1989
DOI: 10.1111/j.1745-6592.1989.tb01022.x
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Contamination of the Sandstone Aquifer of Prince Edward Island, Canada by Aldicarb and Nitrogen Residues

Abstract: Prince Edward Island is wholly dependent upon ground water from a highly permeable fractured sandstone aquifer for all industrial, domestic, agricultural, and potable uses. The contamination of this aquifer by agricultural residues, principally aldicarb and nitrate, has caused concern among Islanders. Ground water quality was monitored between 1985 and 1988 beneath two potato fields to which aldicarb (Temik) was applied at planting once or twice between 1983 and 1986. In May of 1988,12 percent of 48 monitoring… Show more

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Cited by 16 publications
(6 citation statements)
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“…Consequently, if all other factors are held constant, atrazine and DEA are more likely to persist long enough to reach groundwater if the atrazine is applied in cool climates or at cool times of the year than if the herbicide is applied in warm climates or during warm seasons. Several authors have suggested that the effect of temperature may be reinforced by the effects of recharge because cold seasons often coincide with periods of greater precipitation than warm seasons (e.g., Wyman et al, 1985; Jones et al, 1986; Priddle et al, 1989, 1992; Pickett et al, 1990; Porter et al, 1990; Traub‐Eberhard et al, 1994). However, the present study did not observe a statistically significant interaction between airtemp and recharge ( p = 0.94), indicating that the effects of temperature on atrazine residue concentrations in groundwater are independent of the amount of recharge received.…”
Section: Resultsmentioning
confidence: 99%
“…Consequently, if all other factors are held constant, atrazine and DEA are more likely to persist long enough to reach groundwater if the atrazine is applied in cool climates or at cool times of the year than if the herbicide is applied in warm climates or during warm seasons. Several authors have suggested that the effect of temperature may be reinforced by the effects of recharge because cold seasons often coincide with periods of greater precipitation than warm seasons (e.g., Wyman et al, 1985; Jones et al, 1986; Priddle et al, 1989, 1992; Pickett et al, 1990; Porter et al, 1990; Traub‐Eberhard et al, 1994). However, the present study did not observe a statistically significant interaction between airtemp and recharge ( p = 0.94), indicating that the effects of temperature on atrazine residue concentrations in groundwater are independent of the amount of recharge received.…”
Section: Resultsmentioning
confidence: 99%
“…This range of velocities is also applicable to the flow in the unsaturated zone, for the case when portions of the fractures existing in the unsaturated zone become temporarily saturated, as may occur after a significant rainfall or snowmelt event. The number of fractures and their apertures generally decrease with depth, implicitly leading to a decrease of hydraulic conductivity and to the conclusion that the shallow, most active portion of the aquifer is also the most easily contaminated (Francis and Gale ; Priddle et al ).…”
Section: Controls On Recharge and Nitrate Loading To Groundwatermentioning
confidence: 99%
“…In the United States the proportion of the population that relies on groundwater for domestic purposes rises to 51%, with rural areas again being more reliant at 63% of total water use [2]. Sandstone aquifers are a widespread source of drinking water; for example, the province of Prince Edward Island is completely reliant on a fractured sandstone aquifer for all of their water supply [3]. In many locations, especially in rural areas, septic tanks and underground storage tanks are commonly used alongside drinking water wells.…”
Section: Problem Scopementioning
confidence: 99%
“…Sandstone aquifers are a common drinking water source in Canada and around the world. For example, the province of Prince Edward Island (PEI) is completely dependent on a highly permeable fractured sandstone aquifer for all of their industrial, domestic, agricultural, and potable uses [3]. Sandstone aquifers transmit most of their water through joints, fractures, and bedding planes [8].…”
Section: Research Objectivesmentioning
confidence: 99%