1978
DOI: 10.1002/esp.3290030108
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Mapping solute loadings in an area of Devon, England

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1981
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Cited by 15 publications
(5 citation statements)
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“…This process, commonly referred to as "snapshot sampling" (Grayson et al, 1997), involves the simultaneous collection of samples at a large number of nested sites within a catchment. Different authors have used this method explicitly to infer the abovementioned relationships between stream water chemistry and hydrochemically effective catchment characteristics (Walling and Webb, 1978;Eyre and Pepperell, 1999;Salvia et al, 1999;Wayland et al, 2003). Biggs et al (2002) used snapshot sampling to model the effect of deforestation on stream solute concentrations.…”
Section: Introductionmentioning
confidence: 99%
“…This process, commonly referred to as "snapshot sampling" (Grayson et al, 1997), involves the simultaneous collection of samples at a large number of nested sites within a catchment. Different authors have used this method explicitly to infer the abovementioned relationships between stream water chemistry and hydrochemically effective catchment characteristics (Walling and Webb, 1978;Eyre and Pepperell, 1999;Salvia et al, 1999;Wayland et al, 2003). Biggs et al (2002) used snapshot sampling to model the effect of deforestation on stream solute concentrations.…”
Section: Introductionmentioning
confidence: 99%
“…In recent years the quality of river water has received increased attention within those subfields of geography concerned with fluvial geomorphology, hydrology, biogeography, and resource analysis (Anderson and Burt, 1978;Douglas, 1972;Turvey, 1975; Walling and Webb, 1978). Geographers have generally neglected to study river transport of nitrogen, though, despite its important role in cultural eutrophication and the possible health hazards associated with high nitrate concentrations in supplies of drinking water.…”
mentioning
confidence: 98%
“…He believed the glaciation responsible to be the Wolstonian and assigned this an age of 130 ka. This gives a rate of removal of 92 m 3 km −2 a −1 , a unit which Walling and Webb (1978) 9-125 River Ouse and Adur, Sussex Collins (1981) 55-132 North Yorks Moors Arnett (1979) 19-54 River Tyne, Northumberland Hall (1967) 70-127 * The Bubnoff, whilst not universally popular, has the advantage that it is numerically the same as either the average rate of surface lowering expressed as mm ka -1 , or the rate of removal of material expressed as m 3 a -1 km -2 . † This value was erroneously reported by Saunders and Young (1983) has the same numerical value as the Bubnoff, so it is not clear how Saunders and Young arrived at their converted figure.…”
Section: Published Data On Rates Of Denudationmentioning
confidence: 99%