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  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Plant and soil 33 (1970), S. 497-500 
    ISSN: 1573-5036
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary An incubation experiment was conducted on 3 soils with 3 levels of lime-stone and 2 levels of Mo in the laboratory. There was no change in the amount of exchangeable Mo in Culloden and O'Leary soils as affected by the various pH levels after different incubation periods. On Acadia soil, the amount of exchangeable Mo increased after 4 weeks; however, the lime levels had no effect. There was an increase in extractable Mo in response to added Mo.
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  • 2
    ISSN: 1573-5036
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary Aluminum toxicity resulted in abnormal root development with many short thick roots and was found at pH 4.3 with or without added Al. The toxicity of Mn was found with no added Mn, and with 50 and 100 ppm added Mn at pH values ranging from 4.0 to 4.7 and appeared as dark spots on the leaves. At pH values ranging from 5.8 to 6.0, no toxicity symptoms were recorded in the absence of added Mn. Al was more detrimental to seedling development than was Mn. No kernels developed at 25 and 50 ppm added Al at pH≤4.1. Such toxicity was associated with Al contents of 9.6 to 28.5 μg/ml of saturated extract of soil. The highest kernel yields were recorded at pH 5.8 to 6.0 and were associated with 116 to 296 ppm Mn in tissue and of less than 0.1 μg/ml of Al in the saturated extract. Increased rates of Mn and Al resulted in increased concentrations of Ca, Mg, and K in the saturated extract of soil. The results indicated that Al toxicity can be eliminated by liming to soil pH values of greater than 5.5; however, Mn toxicity may occur at pH values as high as 5.8 in the presence of large quantities of Mn.
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Plant and soil 47 (1977), S. 283-287 
    ISSN: 1573-5036
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary Rates of added B up to 1.8 kg/ha had no effect on grain yield, but at rates of 2.24 kg/ha and higher it decreased yield of both barley and wheat. Lime-stone applications up to 4000 kg/ha did not induce B deficiency at low levels of B or alleviate B toxicity at high B levels in the two crops. Liming increased barley yields where soil pH was less than 5.8 but gave no yield response when soil pH exceeded 5.8. In general, liming did not decrease the B concentration of boot stage tissue (b.s.t.) except in barley at 1.8 kg B/ha on Location 1, where liming to pH 6.3 and 6.6 decreased B in b.s.t. from 16.4 to 12.2 and 11.4 ppm. The applications of B generally increased the N concentration of wheat grain where yields decreased due to B toxicity.
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  • 4
    ISSN: 1573-5036
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary Five rates of limestone and 4 rates of fertilizers were used in a split-plot design to study their effects under field conditions on Mo, Cu, B, Mn, and Zn levels in mixed forage tissue and soil, and on the forage yield. An increase in soil pH resulted in an increase in Mo and Cu content of plant tissue while B, Mn, and Zn decreased. The micro-nutrient content of the tissue increased as the harvesting season progressed. Increasing rates of applied fertilizer did not affect the micro-nutrient content of the forage tissue or soil. Liming to a pH of 5.6 and above reduced the availability of Mn and Zn in the soil. In general, the available B was low at pH values greater than 6.1. Lime did not affect the quantities of Mo and Cu in the soil. Manganese is supplied in large quantities by limestone and is not apt to be deficient in limed soil. However, addition of B and Zn may be required on the high pH soils of Eastern Canada in future. Molybdenum was adequate where the soil was limed to a pH of 6.1 or greater. The dry-matter yield of forage increased significantly with successive increases in lime up to pH 6.6 and with each increment of fertilization.
