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  • Nitrogen  (30)
  • Springer  (30)
  • Blackwell Publishing Ltd
  • 1995-1999
  • 1980-1984  (30)
  • 1945-1949
  • 1925-1929
  • 1984  (30)
Collection
Publisher
  • Springer  (30)
  • Blackwell Publishing Ltd
Years
  • 1995-1999
  • 1980-1984  (30)
  • 1945-1949
  • 1925-1929
Year
  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Nutrient cycling in agroecosystems 5 (1984), S. 355-369 
    ISSN: 1573-0867
    Keywords: Nitrogen ; fertilizer ; dynamic model ; sugar beet
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract A concise model is described for calculating day-to-day increments in nitrogen uptake and dry matter of crops grown with different levels of N-fertilizer. Inputs are the initial distribution of inorganic-N down the profile, the maximum yield, the maximum depth of rooting, and the mineralization rate. The validity of the model was tested against measurements of the %N and total dry weights of storage roots and foliage in nine N-fertilizer trials with sugar beet, six of which included both irrigated and unirrigated treatments. Agreement between the model and experiment was good except in one experiment severely attacked by virus yellows. Simulation studies with the model indicated that no simple correlation would be expected between N fertilizer requirement and any single indicator of N availability for crops grown under a wide range of conditions in the UK.
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  • 2
    ISSN: 1432-1009
    Keywords: Watersheds ; Budgets ; Nitrogen ; Phosphorus ; Channelization ; Swamps ; Floodplain
    Source: Springer Online Journal Archives 1860-2000
    Topics: Energy, Environment Protection, Nuclear Power Engineering
    Notes: Abstract Nitrogen and phosphorus exports from channelizedstream watersheds were elevated over those from nearby natural swamp-stream watersheds. Nitrate exports were significantly greater from channelized-stream watersheds, and higher exports were attributed to faster groundwater drawdown, continual streamflow, and transformation of former floodplain to croplands following channelization. Exports of total organic nitrogen and total nitrogen were also significantly greater from channelized-stream watersheds. Differences in the exports of ammonium, filterable reactive phosphorus, and filterable unreactive phosphorus between the two watershed types were not detectable. Particulate phosphorus exports were significantly higher from channelized-stream watersheds, presumably because of greater erosion potential of nearby croplands and steep channel banks in the altered watersheds. The presence of nonpoint sources of pollution increased watershed exports of nutrients regardless of stream morphology. Examination of nutrient budgets for a portion of swamp floodplain at the base of one natural-stream watershed revealed that changes in local groundwater hydrology and stream morphology associated with channelization appeared to have greater effect on nutrient exports than simply the loss of bordering forested floodplain.
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  • 3
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    Archives of microbiology 140 (1984), S. 101-106 
    ISSN: 1432-072X
    Keywords: 5-aminolevulinic acid ; Ammonia ; botryococcus braunii ; Botryococcenes ; Carbon ; Hydrocarbon ; Metabolism ; Nitrogen ; Resting state ; Terpenoids
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Carbon metabolism in photosynthesizing and respiring cells of Botryococcus braunii was radically changed by the presence of 1 mM NH4Cl in the medium, when the so-called “resting state” previously had been subjected to a nitrogen-deficient medium. Ammonia addition to the algae photosynthesizing with 14C-labelled HCO 3 - almost completely inhibited the synthesis of 14C-labelled botryococcenes and other hexane-extractable compounds, and also inhibited the formation of insoluble compounds; however, it resulted in a large increase in the synthesis of alanine, glutamine, other amino acids, and especially of 5-aminolevulinic acid. Total CO2 fixation decreased about 60% and O2 evolution decreased more than 50%. CO2 fixation in the dark with ammonia present led to labelled products derived from phosphoenolpyruvate carboxylation, such as glutamine, glutamate, and malate. Respiratory uptake of O2 increased by about 70%. The inhibition of terpenoid synthesis and increased synthesis of C5 amino acids by Botryococcus upon ammonia addition indicates 1) a diversion of acetyl coenzyme A from synthetic pathways leading to terpenoids and 2) increased operation of pathways leading to the synthesis of amino acids, especially 5-aminolevulinic acid, a precursor to chlorophyll biosynthesis.
