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  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Biology and fertility of soils 11 (1991), S. 83-87 
    ISSN: 1432-0789
    Keywords: Amoebae ; Protozoa ; Rhizosphere ; Nutrient cycling ; Biocontrol ; Microaggregates
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary An ultrastructural investigation of amoebae in situ in the rhizosphere showed that the protozoa are closely associated with soil aggregates and produce long pseudopodia that penetrate micropores. This could partly explain why bacteria are generally confined to the interiors of microaggregates. The presence of cytologically intact and partly digested bacteria in the food vacuoles indicates that rhizosphere bacteria are both ingested and digested by the amoebae. This digestion could lead to the recycling of P and N immobilized in rhizosphere microorganisms.
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Biology and fertility of soils 10 (1990), S. 121-126 
    ISSN: 1432-0789
    Keywords: Biodegradation ; Nutrient levels ; Mineralization ; Rhizosphere ; Microenvironment ; Root exudates ; Priming effect
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary The effect of one form of soil organic matter, such as living roots or root exudates on another form of soil organic matter, such as dead roots or incorporated litter and litter leachates, has been studied from various perspectives over the last 25 years. The effect seems to be either positive (priming) or negative (conserving). The present review concentrates on the conserving effect, measured as a decrease in 14CO2 released, in both field and greenhouse/growth chamber studies. The field experiments suggested that certain physical conditions in the soil, such as less available moisture or restricted aeration which led to lower microbial activity, explained the conserving effect of living roots on soil organic matter. Although more detailed greenhouse/growth chamber studies confirmed the conserving effect per se, it appears that biological rather than physical factors could better explain the reduction in the rate of decomposition of 14C-labelled plant residues in the presence of roots. However, a complex picture has emerged through a variety of postulates, all proposed in attempts to explain the conserving effect. Finally, the most recent studies have argued that the decrease in decomposition of labelled organic matter in planted soil is probably more apparent than real. A decrease in respired 14CO2 could be explained by an incorporation of 14C derived from old roots into the rhizosphere microbial populations of the living roots. To make any further progress on the fundamental question of how soil organic matter moves along its continuum from a living to a refractory state, the microenvironment needs to be examined at periodic intervals. New developments in improved histochemical and electron-probe microanalyses look promising.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Plant and soil 33 (1970), S. 729-732 
    ISSN: 1573-5036
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary 1. Acriflavine adsorption capacities of humic substances are not easy to interpret since factors such as acid pretreatment, strength of extractant, and time and temperature of extraction all affect the data. It is thus difficult to establish with this technique whether qualitative differences exist between organic matter formed under different plant associations. 2. Acriflavine sorption capacity of the acid-precipitable humus extracted may be a measure of the efficiency of humus carbon extraction as related to the organo-mineral complexes in the soil since it correlates negatively with the clay content of the samples. 3. Acriflavine adsorption values of the acid-precipitable humus of the aeolian soils are likely to represent true or total sorption capacities of this fraction in these soils, because the clay content of these soils is low and thus extraction of those sites responsible for the acriflavine sorption reaction will be more complete.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Plant and soil 28 (1968), S. 268-279 
    ISSN: 1573-5036
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary A satisfactory method for extracting all the organic phosphorus from a soil remains to be found. An analysis of the organic phosphorus present in the extract at each stage of the two methods commonly used for determining total organic phosphorus seems to indicate differences in the nature of the organic phosphorus extracted by the two methods. An alkaline extraction consisting of pretreatment with 0.1N HCl and extraction by 1N NaOH followed by acidification with H2SO4 to pH 1.0 was compared with a chelating resin extraction consisting of a 0.1N HCl-0.1N HF pretreatment and a 15-hour Dowex A-1(Na+) resin extraction followed by the removal of Na+ via a Dowex 50W-X4(H+) column. More of the organic phosphorus associated with the humic acids, about 41 and 22 per cent of the ‘total’ organic phosphorus, was extracted from the Ah and Bm horizons, respectively, by the resin method than by the alkaline method. The resin method of extraction was more effective on the Ah than on the Bm horizon samples. An entirely different approach seems to be required for organic phosphorus in Bm horizons of Chernozemic soils. The coefficients of determination for humic acid associated phosphorus obtained with 1N NaOH were 78 and 56 per cent of the ‘total’ organic phosphorus in samples from the Ah and Bm horizons, respectively; those obtained with the Dowex A-1(Na+) resin extraction were 93 and 70 per cent, respectively.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Plant and soil 33 (1970), S. 729-732 