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  • 5
    ISSN: 1573-5036
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary In two greenhouse experiments, sphagnum peat, adjusted to various pH levels, was used to study the effect of various levels of Fe on the growth of carrots (Daucus carota L., var. sativa D.C.). The Fe was added to the medium as sequesterine 330 chelate. Maximum carrot root and top tissue yields were obtained at soil pH 6.6 and 7.1. At soil pH 5.2 and 7.8 the yields were in the intermediate range. The yields were low at pH 4.3, 4.5 and 8.1 and at pH 8.4 the carrots did not grow. The chlorotic symptoms on carrot leaves, accom-panied by reduced yields, were associated with 39 to 82 ppm Fe and 〉 332 ppm Mn in the leaf and were likely due to Mn toxicity. Toxic levels of Mn in tissue were found even at soil pH 8.1 and were associated with reduced carrot yields. The leaf tissue concentrations of Fe and Mn decreased as the pH of soil increased; however, at pH 5.2, 7.8, and 8.1 the tissue Mn concentration increased. The added Fe had no effect on the Fe concentration but decreased the Mn and Zn concentration of leaf tissue and increased carrot root yields. There was a significant interaction between added lime and Fe, whereby the decrease in leaf tissue Mn concentration and increases in root yields with added Fe were much greater at pH 4.5 and 5.2 than at pH values of 6.6 and 7.8. The S concentration in the leaf tissue decreased with added Fe and lime. The leaf tissue Zn concentrations of 184 to 490 ppm and S concentrations of 0.32 to 0.63%, as found here, are considered to be high but not in the toxic range.
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Plant and soil 26 (1967), S. 202-204 
    ISSN: 1573-5036
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Plant and soil 28 (1968), S. 298-305 
    ISSN: 1573-5036
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary A method of determining Fe from plant materials using O-phenanthroline is described. The absorbance of the Fe(C12H8N2) 3 ++ complex from pure iron solutions or from extracts of different plant materials did not vary over a pH range of 2 to 5. Maximum absorbance was obtained after a period of 2 hours of color development and was constant for at least 24 hours. The standard curves prepared by a procedure described elsewhere6 were quite similar to the ones obtained by the method described in this paper. A comparison of 3 methods of extracting Fe from the ash indicated that HCl + H2O2 gave higher results than either of the other methods. The Fe content obtained by this procedure was very similar to the values obtained by AAS. A high percentage of the Fe added to plant tissues and peats was recovered when extracted by HCl + H2O2 and that the reproducibility was good. This is recommended as a simple and satisfactory procedure for accurate determination of Fe.
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  • 8
    ISSN: 1573-5036
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary Five rates of limestone and 4 rates of fertilizers were used in a split-plot design to study their effects under field conditions on Mo, Cu, B, Mn, and Zn levels in mixed forage tissue and soil, and on the forage yield. An increase in soil pH resulted in an increase in Mo and Cu content of plant tissue while B, Mn, and Zn decreased. The micro-nutrient content of the tissue increased as the harvesting season progressed. Increasing rates of applied fertilizer did not affect the micro-nutrient content of the forage tissue or soil. Liming to a pH of 5.6 and above reduced the availability of Mn and Zn in the soil. In general, the available B was low at pH values greater than 6.1. Lime did not affect the quantities of Mo and Cu in the soil. Manganese is supplied in large quantities by limestone and is not apt to be deficient in limed soil. However, addition of B and Zn may be required on the high pH soils of Eastern Canada in future. Molybdenum was adequate where the soil was limed to a pH of 6.1 or greater. The dry-matter yield of forage increased significantly with successive increases in lime up to pH 6.6 and with each increment of fertilization.
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Plant and soil 34 (1971), S. 249-253 
    ISSN: 1573-5036
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary In most cases, the lowest percentage recoveries of added Mo and Cu were obtained after 0 weeks. The highest recoveries of Mo were found after 12 weeks except in the case of peat, where it was after 8 weeks; and of Cu after 4 to 12 weeks of incubation. The exch. Mo content of soil was lower when organic materials and Mo were added than from soil where only Mo was added. However, in the absence of added Mo, the exch. Mo content was higher in soils where O.M. was added. Addition of peat resulted in lowest quantities of exch. Mo. Exch. Cu was higher in the presence of added organic materials, with or without the addition of Cu, when compared with soils without added O.M. The largest quantities of exch. Cu were obtained where F.Y.M. was used as a source of O.M., with or without added Cu.
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  • 10
    Electronic Resource
    Electronic Resource
    Springer
    Plant and soil 33 (1970), S. 497-500 
    ISSN: 1573-5036
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary An incubation experiment was conducted on 3 soils with 3 levels of lime-stone and 2 levels of Mo in the laboratory. There was no change in the amount of exchangeable Mo in Culloden and O'Leary soils as affected by the various pH levels after different incubation periods. On Acadia soil, the amount of exchangeable Mo increased after 4 weeks; however, the lime levels had no effect. There was an increase in extractable Mo in response to added Mo.
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