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  • 4
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    Theoretical and applied genetics 67 (1984), S. 97-111 
    ISSN: 1432-2242
    Keywords: Genetics ; Nitrogen ; Grain crops ; Selection ; Plant breeding
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Summary It is necessary to increase protein productivity of grain crops to meet present and future world protein requirements. Conventional plant breeding methodology has been to select genotypes with enhanced yield or grain protein concentration. In addition to this determination of end product, we suggest measurements of a number of physiological and biochemical processes of nitrogen (N) metabolism which precede plant maturity as selection criteria for enhanced N metabolism and grain crop productivity. The measurement across the growing season of genotypic variation in components of N metabolism would constitute a physiological/biochemical selection program to be incorporated with the determination of harvestable end product. A properly designed physiological/biochemical selection program would integrate the effects of plant genotype, environment, and their interactions allowing identification of the factors limiting productivity of particular genotypes, and would also estimate end product. Our review of literature pertinent to whole plant N metabolism suggests that such a selection program initially include NO 3 - uptake, N2 fixation, N accumulation, N remobilization, seed protein synthesis, and Nitrogen Harvest Index.
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  • 5
    ISSN: 1573-5036
    Keywords: Ammonium ; Barley ; Fertilizer ; Mineralization ; Nitrate ; Nitrogen ; Nitrogen-15
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary Field experiments were carried out using15N-labelled calcium nitrate, to investigate the relative uptake by barley of fertilizer-N and soil-N. On imperfectly drained till soils uptake of soil-N increased with increasing rate of fertilizer, but remained constant on a brown sand, possibly due to more efficient root exploration in the latter soil. In four out of five seasons, late uptake of soil-derived N was a major feature, and uptake from ploughed soil as compared with uptake from direct-drilled soil was correlated with seasonal rainfall patterns. Significantly higher quantities of both fertilizer- and soil-derived N were taken up by winter barley than by spring barley, reflecting the longer growth period and higher dry matter yield from the former crop.
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  • 6
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    Plant and soil 76 (1984), S. 127-137 
    ISSN: 1573-5036
    Keywords: Adenylate pool ; Biomass volume ; CO2 evolution ; Chitin ; DNA ; Electron microscopy ; Enzymes ; Fluorescent antibody ; Fumigation-respiration ; Fungi Histochemistry ; Imunofluorecence ; Jones-Mollison technique ; Microcosms ; Monoclonal antibodies ; Nitrogen ; Nutrients ; Oxygen consumption ; Phosphorus ; Phytotoxins ; Plate counts ; Rhizobium ; Rhizosphere ; Sulphur ; Xenobiotics
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary There is an immense literature on biological and biochemical analyses of soils. Such analyses have revealed the enormous richness of species in soil and their vast range of metabolic potentials and ecological diversity. Accordingly, the approaches used to investigate the soil biota and its biochemistry usually have to be modified or adapted depending upon the purpose of the investigation. Studies of micro-organisms in the soil environment, are complicated because microbial cells are commonly attached to surfaces where they live side-by-side with other populations in consortia usually containing different morphological and physiological types. Such assemblages of organisms cannot be described quantitatively using cultural techniques, such as plate counts, which underestimate both cell numbers and viable biomass. The development of more powerful observational and staining techniques has improved our knowledge of the diverse morphological and biochemical composition of soil micro-communities. Such findings have been amplified at a grosser level by laboratory studies with multi-component systems (microcosms) to mimic field situations and to assess the range of biochemical potentials of microbial consortia. But despite notable advances in analytical methods we are still, with a few exceptions, unable to detect or identify those microorganisms which carry out specific biochemical transformations or determine whether particular cells are alive, dormant or dead at the time of observation. Considerable work has been done to define some of the fundamental ecological attributes of microbial assemblages in soil. Productive work on the metabolic activities of the soil microbiota, specially geochemical transformations of C, N, S and P, has been under way for more than a century. But only in more recent years have more sensitive and reproducible analytical methods become available to measure viable biomass in soil. This will enable some insight to be gained into the role that microbial biomass plays as a labile source and sink for plant nutrients.
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  • 7
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    Plant and soil 76 (1984), S. 213-226 
    ISSN: 1573-5036
    Keywords: Acetylene ; Arable crops ; Cultivation ; Denitrification ; Drainage ; Gas ; Chromatography ; Grassland ; Inorganic N fertilizer ; Irrigation ; Nitrogen ; Nitrous oxide
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary Recent denitrification research is reviewed to answer questions a) how much N is lost from the soil as N2 and N2O and b) how do agronomic practices affect this loss? The methods used to quantify denitrification are also discussed. Gaseous losses of inorganic N range between the equivalent of 0 to 20 per cent of the fertilizer N applied to arable soils and 0–7 per cent on grassland soils. Losses are greater on undrained land and also after using direct drilling to establish arable crops. Appendix 1 summarizes reported measurements of gaseous N losses.
