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首页> 外文期刊>Eurasian Soil Science >PHOSPHATE ION SORPTION AND DESORPTION ISOTHERMS IN LOW-BOG PEAT SOILS CONTAINING IRON
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PHOSPHATE ION SORPTION AND DESORPTION ISOTHERMS IN LOW-BOG PEAT SOILS CONTAINING IRON

机译:含铁低沼泽土壤中磷酸盐离子的吸附和脱附等温线

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摘要

The quantity of sorbed and desorbed phosphate ions is determined by the ash content of the peat and its sorption activity. Sorption and desorption isotherms in low-bog peat soils are described by the Freundlich equation. High-ash peat soils containing iron exhibit higher phosphate-sorption activity and less desorption of phosphate ions than pear soils with a normal ash content.
机译:吸附和解吸的磷酸根离子的量取决于泥炭的灰分含量及其吸附活性。低沼泽泥炭土的吸附和解吸等温线由Freundlich方程描述。与具有正常灰分含量的梨土相比,含铁的高灰分泥炭土具有更高的磷酸盐吸附活性和更少的磷酸盐离子解吸。

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