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  • Low capacity of acid sandy soils to bind P is a reason for its leaching and runoff. Different soil amendments are used to reduce P leaching. This study was conducted to show the effect of CaCO3, dolomite, gypsum, and CaCl2 on P retention by the Ap horizon of a Spodosol. Phosphorus sorption was studied in a batch experiment at an initial P concentration range 0 to 10 mg L-1. The amendment rate of 0.05 mmol Ca (or Ca+Mg) (and also 0.1 mmol in case of CaCO3 and gypsum) per g of soil was used. The influenceof time after soil amendment (1 h to 1 wk) on P retention was assessed. The adsorption of P was described by Langmuir and Freundlich equations. All amendments except for CaCl2 increased soil pH and P retention by soil. CaCO3 was more effective then dolo mite. The carbonates (CaCO3 and dolomite) were more effective in their interaction with soil. Gypsum increased P retention by itself; upon interaction with soil, its effect was weakened. Sorption of P in soil amended with gypsum is faster than sorption i
  • Low capacity of acid sandy soils to bind P is a reason for its leaching and runoff. Different soil amendments are used to reduce P leaching. This study was conducted to show the effect of CaCO3, dolomite, gypsum, and CaCl2 on P retention by the Ap horizon of a Spodosol. Phosphorus sorption was studied in a batch experiment at an initial P concentration range 0 to 10 mg L-1. The amendment rate of 0.05 mmol Ca (or Ca+Mg) (and also 0.1 mmol in case of CaCO3 and gypsum) per g of soil was used. The influenceof time after soil amendment (1 h to 1 wk) on P retention was assessed. The adsorption of P was described by Langmuir and Freundlich equations. All amendments except for CaCl2 increased soil pH and P retention by soil. CaCO3 was more effective then dolo mite. The carbonates (CaCO3 and dolomite) were more effective in their interaction with soil. Gypsum increased P retention by itself; upon interaction with soil, its effect was weakened. Sorption of P in soil amended with gypsum is faster than sorption i (en)
Title
  • Phosphorus retention by the Ap horizon of a Spodosol as influenced by calcium amendments
  • Phosphorus retention by the Ap horizon of a Spodosol as influenced by calcium amendments (en)
skos:prefLabel
  • Phosphorus retention by the Ap horizon of a Spodosol as influenced by calcium amendments
  • Phosphorus retention by the Ap horizon of a Spodosol as influenced by calcium amendments (en)
skos:notation
  • RIV/60460709:41210/03:00005841!RIV/2004/GA0/412104/N
http://linked.open.../vavai/riv/strany
  • 699-706
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(GA526/02/1516)
http://linked.open...iv/cisloPeriodika
  • 10
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 620805
http://linked.open...ai/riv/idVysledku
  • RIV/60460709:41210/03:00005841
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • Phosporus;Sorption;Spodosol;Acid soil;Calcium amendments;Limestone;Gypsum (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • US - Spojené státy americké
http://linked.open...ontrolniKodProRIV
  • [C3C6C033FBC9]
http://linked.open...i/riv/nazevZdroje
  • Soil Science
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...ocetUcastnikuAkce
http://linked.open...nichUcastnikuAkce
http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 168
http://linked.open...iv/tvurceVysledku
  • Borůvka, Luboš
  • Rechcigl, J. E.
issn
  • 0038-075X
number of pages
http://localhost/t...ganizacniJednotka
  • 41210
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