Agrogenic evolution of phosphate fractional composition of Polesye peat soils

The results of the research on studying the influence of drainage and long agricultural use (50 years) of peat soils on the transformation and content evolution as well as on the structure of phosphate fractions are presented. Under the influence of anthropogenic factors along with the reduced content...

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Published inВесцi Нацыянальнай акадэмii навук Беларусi. Серыя аграрных навук no. 4; pp. 37 - 43
Main Author Semenenko, N.N., National Academy of Sciences. Scientific and Practical Center for Arable Farming (Belarus). Institute for Land Reclamation
Format Journal Article
LanguageRussian
Published 2012
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Abstract The results of the research on studying the influence of drainage and long agricultural use (50 years) of peat soils on the transformation and content evolution as well as on the structure of phosphate fractions are presented. Under the influence of anthropogenic factors along with the reduced content of organic matter in soil the equity participation of organic compounds also decreases from 88 to 62% and mineral compounds specifi c weight increases. Relative reserves of mobile (from 5 to 35%), accessible (from 0.8 to 6.8%) and easily accessible (from 0.8 to 5.8%) phosphate compounds increase. As soon as the content of organic matter in soils reduces their phosphate fund becomes more 'crumbly'.
AbstractList The results of the research on studying the influence of drainage and long agricultural use (50 years) of peat soils on the transformation and content evolution as well as on the structure of phosphate fractions are presented. Under the influence of anthropogenic factors along with the reduced content of organic matter in soil the equity participation of organic compounds also decreases from 88 to 62% and mineral compounds specifi c weight increases. Relative reserves of mobile (from 5 to 35%), accessible (from 0.8 to 6.8%) and easily accessible (from 0.8 to 5.8%) phosphate compounds increase. As soon as the content of organic matter in soils reduces their phosphate fund becomes more 'crumbly'.
Author Semenenko, N.N., National Academy of Sciences. Scientific and Practical Center for Arable Farming (Belarus). Institute for Land Reclamation
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DocumentTitle_FL Агрогенная эволюция фракционного состава фосфатов торфяных почв ПолесьÑ
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Snippet The results of the research on studying the influence of drainage and long agricultural use (50 years) of peat soils on the transformation and content evolution...
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SubjectTerms ANAILISIS DEL SUELO
ANALYSE DE SOL
BA©LARUS
BELARUS
CHEMICAL SOIL TYPES
CHIMIE DU SOL
FERTILIDAD DEL SUELO
FERTILITA© DU SOL
http://www.fao.org/aos/agrovoc#c_13929
http://www.fao.org/aos/agrovoc#c_1519
http://www.fao.org/aos/agrovoc#c_33237
http://www.fao.org/aos/agrovoc#c_5648
http://www.fao.org/aos/agrovoc#c_7161
http://www.fao.org/aos/agrovoc#c_7170
http://www.fao.org/aos/agrovoc#c_7182
http://www.fao.org/aos/agrovoc#c_7198
PEAT SOILS
PEATLANDS
PROPIEDADES FA­SICO - QUA­MICAS SUELO
PROPRIA©TA© PHYSICOCHIMIQUE DU SOL
QUA­MICA DEL SUELO
SOIL ANALYSIS
SOIL CHEMICOPHYSICAL PROPERTIES
SOIL CHEMISTRY
SOIL FERTILITY
SOL TOURBEUX
SUELO TURBOSO
TIPOS QUA­MICOS DE SUELOS
TOURBIAЁRE
TURBERAS
TYPE DE SOL CHIMIQUE
Title Agrogenic evolution of phosphate fractional composition of Polesye peat soils
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