of surface waters in the Eastern U.S. , 1989 .

[15]  J. Houghton,et al.  Climate change : the IPCC scientific assessment , 1990 .

[16]  T. Moore,et al.  Controls on dissolved organic carbon concentrations in streams, southern Québec , 1990 .

[17]  J. Baldock,et al.  Concentration and composition of dissolved organic carbon in streams in relation to catchment soil properties , 1993 .

[18]  H. Seip,et al.  Dissolved organic carbon fractions in soil and stream water during variable hydrological conditions at Birkenes, southern Norway. , 1992 .

[19]  R. Maclean The role of the vadose zone in the generation of runoff from a headwater basin in the Canadian shield , 1992 .

[20]  S. Schiff,et al.  Physical properties governing groundwater flow in a glacial till catchment , 1993 .

[21]  K. Bencala,et al.  Hydrological controls on dissolved organic carbon during snowmelt in the Snake River near Montezuma, Colorado , 1994 .

[22]  S. Schiff,et al.  Examining the contributions of glacial till water to storm runoff using two‐ and three‐component hydrograph separations , 1994 .

[23]  P. Dillon,et al.  Dissolved organic and inorganic carbon mass balances in central Ontario lakes , 1997 .

[24]  S. Schiff,et al.  Export of DOC from forested catchments on the Precambrian Shield of Central Ontario: Clues from 13C and 14C , 1997 .

[25]  S. Schiff,et al.  Sources and flowpaths of dissolved organic carbon during storms in two forested watersheds of the Precambrian Shield , 1998 .