DOI: 10.31274/rtd-180813-1712
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Available and inorganic forms of phosphorus in selected Alfisols and Mollisols

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Cited by 3 publications
(2 citation statements)
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References 12 publications
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“…The regional model used in the present study is a modi fication of the model of Corliss (1958 (Protz, 1965;Tembhare, 1973 Cardoso (1957) Corliss (1955) Corliss (1958) Coultas (1951) Fenton (I966) Foth (1952); Foth and Riecken (195^) Green (1952)} Green andRiecken (1953) Hutton (1948; Hunter (1950) Hunter, Riecken, and McClelland (1953) (Black, 1968). This release from covalency to ionic bonding upon an increase in base results in a buffering effect and makes an end point arbitrary.…”
Section: Loess Soils In Iowamentioning
confidence: 99%
“…The regional model used in the present study is a modi fication of the model of Corliss (1958 (Protz, 1965;Tembhare, 1973 Cardoso (1957) Corliss (1955) Corliss (1958) Coultas (1951) Fenton (I966) Foth (1952); Foth and Riecken (195^) Green (1952)} Green andRiecken (1953) Hutton (1948; Hunter (1950) Hunter, Riecken, and McClelland (1953) (Black, 1968). This release from covalency to ionic bonding upon an increase in base results in a buffering effect and makes an end point arbitrary.…”
Section: Loess Soils In Iowamentioning
confidence: 99%
“…The depth to the minimum phoaphorua value alao correaponda well with valuea for the Down# aeriea reported by theae reaeachera. The zone of phoaphorua depletion may form due to removal of thia element by planta, tranalocation downward with collodial conatituenta, or leaching in aolution (aneck, 1973;Runge, 1963;Tembhare, 1973;Ridley, 1984).…”
Section: Phyaical and Chemical Parmwteramentioning
confidence: 99%