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  • 8
    ISSN: 1573-5036
    Keywords: Carbon ; Concepts ; Cultivation effects ; Nitrogen ; Nitrogen-15 ; Organic matter models ; Particle size fractions ; Phosphorus
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary Changes in the composition of organo-mineral particle size fractions as a result of cultivation of a grassland soil are discussed with reference to models of soil organic matter formation and turnover. The data presented indicated that physically stabilized organic matter is an important reservoir, with an intermediate turnover time, which is responsible for nutrient supply in agricultural soils. Possible mechanisms of stabilization and mobilization of organic matter are presented in the light of the arrangement of organic and inorganic components of the soil.
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  • 9
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    Plant and soil 79 (1984), S. 343-351 
    ISSN: 1573-5036
    Keywords: Alnus rubra ; Aluminum ; Annual returns ; Essential elements ; Litterfall ; Leaf litter ; Nitrogen ; Nutrients ; Red alder
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary Litterfall was collected over 1 year from eight natural stands of red alder growing on different sites in western Washington. The stands occurred at various elevations and on different soils, and differed in age, basal area, and site index. Most litterfall was leaf litter (average 86 percent). Amounts of litterfall and leaf litter varied significantly (P〈0.05) among the sites. Average weights of litterfall and leaf litter in kg ha−1 yr−1, were 5150 and 4440, respectively. Weight of leaf litter was not significantly (P〈0.05) related to site index, stand age, or basal area. The sites varied significantly (P〈0.05) in concentrations of all elements determined in the leaf litter, except Zn. Average chemical concentrations were: N, 1.98 percent; P, 0.09 percent; K, 0.44 percent; Ca, 1.01 percent; Mg, 0.21 percent; S, 0.17 percent; SO4−S, nil; Fe, 324 ppm; Mn, 311 ppm; Zn, 53 ppm; Cu, 13 ppm; and Al, 281 ppm. There were significant correlations between some stand characteristics and concentrations of some elements, and among the different chemical components of the leaf litter. Important correlations were found between stand age and P concentration (r=−0.84,P〈0.01); weight of leaf litter and P concentration (r=0.74,P〈0.05); weight of leaf litter and K concentration (r=0.71,P〈0.05); concentrations of N and S (r=0.81,P〈0.05); and concentrations of Fe and Al (r=0.98,P〈0.01). Returns of the different elements to the soil by leaf litter varied among the different sites. Average nutrient and Al returns, in kg ha−1 yr−1, were: N, 82; Ca, 41; K, 19; Mg, 8; S, 7; P, 4; Fe, 1; Mn, 1; Al, 1; Zn, 0.2, and Cu, 〈0.1.
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  • 10
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    Plant and soil 76 (1984), S. 3-21 
    ISSN: 1573-5036
    Keywords: Agriculture ; Barley ; Budgets ; Fauna ; Fertilizers ; Global cycles ; Lucerne ; Meadow fescue ; Microorganisms ; Nitrogen
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary Agro-ecosystems have developed from mixed- and multiple-cropping systems with relatively closed N cycles to intensively managed monocultures with large N inputs in the form of commercial fertilizers. Cultivation of increasingly larger areas of land has resulted in substantial losses of soil organic matter and N. Also, the move from slash and burn agriculture to intensively ploughed systems has resulted in losses through increased erosion. The use of N fertilizers has increased rapidly toca. 60 Tg N yr−1 (1980/81), which is equivalent to at least 40% of the N fixed biologically in all terrestrial systems and 36% more than is fixed in all croplands. On a global scale, the major losses of N from agro-ecosystems are estimated to be: harvest, 30 Tg; leaching, 2 Tg; erosion, 2–20 Tg; denitrification 1–44 Tg; and ammonia volatilization, 13–23 Tg. However, the data base is very crude and several estimates may be wrong by as much as one order of magnitude. Additions of N fertilizers have both direct and indirect effects on soil microorganisms. The possible importance of such effects is briefly discussed and a specific example is given on long-term effects on soil microbial biomass and nitrification rates in 27-year-old cropping systems with different N additions: (i) 0 kg N ha−1 yr−1, (ii) 80 kg N ha−1 yr−1, (iii) farmyard manureca. 80 kg N ha−1 yr−1. Few detailed N budgets exist for agro-ecosystems, despite its major importance as a limiting plant nutrient and the large losses of N from such systems. In conclusion, preliminary nitrogen budgets for four cropping systems (barley receiving 0 or 120 kg N ha−1 yr−1; meadow fescue ley with 200 kg N ha−1 yr−1 and a lucerne ley) are presented, with special attention to N flow through the soil organisms.