    ISSN: 1573-5036
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary 1. Acriflavine adsorption capacities of humic substances are not easy to interpret since factors such as acid pretreatment, strength of extractant, and time and temperature of extraction all affect the data. It is thus difficult to establish with this technique whether qualitative differences exist between organic matter formed under different plant associations. 2. Acriflavine sorption capacity of the acid-precipitable humus extracted may be a measure of the efficiency of humus carbon extraction as related to the organo-mineral complexes in the soil since it correlates negatively with the clay content of the samples. 3. Acriflavine adsorption values of the acid-precipitable humus of the aeolian soils are likely to represent true or total sorption capacities of this fraction in these soils, because the clay content of these soils is low and thus extraction of those sites responsible for the acriflavine sorption reaction will be more complete.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Plant and soil 31 (1969), S. 182-184 
    ISSN: 1573-5036
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Plant and soil 41 (1974), S. 51-64 
    ISSN: 1573-5036
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary Humic substances extracted with chelating resin from a Dark Brown Chernozem (Typic Haploboroll) Ah, a Black Chernozem (Udic Haploboroll) Ah, and a Dark Gray Luvisol (Typic Cryoboralf) Ahe were fractionated by Bio-Gel P. The eluted material was combined to form three or four fractions for further characterization. Most of the extracted polydisperse humic substances of the three soils were eluted near V0 and distributed around a single mean value. The ash content of this material varied from 1.36 to 1.78 per cent. Carboxyl acidity may thus be obtained without interference from any cations. The humic substances from the Dark Brown and Black Chernozem Ah gave similar elution profiles, whereas those from the Dark Gray Luvisol Ahe were less aliphatic and more aromatic in nature. The materials of low molecular weight had the highest content of ash, C, and carboxyl groups. They represented only 3.6 to 14.1 per cent of the C extracted and were considered, on the basis of increased C content, decreased optical density, and infrared spectral configurations, to consist of polynuclear, fused-ring, aromatic structures.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Plant and soil 75 (1983), S. 51-61 
    ISSN: 1573-5036
    Keywords: Aggregate fractions ; Fatty acids ; Long-term rotation ; Triticum aestivum ; Water-stable aggregates
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary Three non-replicated, unfertilized, dryland grain rotations—continuous wheat, wheat-fallow, and wheat-wheat-fallow—were established in 1912 on a Dark Brown Chernozemic (Typic Haploboroll) soil. The effect of long-term cropping on the chemical constituents of total water-stable aggregates was assessed. There was a loss in percentage of total water-stable aggregates and a shift in aggregate size distribution with time. Together with an increase in the 100 μm diameter fraction, there was an increase in the sand component of this fraction. These sand particles are probably held together by alkaline-soluble, acid-insoluble organic matter. Organic carbon, polysaccharides, polyuronides, phenols, and chloroform/methanol-extractable organic matter were all associated with the 〉250 μm diameter fractions. Although the aggregates had generally the same suite of aliphatic carboxylic acids, the relative proportions changed with cultivation.
    Type of Medium: Electronic Resource
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  • 9
    Publication Date: 1969-01-01
    Print ISSN: 0361-5995
    Electronic ISSN: 1435-0661
    Topics: Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Published by Wiley
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  • 10
    Publication Date: 1964-02-01
    Description: One mineral soil with known amounts of organically bound phosphorus added to it, two organic soils, and five known phosphate esters were ignited at various temperatures to study losses of phosphorus as a result of ignition.Incomplete recoveries of phosphorus were obtained from the mineral soil. For the organic soils incomplete combustion occurred at temperatures below 650 °C and volatilization at temperatures higher than 400 °C. Either complex formation or resistance to oxidation occurred in the case of RNA, phytin, and lecithin.
    Print ISSN: 0008-4271
    Electronic ISSN: 1918-1841
    Topics: Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
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