COLIFORM CONTAMINATION OF A COASTAL EMBAYMENT - SOURCES AND TRANSPORTPATHWAYS

Citation
Pk. Weiskel et al., COLIFORM CONTAMINATION OF A COASTAL EMBAYMENT - SOURCES AND TRANSPORTPATHWAYS, Environmental science & technology, 30(6), 1996, pp. 1872-1881
Citations number
39
Categorie Soggetti
Environmental Sciences","Engineering, Environmental
ISSN journal
0013936X
Volume
30
Issue
6
Year of publication
1996
Pages
1872 - 1881
Database
ISI
SICI code
0013-936X(1996)30:6<1872:CCOACE>2.0.ZU;2-B
Abstract
Fecal bacterial contamination of nearshore waters has direct economic impacts to coastal communities through the loss of shellfisheries and restrictions of recreational uses. We conducted seasonal measurements of fecal coliform (FC) sources and transport pathways contributing to FC contamination of Buttermilk Bay, a shallow embayment adjacent to Bu zzards Bay, MA. Typical of most coastal embayments, there were no dire ct sewage discharges (i.e., outfalls), and fecal bacteria from human, domestic animal, and wildlife pools entered open waters primarily thro ugh direct deposition or after transport through surface waters or gro undwaters. Direct fecal coliform inputs to bay waters occurred primari ly in winter (December-March) from waterfowl, similar to 33 x 10(12) F C yr(-1) or similar to 67% of the total annual loading. Effects of wat erfowl inputs on bay FC densities were mitigated by their seasonality, wide distribution across the bay surface, and the apparent limited di spersal from fecal pellets. On-site disposal of sewage by septic syste ms was the single largest FC source in the watershed-embayment system, 460 x 10(12) FC yr(-1), but due to attenuation during subsurface tran sport only a minute fraction, < 0.006 x 10(12) FC yr(-1), reached bay waters (< 0.01% of annual input to bay). Instead, surface water flows, via storm drains and natural streams under both wet- and dry-weather conditions, contributed the major terrestrial input, 12 x 10(12) FC yr (-1) (24% of annual input), all from animal sources. Since most of the surface water FC inputs were associated with periodic, short-duration rain events with discharge concentrated in nearshore zones, wet-weath er flows were found to have a disproportionately high impact on nearsh ore FC levels. Elution of FC from shoreline deposits of decaying veget ation (wrack) comprised an additional coliform source.