Zinc in Soils and Plants 1993
DOI: 10.1007/978-94-011-0878-2_11
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The Distribution and Correction of Zinc Deficiency

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Cited by 121 publications
(45 citation statements)
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“…This partitioning of Zn is influenced by soil pH, clay content, organic matter and sesquioxides. Arid and semi-arid region soils that are low or high in pH, low or high in organic matter content, sandy, calcareous, or water-logged are commonly deficient in Zn (Takkar and Walker, 1993). In order to supply Zn to crops grown on these soils, the method of application for effective availability and absorption by plants can be a critical concern.…”
Section: Introductionmentioning
confidence: 99%
“…This partitioning of Zn is influenced by soil pH, clay content, organic matter and sesquioxides. Arid and semi-arid region soils that are low or high in pH, low or high in organic matter content, sandy, calcareous, or water-logged are commonly deficient in Zn (Takkar and Walker, 1993). In order to supply Zn to crops grown on these soils, the method of application for effective availability and absorption by plants can be a critical concern.…”
Section: Introductionmentioning
confidence: 99%
“…Zn deficiency is common in wheat-growing areas of the world, particularly in calcareous soils (Welch et al 1991;Takkar and Walker 1993;White and Zasoski 1999).…”
Section: Introductionmentioning
confidence: 99%
“…Generally, Zn concentration range of noncontaminated soils varies from 10 to 300 mg kg -1 soil (Ohnesorge & Wilhelm, 1991). In highly weathered soils, Zn natural reserve is very low and its deficiency has imposed several limitations on the absolute development of economically important crops in the intertropical zone (Takkar & Walker, 1993). In plants, Zn acts as a catalyzing component of more than 300 enzymes, and it is necessary for triptophane, a precursor amino acid of indoleacetic acid (IAA), a growth promoting plant hormone (Mengel & Kirkby, 2001).…”
Section: Introductionmentioning
confidence: 99%