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  • 11
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    Plant and soil 76 (1984), S. 67-73 
    ISSN: 1573-5036
    Keywords: Maize ; Nitrogen ; Nitrogen uptake ; Tillage ; Zea mays L
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary Nitrogen (N) accumulation data from a replicated field study were fitted to a tanh (time) function and the derivate obtained to determine relative maximum rates of accumulation by maize. Both positive and negative effects of tillage on N accumulation rates were observed. Most of the N accumulation occurred over a 30-day period and time of N accumulation was not affected by tillage. Tilled profiles tend to contain greater NO3−N, greater aeration, and lower moisture contents than untilled profiles, and these characteristics interact to affect plant N accumulation.
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  • 12
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    Plant and soil 77 (1984), S. 73-86 
    ISSN: 1573-5036
    Keywords: Fertiliser ; Foliar analysis ; Nitrogen ; Phosphorus ; Pinus radiata ; Potassium ; Soil organic matter ; Steenbjerg effect
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary Copper deficiency inPinus radiata in Gippsland, Victoria was found to be associated with acid, organic-rich sandy podzols. A trial designed to find a Cu supplement for P and NPK fertilisation on these soils showed significant growth in stem-length following Cu-solution treatment in the nursery, and Cu fertiliser applied in the field up to at least 13.5 kg Cu ha−1. The Steenbjerg effect was evident in foliar concentrations of nutrients following fertilisation; this makes diagnosis from foliar analysis difficult. Foliar Cu∶N ratios proved a more sensitive indicator of Cu fertiliser treatment than either Cu or N alone. Two phases of seasonal drainage and podzol development were identified in the experiment. Trees growing on the better-drained, more acid soil with a high content of organic matter responded better to Cu fertiliser.
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  • 13
    ISSN: 1573-5036
    Keywords: Dehydrogenase ; Electron transport system ; Nitrogen ; Oxygen pH ; Substrate ; Temperature
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary Dehydrogenase activity was measured in a sandy loam soil under a variety of incubation conditions using the reduction of 2-(p-iodophenyl-3-(p-nitrophenyl)-5-phenyl tetrazolium chloride (INT) to iodonitrotetrazolium formazan (INT-formazan). There was a high positive correlation between dehydrogenase activity and substrate concentration, incubation temperature, and soil pH. Dehydrogenase activity also displayed a high negative correlation with O2 concentrations. Ammonium sulfate at concentrations from 40 to 120 μg/g soil had no significant effect on dehydrogenase activity. However, at concentrations of 160 and 200 μg/g, dehydrogenase activity was significantly reduced. Potassium nitrate at concentrations ranging from 40 to 200 μg/g had no significant effect on soil dehydrogenase activity, whereas sodium nitrite significantly inhibited activity at concentrations of 120 and 160 μg/g soil.
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  • 14
    ISSN: 1573-5036
    Keywords: Ammonium sulfate ; Nitrification ; Nitrogen ; Slow-release fertilizers ; Sulfur-coated urea
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary We have compared sulfur-coated urea granules (SCU) with ammonium sulfate granules (AS) in regard to nitrogen (N) release, diffusion, nitrification and the effect of irrigation. In the experiments plastic containers were filled with six layers of soil, separated from each other by fine nylon cloths. The fertilizer granules were placed between the two central layers, and irrigation was simulated by application of tap water to the uppermost layer. Nitrogen release from the SCU was slow, and after three months, 29.5% of the applied N remained in the granules. At the end of the experiment there was a deficit of 37.1% N in the case of the AS granules, while there was virtually none with the SCU. Throughout the experiment, N from SCU remained at a relatively even level, while 95% of the N applied as AS had disappeared after irrigation. Nitrification was rapid in both cases.
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  • 15
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    Plant and soil 76 (1984), S. 165-173 
    ISSN: 1573-5036
    Keywords: Biomass ; Carbon ; Chloroform fumigation ; Drying ; Mineralization flush ; Nitrogen ; Paddy soil
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary Soil samples of paddy fields with different fertilizer managements in Yamaguchi Agricultural Experiment Station, Japan were used to investigate the contribution of microbial biomass to the pool of mobile plant nutrients in paddy soil. The quantities of nutrients mobilized in soils which had been fumigated or dried were closely related to the quantities available in freshly killed biomass. A “KN-factor” (28 days) of 0.24 for the proportion of total N mineralized from dead biomass in paddy soils was obtained. It was observed that the C to N ratio mineralized from freshly killed biomass by chloroform fumigation of paddy soils was nearly 10 under aerobic conditions. For an approximate calculation of biomass C from the flush-N by chloroform fumigation of paddy soils, the equations of (B=33 Fn, 10 days) and (B=26 Fn, 28 days) were indicated. In oven-dried (70°C, 24 h) and rewetted soils, about 66% of N was mineralized from the freshly killed biomass during 28 days of incubation and the remaining 34% was derived from non-biomass organic matter of paddy soils.
