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  • Articles  (1,835)
  • Ovid Technologies  (609)
  • Blackwell Publishing Ltd  (582)
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  • Periodicals Archive Online (PAO)  (267)
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  • 2020-2024
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  • 1965-1969
  • 1960-1964  (1,396)
  • 1945-1949  (439)
  • 1963  (763)
  • 1960  (633)
  • 1948  (439)
  • Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition  (1,835)
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  • Articles  (1,835)
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  • 2020-2024
  • 2020-2022
  • 1965-1969
  • 1960-1964  (1,396)
  • 1945-1949  (439)
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  • 1
    Publication Date: 1963-07-01
    Description: A preliminary study of the mineralogical composition of the fine sand fractions of 51 samples of tills and stratified sands in northern Ontario was carried out. About 40 different minerals were identified in widely varying amounts. In all but a few samples, feldspar was the most abundant mineral while quartz was never the most abundant. Several deposits containing Palaeozoic limestone and dolomite fragments from the rocks of the James Bay lowlands were quite similar in composition to the calcareous southern Ontario deposits. Other samples, containing large amounts of pyroxenes, shale fragments or "greenstones", differed greatly from similar deposits in southern Ontario. The composition of the fine sand correlated well with the field classification of soils in this region, with a few exceptions.
    Print ISSN: 0008-4271
    Electronic ISSN: 1918-1841
    Topics: Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
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  • 2
    Publication Date: 1960-02-01
    Description: The formation of nitrate in eight grassland soils of the Kamloops, British Columbia, area was studied using a laboratory incubation technique. All the accumulative totals of nitrate nitrogen produced by these soils were low and suggest that the amount of nitrate formed may be inadequate for optimum plant growth. The desert-like soils, although they are regarded as being members of the Brown great soil group, released the most nitrate nitrogen. The Shallow and Degrading Black soils released nitrate in intermediate amounts while the Brown and Dark Brown soils produced the smallest quantities. The correlations between the accumulative total of nitrate released during incubation with: C/N ratio, total nitrogen and organic matter, were not highly significant. Poor correlation was obtained in the comparison between the accumulative total nitrate formed and the forage produced during the period 1954–1957.
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    Electronic ISSN: 1918-1841
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  • 3
    Publication Date: 1960-08-01
    Description: Soil productivity data included in this study were obtained from field experiments laid down in areas of soil, characteristic of individual member profiles of catenary groups of the Weyburn and Oxbow Associations, and of a mapping complex comprising members of the Sceptre, Kindersley, and Flaxcombe Associations.The criteria used to assess soil productivity included the yield of gram with and without phosphorus and nitrogen fertilization, uptake of fertilizer phosphorus, 'A' values (from field and greenhouse experiments) and extractable phosphorus (NaHCO3 and H2CO3).The data illustrate the variability in yield and response to phosphorus fertilization that can be expected within relatively short distances in any one field in which complexity of soil pattern occurs. These differences in productivity were closely associated with pedogenic differences used to classify the soils.It was concluded that considerable care must be taken in the interpretation and application of fertility data obtained from small plot experiments as the data are applicable to only one particular soil type, in most instances the soil member on which the test was established; such data cannot be used to represent mapping units which include even closely associated soil types.
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  • 4
    Publication Date: 1960-02-01
    Description: Twenty years' results showed that 37 per cent of the over-winter precipitation at Swift Current was conserved in stubble fields and 9 per cent in fallow. Further analysis showed that rainfall and snowfall were conserved equally well in stubble but that conservation in fallow was mostly from rainfall. Much of the snow was blown from the fallow and accumulated in the stubble.Fall moisture was also a factor, in that each inch of moisture stored in the soil in the fall reduced the over-winter conservation by approximately 0.2 inch.Nine years' results with fall cultivation on stubble showed that one-way disking after harvest reduced the winter storage in 3 years out of 9. Apparently any gain in moisture conservation from the removal of weed growth was more than offset by reduced snow accumulation during the winter. Blade tillage in the fall resulted in greater moisture storage at seed-time in 1 year out of 9.
