1964
DOI: 10.1080/03650346409414111
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Die Molybdänversorgung der Thüringer Böden und der Einfluß einer Molybdändüngung auf Ertrag, Rohprotein- und Mineralstoffgehalt von Luzerne

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Cited by 3 publications
(2 citation statements)
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“…To account for pH dependence of anion availability, it is suggested to calculate an availability parameter that considers both ion concentrations and pH values (Saarela and Sippola 1990). Müller et al (1964) established the so-called Mo soil number (= pH + 0.01 × Mo ox (ng·g -1 )) to predict availability of Mo in arable soils. This index, however, was not suitable for the calculation of needle contents at the forest sites, neither based on pH(H 2 O) nor on pH(CaCl 2 ).…”
Section: Molybdenum In Needlesmentioning
confidence: 99%
“…To account for pH dependence of anion availability, it is suggested to calculate an availability parameter that considers both ion concentrations and pH values (Saarela and Sippola 1990). Müller et al (1964) established the so-called Mo soil number (= pH + 0.01 × Mo ox (ng·g -1 )) to predict availability of Mo in arable soils. This index, however, was not suitable for the calculation of needle contents at the forest sites, neither based on pH(H 2 O) nor on pH(CaCl 2 ).…”
Section: Molybdenum In Needlesmentioning
confidence: 99%
“…These contents were evaluated as a function of the pH value and the geological origin of the soil. Reisenauer (1956), Trobisch (1962), Müller et al (1964), and Schnorr and Bergmann (1968) proved that there is a well-established negative correlation between pH value and "available" molybdenum content in the soil of several geological origins (Michael and Trobisch 1961, Podlesak 1983, Grün et al 1989.…”
Section: Floramentioning
confidence: 99%