1987
DOI: 10.1007/bf01051056
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Estimates of soil phosphorus for different soil series

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Cited by 13 publications
(3 citation statements)
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“…Neither of the current systems employ any modifying or weighting factor based on accompanying information such as soil properties. Soil type was introduced briefly for the north of Scotland (MISR/SAC, 1985) with a recommendation system developed from a combination of long-term field and pot trials coupled with knowledge of differences in the reactivity of P and sorption properties (Reith et al, 1987). While being based on sound experimental understanding and evidence, the practicality of extrapolating an essentially regionally based system up to a national advisory service meant it was never progressed.…”
Section: Discussionmentioning
confidence: 99%
“…Neither of the current systems employ any modifying or weighting factor based on accompanying information such as soil properties. Soil type was introduced briefly for the north of Scotland (MISR/SAC, 1985) with a recommendation system developed from a combination of long-term field and pot trials coupled with knowledge of differences in the reactivity of P and sorption properties (Reith et al, 1987). While being based on sound experimental understanding and evidence, the practicality of extrapolating an essentially regionally based system up to a national advisory service meant it was never progressed.…”
Section: Discussionmentioning
confidence: 99%
“…Their primary interest was change in soil carbon content over 50–70 years. A series of experiments were conducted between 1950 and early 1980s, by the Macaulay Institute of Soil Research (now The James Hutton Institute), to support national agricultural improvements in soil fertility and food security (Reith et al, 1987). Over 30 years, approximately 1000 field experiments were conducted on sites chosen to represent the NE Scotland soil conditions and responses to inorganic P inputs.…”
Section: Methodsmentioning
confidence: 99%
“…Following the digestion of 1 g (dry) soil with a mixture of acids in the proportion of 2.5 mL concentrated HNO 3 and 10 mL concentrated HCl (USEPA, 3050B), Ca concentration in the soil was measured using flame atomic absorption spectrometry (AA-6300 Shimadzu, Japan) at a wave length of 422.7 nm. Particles finer than 2 mm were used for TN, TP and Ca analyses (Reith et al, 1987;.…”
Section: Laboratory Analysismentioning
confidence: 99%