1990
DOI: 10.1016/0016-7061(90)90031-4
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Exchange equilibria of potassium in soils, V. Effect of natural organic matter on K-Ca exchange

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Cited by 13 publications
(7 citation statements)
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“…The small Kv values are in accordance with the results reported for soils containing large amounts of organic matter and noncrystalline aluminum silicates (Goulding 1983). The relatively large Kv values at small EK values may also be attributed to the presence of organic matter and noncrystalline aluminum silicate because soil organic matter, in some soils, contributed positively to the K selectivity (Poonia et al 1986;Poonia and Niederbudde 1990) and because some noncrystalline aluminum silicates having high silica contents exhibited a high K-selectivity (Perrott 1981). Since In Kv decreased quite linearly as EK increased in the relatively small EK range of 0 to 0.1, we used the following equation:…”
Section: Resultssupporting
confidence: 90%
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“…The small Kv values are in accordance with the results reported for soils containing large amounts of organic matter and noncrystalline aluminum silicates (Goulding 1983). The relatively large Kv values at small EK values may also be attributed to the presence of organic matter and noncrystalline aluminum silicate because soil organic matter, in some soils, contributed positively to the K selectivity (Poonia et al 1986;Poonia and Niederbudde 1990) and because some noncrystalline aluminum silicates having high silica contents exhibited a high K-selectivity (Perrott 1981). Since In Kv decreased quite linearly as EK increased in the relatively small EK range of 0 to 0.1, we used the following equation:…”
Section: Resultssupporting
confidence: 90%
“…Recently, Levy et al (1988) have studied K-Ca exchange on kaolinite and kaolinitic soils. Poonia and Niederbudde (1990) and Dhillon and Dhillon (1991a, b) investigated the effect of natural soil organic matter and farmyard manure on the Kselectivity of soils. Datta and Sastry (1991) measured the critical K concentration for the release of non-labile K in soils dominated by micaceous clay minerals.…”
mentioning
confidence: 99%
“…Omalos samples exhibit the lowest K + availability and they are slightly different to La soil samples which are probably connected with increased K leaching due to higher precipitation in Omalos Plateau compared to Lasithi Plateau. In addition, potassium availability in our case is controlled by both illite content and organic matter, which is an unusual case and it is observed only when organic matter contribution in the total CEC is less than 15%, which has been shown by detailed study of Poonia and Niederbudde [52] on the K + absorption in soils. The aforementioned is verified by the weak interrelation of OM% and CEC as revealed in PCA (Figure 2(b)).…”
Section: +supporting
confidence: 67%
“…The qualitative nature of the soil substrate and their quantitative proportion of surface reactivity, referred as surface charge density (SCD), control the rate of SOC sequestration. Increase in organic C enhances SCD of the soil and the ratio of internal/external exchange sites (Poonia and Niederbudde, 1990). It may be mentioned that the dominant soils in SAT environments are black soils (Vertisols and their intergrades, with some inclusions of Entisols in the hills) and associated Alfisols.…”
Section: Distribution Of Soil Carbon In Different Soil Orders Of Tropmentioning
confidence: 99%