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rdf:type
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Description
| - 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)
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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)
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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)
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skos:notation
| - RIV/60460709:41210/03:00005841!RIV/2004/GA0/412104/N
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http://linked.open.../vavai/riv/strany
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http://linked.open...avai/riv/aktivita
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http://linked.open...avai/riv/aktivity
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http://linked.open...iv/cisloPeriodika
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http://linked.open...vai/riv/dodaniDat
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http://linked.open...aciTvurceVysledku
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http://linked.open.../riv/druhVysledku
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http://linked.open...iv/duvernostUdaju
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http://linked.open...titaPredkladatele
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http://linked.open...dnocenehoVysledku
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http://linked.open...ai/riv/idVysledku
| - RIV/60460709:41210/03:00005841
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http://linked.open...riv/jazykVysledku
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http://linked.open.../riv/klicovaSlova
| - Phosporus;Sorption;Spodosol;Acid soil;Calcium amendments;Limestone;Gypsum (en)
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http://linked.open.../riv/klicoveSlovo
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http://linked.open...odStatuVydavatele
| - US - Spojené státy americké
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http://linked.open...ontrolniKodProRIV
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http://linked.open...i/riv/nazevZdroje
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http://linked.open...in/vavai/riv/obor
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http://linked.open...ichTvurcuVysledku
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http://linked.open...cetTvurcuVysledku
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http://linked.open...ocetUcastnikuAkce
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http://linked.open...nichUcastnikuAkce
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http://linked.open...vavai/riv/projekt
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http://linked.open...UplatneniVysledku
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http://linked.open...v/svazekPeriodika
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http://linked.open...iv/tvurceVysledku
| - Borůvka, Luboš
- Rechcigl, J. E.
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issn
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number of pages
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http://localhost/t...ganizacniJednotka
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