Y. Ouyang et Rs. Mansell, Potential impacts of density-driven pesticide transport upongroundwater contamination: Modeling, SOIL CROP, 59, 2000, pp. 150-159
Citations number
30
Categorie Soggetti
Agriculture/Agronomy
Journal title
SOIL AND CROP SCIENCE SOCIETY OF FLORIDA PROCEEDINGS
Pollution of groundwater resources by accidental pesticide spillage has lon
g been an environmental concern. Spills involving concentrated mixtures of
water-soluble pesticides such as acephate (acetylphosphoramidothioic acid O
,S-dimethyl ester) may result in very high contaminant concentrations in lo
cal groundwater resources. Localized high concentrations in the aqueous pha
se may actually increase the fluid density above that of ambient groundwate
r. If local increases in fluid density are substantial, density-coupled flu
id flow and chemical transport may result due to the local gravitational bu
oyancy force. The USEPA supported FEMWATER model was used to investigate im
pacts of the density-driven force upon water flow and acephate transport ac
ross a layered and slightly sloping landscape with a pond located down-slop
e from a spill site. A hypothetical water-saturated soil consisting of sand
, clay, and silt/sand horizons with a surface area of 18 by 36 m was used i
n this study. A 1 h spillage of an acephate solution (concentration = 790 k
g m(-3), density = 1350 kg m(-3)) to the top of the groundwater table was u
sed as a contaminant point source. In general, significant impacts of the d
ensity-driven force upon the longitudinal and vertical transport distances
of acephate became profound as time elapsed. Specifically, the longitudinal
transport distance was shorter and the vertical transport distance was dee
per when the density-driven force was employed. Although simulation results
suggested that density-driven transport of acephate would be significant,
an analysis of water heads and flow velocity vectors revealed that effects
of density-driven water flow were minimal except initially in the immediate
vicinity of the spill. Simulations further demonstrated that the presence
of slowly permeable clay and silt/sand layers beneath the rapidly permeable
sand layer delayed the vertical transport of acephate.