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  • 5
    Publication Date: 1963-07-01
    Description: Three soils were used in greenhouse experiments to determine the effect of KCl and K2CO3 on the Sr90 concentration in oats, alfalfa, and timothy. In addition soils were moist incubated to determine the effects of similar potassium treatments on water soluble Sr90, calcium, and potassium.The general trend of results found in the greenhouse experiments was that increasing levels of added potassium caused decreases in calcium, magnesium, and Sr90 contents and increases in potassium contents of the crops. The decreases of Sr90 were frequently greater when potassium was applied as the carbonate compared with its addition as the chloride. There were some exceptions to these trends. For instance, Sr90 concentrations in oat grain increased with the addition of KCl to two of the soils. Increases in Sr90 content were also found for timothy grown in one of the soils when KCl was applied.The greater apparent effectiveness of K2CO3 in reducing Sr90 content of crops compared with the addition of the chloride is explained in part by the results of incubation experiments, where KCl caused increases in water soluble Sr90 whereas K2CO3 caused either smaller increases or decreases.
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    Electronic ISSN: 1918-1841
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  • 6
    Publication Date: 1963-01-01
    Description: Details are given of a procedure for the determination of carbon bonded sulphur in soils and soil extracts.Significant amounts of carbon bonded sulphur were found in a few selected Quebec soils. Organic soils contained substantially more carbon bonded sulphur than mineral soils, and also a higher proportion of the total sulphur was in a carbon bonded form in the organic (47–58 per cent) than in the mineral soils (12–35 per cent).The distribution of carbon bonded sulphur between acid-extractable, alkali-extractable and non-extractable fractions was determined on the same samples. The recovery of carbon bonded sulphur in these fractions was high in the organic soils, but 16–48 per cent was not accounted for in three mineral surface soils. For all samples, very little carbon bonded sulphur was non-extractable and, in all samples, except a podzol B21 horizon, more of this sulphur fraction was extracted by alkaline than by acid extraction.The importance of this fraction as a source of sulphur for plants cannot yet be assessed.
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  • 7
    Publication Date: 1960-08-01
    Description: Oats grown with different nutrient treatments in temperature-controlled soil in the greenhouse produced higher yields of grain and straw when soil temperature was increased from 41° to 67°F. Yields were usually less at 80°F. than at 41°F. This relationship between growth and soil temperature was also apparent at the heading stage. At 7th leaf, however, the best temperature for growth varied with nutrient treatment. Root yields usually decreased with increase in soil temperature.Increasing soil temperature from 41° to 67°F. increased uptake of N, P and K. In many instances increases in the concentration of N, P and K in the plant contributed to these increases in uptake. The effect of soil temperature on uptake was more consistent for P than for other elements.Nitrates and native phosphorus in incubated soil samples increased with increase in temperature from 41° to 80°F. but exchangeable K values were not affected.
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  • 8
    Publication Date: 1963-01-01
    Description: A study was made of the adsorption of monosilicic acid from dilute solutions by soils and other solids and the results were applied to a consideration of silica in natural soil solutions. Freshly precipitated hydroxides of polyvalent metal ions were most effective, some soil samples and iron-oxide minerals were moderately effective, and alkaline-earth carbonate minerals were ineffective in adsorbing dissolved silica. The adsorption data approximately conformed to Freundlich's adsorption equation. Adsorption of Si(OH)4 increased throughout the reaction range pH 4 to pH 9 and, with a ferruginous soil sample, adsorption decreased as the pH was increased above 10.The data obtained support the hypothesis that a pH-dependent adsorption reaction is involved in controlling the concentration of silica in soil solutions. Adsorption of Si(OH)4 as soil moisture evaporates may contribute to the accumulation of amorphous coatings on soil particle surfaces.
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  • 9
    Publication Date: 1963-01-01
    Description: A procedure for the removal of free iron from soils and clays by a single extraction at 50 °C. with sodium hydrosulphite in a citrate buffer at pH 4.75 is described. The effects of pH, temperature and reagent concentrations on the rate of removal of free iron from soils and hematite were investigated. The crystal structures of clay minerals other than nontronite were not attacked by this procedure. The single extraction removed as much or more iron than was removed by successive extractions in three procedures proposed by other workers.
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  • 10
    Publication Date: 1960-08-01
    Description: Top dressings of ammonium nitrate were made during the growing season to crops of barley and oats showing symptoms of acute nitrogen deficiency. The addition of nitrogen in the early stages of plant growth resulted in increased vegetative growth and increased yields. Applications of nitrogen delayed until the shot-blade stage had little effect on yield, but substantially increased the protein content. The yield of protein per acre was increased with higher rates of fertilization, regardless of whether the effect of the added nitrogen was to increase yield or protein content.
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