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  • 16
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    Plant and soil 76 (1984), S. 233-241 
    ISSN: 1573-5036
    Keywords: Chemo-denitrification ; Iron oxyhydroxide ; Nitrate ; Nitric oxide ; Nitrite ; Nitrogen ; Nitrogen dioxide ; Reduced conditions ; Soil
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary Nitrite is very important in N transformation processes because it is an intermediate product in the aerobic nitrification as well as in the anaerobic denitrification process. Under soil conditions whereby aerobic and anaerobic zones are close to each other, the mobile nitrite can be a link between both N transformation processes. Because of its low stability in acid conditions, nitrite can be a key compound in N loss processes. The results are presented in three sets of incubation experiments using soil+added nitrite before and after oxidation of organic matter; soil+added nitrite and various iron oxide minerals; nitrite solutions without soil but with added ferrous iron. It was found that under acid conditions, soil organic matter as well as the soil mineral phase have a stimulating effect on the nitrite decomposition. Conditions favouring the solubility of Fe(III)-compounds and promoting the formation of Fe2+ increase the nitrite decomposition, even under slightly acid conditions. Of the gaseous decomposition products, only trace amounts of NO2 occur while NO is the major component. Conditions whereby NO and NO2 cannot escape from the medium promote production of some nitrite.
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  • 17
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    Plant and soil 76 (1984), S. 257-274 
    ISSN: 1573-5036
    Keywords: Biomass turnover ; Carbon ; Experimental verification ; Models ; Nitrogen
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary Many mathematical descriptions of C and N transformations in soils have been developed in the last decade, but only a few explicitly model the activity and mass of soil organisms. Great difficulties still exist in establishing basic parameters governing the kinetics of microbial turnover. The present state of the art is discussed briefly. The model of Van Veen and Frissel on C transformations and related mineralization and immobilization of N has been developed further based on laboratory and field data obtained with different Australian soils. Firstly, case studies show the large effects of the frequency of drying and rewetting of soils on the decomposition of organic matter and on the turnover of biomass. Secondly, the more refined model embraces the concept that soils have characteristic capacities to preserve both organic matter and microorganisms. Preservation of microorganisms could result from protection against predation and/or from amelioration of harsh environmental conditions. Biomass formed in excess of a soil's preservation capacity is assumed to die at a relatively high rate. Furthermore, biomass and its immediate organic products of decay are considered to form mainly a closed system from which only small proportions of the products leak out as stabilized materials. These concepts have been tested with data from laboratory experiments in which14C- and15N- labelled substrates and bacteria were added to a clay and sandy soil. Net mineralization of C and N (labelled and unlabelled) and changes in the total and labelled biomass as determined by the chloroform fumigation technique allowed for a thorough testing of these concepts in the manner in which they were included in the model. The fits between experimental observations and model outputs were very close. The model indicated that the contrasting metabolism of both C and N in a clayversus a sandy soil could largely be explained by differences in the capacities of the two soils to preserve microorganisms. The ability of a simulation model to describe accurately not only short-term events,e.g. N cycling during one growing season, but also the same processes over, say a decade, is an important criterion in assessing its predictive power. In this paper some of the results will be discussed of testing the model, developed from a consideration of the aforementioned laboratory studies, for its accuracy in describing the decomposition of plant residues in an 8-year field experiment.
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  • 18
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    Plant and soil 76 (1984), S. 139-148 
    ISSN: 1573-5036
    Keywords: Chloroform-fumigation ; Microbial biomass ; Mor humus ; Nitrogen ; Peat ; Phosphorus
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary Samples of peat and mor humus were treated with CHCl3 to kill microbial cells and the amounts of C as CO2, N as soluble- and mineral-N, and P as inorganic-P released by the treatment were compared with estimates of the microbial biomass by the Anderson and Domsch test and ATP determination. Increased amounts of soluble-N and inorganic-P, extracted with 1M KCl and 0.01M CaCl2 respectively, were detected immediately after the fumigation treatment. However, the subsequent rates of production of CO2−C and mineral-N measured during a 10-day incubation period at 25°C were low and variable, resulting in anomalously low estimates of microbial biomass. The flush of inorganic-P was more consistent and, in mor humus, generally related to biomass-C as measured by the Anderson and Domsch test.
