2017
DOI: 10.1016/s1002-0160(17)60380-1
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Kinetics of Soil Potassium Release Under Long-Term Imbalanced Fertilization in Calcareous Soils

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Cited by 6 publications
(5 citation statements)
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“…This behavior documented before in the application of vermicompost, zeolite, and a combination of both to release potassium and in another study about the release of potassium from soil amended with clinoptilolite zeolite and corn stalk charcoal. , Furthermore, the release of potassium from zeolite F was derived from feldspar powder . Limestone soils (chloritic and kaolinitic) also exhibit this mechanism …”
Section: Resultssupporting
confidence: 87%
See 1 more Smart Citation
“…This behavior documented before in the application of vermicompost, zeolite, and a combination of both to release potassium and in another study about the release of potassium from soil amended with clinoptilolite zeolite and corn stalk charcoal. , Furthermore, the release of potassium from zeolite F was derived from feldspar powder . Limestone soils (chloritic and kaolinitic) also exhibit this mechanism …”
Section: Resultssupporting
confidence: 87%
“…92 Limestone soils (chloritic and kaolinitic) also exhibit this mechanism. 93 A similar pattern was observed in previous studies with soils. 94 According to the literature, in soils, the faster release at the beginning of the process is normally related to the exit of the cations from the surface sites.…”
Section: Response Optimizationmentioning
confidence: 99%
“…The evaluation of K kinetics is based on the extraction of K at different times. Based on previous research, the CaCl 2 method is recommended for determining the rate of K release in calcareous soils [29][30][31]. In the current study, K was extracted by 0.01 mol L −1 CaCl 2 after incubation (25 ± 1 • C) periods of 1, 3, 7, 14, 21, 30, 50, and 80 days [30].…”
Section: Kinetic Release Of Soil Potassium (K)mentioning
confidence: 98%
“…For all soils, the slope derived from the power function was less than one, indicating that the K-release rate decreased over time [ 110 , 111 ]. The variabilities in K release among the soils could be ascribed to the differences in types of clay minerals, contents of clay and silt, and climate conditions [ 115 ]. Besides [ 116 ], revealed that soil available K is primarily regulated by the rate of K released into forms suitable to be taken up by plants.…”
Section: Resultsmentioning
confidence: 99%