Effect of pH on the content of K, Al, Fe, Si, Ca, and Mg in soil solution
1987
Stawinski, J. | Wierzchos, J. | Jozefaciuk, G. (Polish Academy of Sciences, Lublin (Poland). Inst. of Agrophysics) | Rodriguez, P.C. (Instituto of Soil Science and Plant Biology, Madrid (Spain))
Four soils differing with respect to typology, kind and genus were used. The relationships between the concentrations of Al, Fe, Si, and K and pH have a parabolic character for the soils studied. The minima of these relationships for Al and Fe do not depend on the kind of soil and occur in narrow pH intervals: 4.2-5.1 and 4.2-5.6, respectively
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书目信息
Polish Journal of Soil Science (Poland)
卷
20
期
1
ISSN
0079-2985
页码
pp. 33-39
其它主题
Solution du sol/ fertilite du sol; Soluciones del suelo/ fertilidad del suelo
语言
英语
注释
6 ref. Summaries (En, Pl)
类型
Summary
1991-08-15
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