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  • 19
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    Plant and soil 76 (1984), S. 275-285 
    ISSN: 1573-5036
    Keywords: Biomass dynamics ; carbon ; Nitrogen ; Nutrient management ; Soil organic matter
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary Dynamics of C, N, S, and to some extent P are expressed by a knowledge of the size and turnover rates of plant constituents such as soluble C and N components, cellulose and hemicellulose, and lignin. Soil organic matter constituents include: the microbial biomass as determined chemically or microscopically, non-biomass active components determined by isotopic dilution, stabilized N constituents for which good techniques are not yet available, and resistant or old C and associated N determined by carbon dating. The processes involved in the nutrient transformations and transfers are reasonably well understood. The control mechanisms require further elucidation to be able to extrapolate from the laboratory to the field, and between field sites. Major control mechanisms requiring further insight include the effects of C availability on transformations of C and N. The other control for which every little is known is that of spatial compartmentalization. Compartmentalization ranges from landscape or management sequences to pedogenic layers, rhizosphere-mycorrhizal effects, clay-sesquioxide surfaces, aggregation, localized enzymes, and microbial effects such as membrane boundaries. Control mechanisms for concurrent mineralization-immobilization, the stabilization of microbial products, and the relative role of the biomass as a catalyst rather than as a source-sink for nutrients, must be understood. There is potential for combining a knowledge of microbial production and turnover with that of the roles of the soil organic active fraction as a temporary storehouse for nutrients. This, in conjunction with management techniques such as zero tillage and crop rotation, should make it possible to better utilize soil and fertilizer N, especially in areas of the world where the cost of nutrients is high relative to the value of the crop grown.
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  • 20
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    Plant and soil 79 (1984), S. 101-121 
    ISSN: 1573-5036
    Keywords: Base saturation ; Bio-climatic zones ; Calcium ; Clay accumulation ; Copper ; C:N ratio ; EDTA ; Forest soils ; Greece ; Iron ; Magnesium ; Manganese ; Nitrogen ; Phosphate ; Potassium ; Soil classification ; Zinc
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary Soils derived from a number of different parent materials (lithologies) and developed along a climatic gradient, manifested by the altitudinal succession of natural vegetation zones (Mediterranean, sub-Mediterranean, Mountainous and Pseudoalpine), were sampled throughout mainland Greece. In soils derived from siliceous parent materials low in clay, acidity increase and percent base saturation decreases from the Mediterranean to the Pseudoalpine vegetation zones. Clay illuviation is found mainly in soils developed in the Mediterranean and the sub-Mediterranean zones. No such changes are apparent in clayey soils rich in bases. Organic matter content of the mineral portion of the soil profile increases by a factor of 2 with a decrease in mean annual air temperature of about 10°C. The pattern of change in clay and soil organic matter content with climate is in relatively good agreement with soil development trends in the area, when soil profiles are named according to the FAO-Unesco soil map of the world. Concentrations of Ca and Mg decrease and those of total N, total and extractable P, K, Fe, Mn and Zn increase from the Mediterranean to the Mountainous zone. Within the same zone, however, concentrations of N, Ca, K, Fe, Mn and Zn decrease, but those of Mg, total and extractable P increase with soil depth. The concentrations of most macro- and micronutrients in the humic horizon are several times higher than those in the mineral portion of the soil profile due to biological enrichment.
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  • 21
    ISSN: 1573-5036
    Keywords: Acidity ; Aluminium ; Cowpea ; Nitrogen ; Rhizobium
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary The interaction of pH (4 or 6), aluminium (0 or 16 ppm at pH 4) and N source (symbiotic or combined) on the growth and nutrient status of cowpea (Vigna unguiculata) was studied in a glasshouse experiment. Low pH significantly decreased the growth of the plants dependent on symbiotic nitrogen fixation but at pH 4 the addition of 16 ppm Al further depressed growth in both nitrogen regimes. Al-ions appear to exert their effect primarily on the root system, as shown by the reduction in total length and fresh weight. The symbiotic development of the plants was affected by low pH but more markedly by the Al treatment. Shoot nitrogen concentrations were reduced from ca. 2.6% at pH 6 to 1.8% and 0.9% at pH 4 without and with aluminium respectively. Calcium concentration was decreased by low pH and further by Al in both nitrogen regimes. In all Al-treated plants, the aluminium was mainly accumulated in the roots and was associated with an increase in their phosphorus concentration.
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  • 22
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    Plant and soil 81 (1984), S. 291-293 
    ISSN: 1573-5036
    Keywords: Casuarinaceae ; Citrulline ; Frankia ; Nitrogen ; Nutrition ; Xylem sap
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary The major nitrogenous compound in the xylem sap ofCasuarina equisetifolia is citrulline, irrespective of nitrogen nutrition (dinitrogen fixation, nitrate or ammonium). The detection of citrulline in non-nodulated Casuarina suggests that its formation is not confined to root nodules. This precludes the possibility of using the relative citrulline content of xylem sap for quantification of N2 fixation in Casuarina. The possibility exists, however, that the relative abundance of citrulline to other nitrogenous compounds (e.g. amides or nitrate) in the xylem sap could be used as an indicator of N2 fixation and should be evaluated further.
