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• W2155251384 abstract "Forms of potassium in soils have been a key focus in soil-fertility studies. Clay minerals are the main source of plant nutrients in soil, as their specific surface characteristics determine the release pattern of some important nutrients, such as potassium. Three forms of K consist of unavailable, slowly available and readily available exist in equilibrium in the soil system. Relationships between soil potassium forms within the clay mineralogical suite were determined in twenty four soil samples in three pedons from paddy soils, two from kiwifruit and one from citrus land in the north of Iran. The results showed that, the characteristics of different forms of potassium in adjacent pedons under different land uses depended on their specific clay mineralogy. Mineralogical analyses showed that smectite, illite and vermiculite were the most abundant clay minerals in the studied soils. Mean soluble and exchangeable potassium in paddy soils were rather low compared to non-paddy soils due to potassium fertilization in non-paddy soils. Non-exchangeable potassium in the samples, which was dominated by smectite, was lower than that in samples dominated by vermiculite, hydroxy-interlayer vermiculite (HIV) and illite; this was related to the inability of smectite in potassium fixation. Therefore, taking into account both exchangeable and HNO3-extractable K gives a better indication for K potential and soil-quality management." @default.
• W2155251384 created "2016-06-24" @default.
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• W2155251384 date "2011-01-01" @default.
• W2155251384 modified "2023-09-22" @default.
• W2155251384 title "Clay mineralogy and its relationship with potassium forms in some paddy and non-paddy soils of northern Iran" @default.
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