HR: 1340h
AN: H43B-0372 [Abstracts]
TI: Geochemical Impacts of CAFOs: Implications for Modifying Existing Regulatory Standards in
Michigan
AU: * Borrello, M C
EM: Borrello@alma.edu
AF: Alma College, 614 W. Superior Street, Alma, MI 48801
United States
AU: Oemke, M P
EM: Oemke@alma.edu
AF: Alma College, 614 W. Superior Street, Alma, MI 48801
United States
AU: Snowdon, L
EM: lissa320@aol.com
AF: Alma College, 614 W. Superior Street, Alma, MI 48801
United States
AU: Farley, A
EM: aafangel06@hotmail.com
AF: Alma College, 614 W. Superior Street, Alma, MI 48801
United States
AB:
Concentrated Animal Feeding Operations (CAFOs), those facilities consisting of 1000 + cattle or hogs, are increasingly among
the most significant sources of agricultural contamination in many surface waters in Michigan and around the country. Many
environmental and rural citizens' groups argue that Michigan law controlling CAFO operations has been inadequate in dealing
with the large volume of nutrient loading observed in streams. Stream impacts due to CAFOs have been measured using the same
traditional biological and geochemical parameters as those used to assess general agricultural runoff. Geochemical
parameters used include: total nitrogen, nitrate and ammonia, total phosphorous, dissolved oxygen (DO) and conductivity.
These parameters are used not only as indicators of stream impact in agricultural states such as Michigan and Indiana but
also provide the basis for regulatory standards.
This study focused on two large CAFOs in which samples were taken in agricultural drains upstream and downstream from known,
historic discharges of these facilities. Traditional analyses of total nitrogen and total phosphorous showed only subtle
differences when comparing the upstream and downstream sites. Differences in DO were more pronounced between the sites
(consistently lower for the downstream locations) but did not offer a direct correlation with presumed CAFO impacts. Other
results, however, suggest that it is possible to isolate CAFO impacts by comparing transient chemical constituents such as
(inorganic) orthophosphate and ammonia and by plotting these comparisons against DO. Ammonia concentrations plotted against
orthophosphate displayed moderate to strong correlation (r = 0.84) for downstream sites but weak correlations (r = 0.04) for
upstream sites. Ammonia and nitrate concentrations correlated strongly for downstream sites (r = 0.58) but weak for upstream
sites (r = 0.09). Also, 24 hour DO analyses of all the sites indicated higher fluctuations throughout the day but only for
the upstream sites. DO appeared to correlate strongly with orthophosphate concentrations (r = 0.68) for the downstream sites
as compared with upstream site correlations (r = 0.058).
If new laws and/or guidelines are to be established that adequately address and mitigate potentially negative impacts on
surface water from CAFOs, a method of geochemical assessment has to be developed that will isolate CAFO impacts from general
agricultural influence. The results of this study suggest that traditional means of assessing agricultural runoff in surface
waters are inadequate in determining short and long-term CAFO impacts on surface water quality. Subtle differences do occur
using traditional geochemical parameters, but using these parameters alone are insufficient and ineffective in providing a
definitive assessment of CAFO impacts relative to the impacts that already exist. What may be needed is a greater focus on
the short-term geochemical relationships between parameters such as ammonia, orthophosphate and dissolved oxygen. State and
federal guidelines regulating CAFO facilities may need to incorporate these types of analyses in order to better assess
future impacts.
DE: 4825 Geochemistry
DE: 1806 Chemistry of fresh water
DE: 1860 Runoff and streamflow
DE: 1871 Surface water quality
DE: 0345 Pollution--urban and regional (0305)
SC: Hydrology [H]
MN: 2004 AGU Fall Meeting