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  • 23
    ISSN: 1573-5036
    Keywords: Balsam fir ; Foliar analysis ; Lime ; Nitrogen ; Phosphorus
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary The following fertilizer treatments were applied to a 20-year-old aspen-birch-sprucefir stand in southeastern Maine: N at 448 kg/ha, P at 112 kg/ha, N and P applied as above in addition to 1751 kg/ha Ca and 27 kg/ha Mg. Five years after treatment, foliar concentrations of N, P and Ca for understory blasam fir exhibited significant increases in response to fertilization with those nutrients. Mean five-year height growth, adjusted for pretreatment differences, increased 36 percent in response to fertilization with N alone and in combination with P and lime.
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  • 24
    ISSN: 1573-5036
    Keywords: Calcium ; Eucalyptus saligna ; Eucalyptus wandoo ; Foliar nutrients ; Magnesium ; Nitrogen ; Phosphorus ; Potassium ; Rehabilitation ; Seasonal trends
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary Seasonal changes in the foliar concentration of macronutrients (N, P, K, Ca and Mg) in sapling trees ofEucalyptus saligna Sm. andE. wandoo Blakely growing in rehabilitated bauxite mined areas in the Darling Range of Western Australia are described. Foliar N concentration decreased with age of the fully expanded leaf tissue. Leaf N concentrations were also high when rates of litter decomposition were expected to be high during the period of early spring. The greatest foliar N difference between trees growing in good soil conditions and those from poorer soil conditions also occurred during this period. Levels of P in leaves were highest in young developing leaves but once the leaves reached full size, no seasonal trend in P concentration was observed. Foliar K was lower during the winter and probably related to the period of maximum leaching by precipitation. High foliar K during summer, however, could be related to the role of K in lowering cellular water potential. Leaf Ca was highest during early sping. Low mobility of cellular Ca during the cool portion of the year was indicated. Foliar Mg showed a weak pattern of decreasing concentration with leaf age. The best season for sampling for these broadleafed evergreen species to provide information on plant nutrient status appears to be in spring.
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  • 25
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    Plant and soil 80 (1984), S. 391-405 
    ISSN: 1573-5036
    Keywords: Carbon ; Clear cutting ; Exponential decay ; Forest ; Litter ; Mineralization ; Nitrogen ; Podzol ; Respiration ; Rhizosphere Soil
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary Leaf litter breakdown and fine root production, including exudation, are two major influences upon carbon and nitrogen mineralization rates in forest soil. Sieving and root removal experiments were used to examine their effects. Although carbon mineralization rates declined in smaller particle size fractions of forest litter, this trend largely disappeared when results were calculated on an ash-free basis. Nitrogen mineralization by contrast, was greatest in smaller fractions. Much of the variation in carbon mineralization rates appeared to be associated with fine roots. A rapid initial exponential decay phase noted in laboratory respiration studies was probably associated with disappearance of available carbon in the form of root exudates and/or the microorganisms dependent on them. Clear cutting caused a marked reduction in the size of available carbon pools, reflecting decreased root exudation and rhizosphere activity. A model of mineralization is proposed which represents the available and humified carbon pools.
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  • 26
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    Nutrient cycling in agroecosystems 5 (1984), S. 245-257 
    ISSN: 1573-0867
    Keywords: Adamantane-type compounds ; Fertilizer ; High analysis nutrient compounds ; Nitrogen ; Phosphorus ; Phytotoxicity
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract In a preliminary assessment of the fertilizer capability of three high analysis NP(S) compounds, their possible phytotoxic effects were investigated in solution culture tubes. One of the compounds was studied in more detail in pot experiments with sand and a red-brown earth soil. Two adamantane-type compounds (APA and APAS) were capable of supplying N and P to plants, but also showed toxicity effects. With APA, this effect appeared to be dissipated in soil but not in sand. The toxic effect was alleviated by addition of soluble P or soluble P + N. Some plants absorbed excessive amounts of P, probably not all in the form of orthophosphate.
