COS 140-4 - Altered urban hydrology: Effects on the transport of organic matter in streams

Thursday, August 9, 2007: 2:30 PM
F1, San Jose McEnery Convention Center
Kenneth T. Belt1, Sujay S. Kaushal2, Christopher M. Swan3, Richard Pouyat4, Peter M. Groffman5, Istvan Turcsanyi6 and William Greenwood6, (1)Northern Research Station, US Forest Service, Baltimore, MD, (2)Department of Geology and Earth System Science Interdisciplinary Center, University of Maryland, College Park, MD, (3)Geography and Environmental Systems, University of Maryland, Baltimore County, Baltimore, MD, (4)Chesapeake Bay Career Consulting, (5)Cary Institute of Ecosystem Studies, Millbrook, NY, (6)UMBC Center for Urban and Environmental Research and Education, Baltimore, MD
The large anthropogenic drainage densities of urban catchments facilitate OM (organic matter) transport, creating a “gutter subsidy” to streams that likely dwarfs riparian input.  Storm and dry weather DOC (dissolved organic carbon), TSS (total suspended solids), and FPOM (fine particulate OM) sample results from twelve streams of the BES LTER urban stream network revealed temporally dynamic systems greatly influenced by land cover, with high OM fluxes and concentrations.

Summer DOC concentrations were lowest at the 3 streams with the most vegetated catchments (mean of 1.3 mg/l), and highest in the urban streams (3.3 mg/l), with suburban streams having intermediate values (2.2 mg/l).  Additionally, a mean of 8.5 mg/l was seen in a residential storm drain groundwater flow.  Mean areal summer instantaneous DOC fluxes at forested, suburban and urban streams were 0.18, 0.41 and 0.85 mg/s/ha, respectively (5.5, 12.6, 26.1 kg/ha/yr).

Mean dry weather FPOM concentrations ranged from 0.38 mg/l (restored suburban) to 2.77 mg/l (forested).  OM % (of TSS) ranged from 13% (restored suburban) to 31 % (forested), to 62% at a sewage impacted underground stream.  Flows influenced by recent storms had higher FPOM concentrations, by factors of 18 (forested), 23 (suburban) and 5 (urban).  At a suburban stream storm monitoring station, TSS and FPOM concentrations responded strongly to flow rate (power function slopes of 0.67 and 0.42 respectively).  The % organic matter (of TSS), however, decreased with flow rate (slope = -0.25).

These results suggest that urban catchments, with their altered drainage pathways and strong terrestrial-aquatic linkages, can transport appreciable quantities of dissolved and particulate organic matter.  This has implications for aquatic food webs and productivity, and for pollutant fates.  It also suggests that restoration might play a role in facilitating the retention of this OM to the advantage of the aquatic community.

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