1972
DOI: 10.1111/j.1365-2427.1972.tb00051.x
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The chemical composition and flow of the South Winterbourne in Dorset

Abstract: Summary Weekly observations were made of the South Winterbourne from October 1970 to December 1971. Flow commenced in November 1970 and ceased in July 1971, a maximum flow of 1.51 m3 s−1 being recorded in January 1971. The chemical composition was not very variable, but nitrate showed a positive correlation with flow.

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Cited by 17 publications
(4 citation statements)
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“…However, the values for r are generally low and never exceed 0.65. The high correlations obtained by Casey & Ladle (1976) and Casey & Newton (1972) were for rivers where there was a much greater range in discharge and/or nitrate concentration. Table 7 shows that correlations and results based on just a small number of samples or for data collected over a short period should be interpreted with care.…”
Section: Multiple Regression Analysismentioning
confidence: 76%
“…However, the values for r are generally low and never exceed 0.65. The high correlations obtained by Casey & Ladle (1976) and Casey & Newton (1972) were for rivers where there was a much greater range in discharge and/or nitrate concentration. Table 7 shows that correlations and results based on just a small number of samples or for data collected over a short period should be interpreted with care.…”
Section: Multiple Regression Analysismentioning
confidence: 76%
“…Casey (1969) and Casey & Newton (1972 studied ionic composition in a number of rivers in the hard water area of Dorset (UK). This may happen to some anions while rain is seeping through agricultural land or in certain springs.…”
Section: River Chemistrymentioning
confidence: 99%
“…This may happen to some anions while rain is seeping through agricultural land or in certain springs. A very typical case is given by Casey & Newton (1972) for the river South Winterbourne (Dorset, UK), where the NO − 3 concentration increased logarithmically from ≈ 1 mg −1 up to 6 mg −1 , while the flow increased from 0.1 to 1.6 m 3 s −1 . Typical examples are the Ca 2+ and HCO − 3 ions, the concentrations of which are fixed by the pH and the solubility product of the CaCO 3 , but this is not always the case in hard waters.…”
Section: River Chemistrymentioning
confidence: 99%
“…Levels recorded from spring water were relatively high (Casey & Newton, 1972 ;Johnston, 1972) but well below the maximum of 1o g m' set by the WHO for drinking water. Nitrate-N levels were higher in winter than summer at Stations 1 and 2 but no clear seasonal pattern was found at the upstream sites .…”
Section: Water Chemistrymentioning
confidence: 99%