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  • 27
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    Plant and soil 81 (1984), S. 421-428 
    ISSN: 1573-5036
    Keywords: Acetylene inhibition ; Denitrifiers ; Electron acceptor ; Incubation ; Nitrate ; Nitrous oxide ; Nitrogen
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary A total of 81 strains isolated by T. N. Gamble from soils from eight countries, fresh water lake sediments and nitrified poultry manure were examined for their ability to grow on N2O as their electron acceptor, as well as for their tendency to produce N2O from NO 3 − in the absence and presence of acetylene. Seventy-seven of the 81 strains were confirmed as denitrifiers. Fifty-nine of the 77 strains grew on N2O, while 12 strains produced N2O but could not utilize it. Six strains reduced NO 3 − to N2 but could not grow on N2O, suggesting that even if N2O is always an intermediate product of denitrification, it is not always a freely diffusible intermediate. The organisms, however, would consume N2O that accumulated early in growth and accumulated N2O in the presence of acetylene. Thus the total number of N2O users was 65 strains or 83% of the total tested. This implies that the N2O reducing capacity of denitrifiers occur widely in nature. A high proportion ofPseudomonas fluorescens biotype II reduced N2O. The accumulation of N2O from NO 3 − in the presence of acetylene provides strong evidence that N2O is generally an intermediate in denitrification as well as provides additional support for the usefulness of this chemical as a general inhibitor of N2O reduction.
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  • 28
    ISSN: 1573-5036
    Keywords: Citrus ; Controlled-release fertilizers ; Nitrogen ; Nutrition ; Sulfur-coated urea ; Ammonium nitrosulphate
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary The effect of one application of the slow-release fertilizer, sulfur-coated urea, on the nitrogen level in leaves, fruit and bark of Washington Navel orange trees was studied during the different periods of the annual vegetative cycle, in comparison with two annual applications of the fertilizer ammonium nitrosulphate. Results indicate that a single spring application of 750 g nitrogen per tree maintains N levels in old leaves, spring shoots, ovaries, fruit and bark statistically equal to those obtained using double doses of ANS in two applications.
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  • 29
    ISSN: 1573-5036
    Keywords: Branch nutrients ; Calcium ; Eucalyptus saligna ; Eucalyptus wandoo ; Foliar nutrients ; Magnesium ; Nitrogen ; Phosphorus ; Potassium ; Rehabilitation ; Soil nutrients
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Summary The macronutrient variation within four 6 year oldEucalyptus saligna and four 5 year oldE. wandoo growing on rehabilitated bauxite pits was determined. Significant differences in mean nutrient concentrations were generally recorded between good soil condition sites and poor soil sites, between tree individuals, branch height, and plant organ type; but mean nutrient values were not different among canopy aspects. Fully expanded leaves of the current year provided the most uniform nutrient levels among the plant organs and showed major differences between sites with good soil nutrient conditions and those with poor conditions. Differences in foliar and branch levels of N, P, K, Ca and Mg, the variation between sites, canopy heights and plant organ types, and the use of foliar nutrient levels to indicate deficiencies are discussed.
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  • 30
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    Environmental biology of fishes 10 (1984), S. 243-251 
    ISSN: 1573-5133
    Keywords: Lipid ; Protein ; Carbohydrate ; Nitrogen ; Ash ; Caloric content ; Larval development ; Nutrition ; Elopiformes ; Albulidae
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Synopsis Energy use and changes in whole-body content of lipid, protein, nitrogen, carbohydrate and ash were followed during metamorphosis of leptocephalous larvae of the bonefish (Albula). During metamorphosis, which requires about 8–12 days, larvae lost about 3–4 mg of lipid, or about 50% of the total lipid content. Lipid levels, calculated on a dry weight basis, showed no discernible trends, with values ranging from 138–185 mg (g dry wt)−1. Protein content was 8.4 mg per larva and showed no significant change. However, protein levels increased from 147 to 329 mg (g dry wt)−1. Nitrogen content decreased slightly from about 3.5 to 3.2 mg per larva. A comparison of protein and nitrogen values, expressed as % dry weight, showed that, in larvae which were just beginning to metamorphose, 70% of the total nitrogen was non-protein nitrogen (NPN). The NPN decreased to 58% of the total nitrogen towards the end of metamorphosis. Carbohydrate content fell from about 3.5 to 0.6 mg per larva, which represents an 83% loss. Carbohydrate levels also fell from about 81 to 32 mg (g dry wt)−1. In addition, most of the carbohydrate appears to be bound to protein. Ash content decreased by 52%, from 4.6 to 2.2 mg per larva. Caloric content fell slightly from about 182 to 141 calories per larva whereas caloric density showed no discernible trends, with values ranging from 4.180 to 4.725 kcal (g dry wt)−1. These results indicate that metamorphosing leptocephali, which apparently do not feed, probably derive most of their energy requirements from metabolizing endogenous lipid and carbohydrate stores formed during the premetamorphic interval.
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