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  • 1
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Science Ltd
    Grass and forage science 60 (2005), S. 0 
    ISSN: 1365-2494
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Soil organic carbon (SOC) stocks in different terrestrial ecosystems have already been calculated. However, SOC stocks of grassy verges and grass-covered urban areas have never been reported. In this study the total grass-covered area of verges and urban areas in different agro-pedological regions of Flanders, Belgium was calculated and SOC stocks estimated. The total grassy area of verges along roads, waterways and railways was calculated to be 18 027 ha, 9530 ha for gardens and parks and 2360 ha for recreations areas. Total SOC stock for grass-covered verges, extrapolated to a depth of 1 m, was estimated to be 3520 kt SOC. Total SOC stock for grassy vegetation in urban areas was 1738 kt SOC. These total SOC stocks equate, respectively, to 0·10 and 0·05 of the total SOC stock in Flemish grassland.
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  • 2
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Science Ltd
    Grass and forage science 59 (2004), S. 0 
    ISSN: 1365-2494
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Articles 3·3 and 3·4 of the Kyoto protocol provide Annex I countries the possibility to reduce greenhouse gas emissions through the sequestration of carbon (C) in their terrestrial ecosystems. For such accounting, the 1990 flux is needed and, therefore, a correct knowledge of the baseline (1990) C stocks is necessary. In addition, a correct methodology should be used to investigate the capacity of ecosystems to sequester C through changes in land use or management by the end of the first commitment period (2008–2012). At national and regional scales, formulation of baseline C stocks in terrestrial ecosystems is difficult and uncertain. Differences in method of analysis, sampling depth of soil, lack of sufficient C data and the necessity to extrapolate C data to total soil organic C stocks, provide problems when comparing databases with each other. In this study, three extrapolation models were compared with the classical layer-based method to determine the model with the best fit. The model with the best predictions, in relation to the classical layer-based model, uses recent soil C profiles for estimating the parameter k, which represents the decrease in the proportion of soil organic C with depth, and for extrapolating the C data available for 1990 and 2000 to a depth of 1 m. The other two models gave large underestimates.
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  • 3
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Journal of Chromatography A 45 (1969), S. 315-316 
    ISSN: 0021-9673
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Bioresource Technology 50 (1994), S. 193-200 
    ISSN: 0960-8524
    Keywords: Wood-wastes ; composting ; enzymes ; humification ; microbial biomass ; nitrification ; specific respiration activity
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition , Process Engineering, Biotechnology, Nutrition Technology
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Biology and fertility of soils 32 (2000), S. 186-193 
    ISSN: 1432-0789
    Keywords: Key words Nitrogen variability ; Grazed grassland ; Nitrogen losses ; Leaching ; Geostatistics
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract  The within-field variability of soil mineral nitrogen (Nmin) in a grazed grassland of 8000 m2 was examined. NO3 –-N concentrations were characterized by a high spatial variability. This can be explained by the uneven deposition of animal excreta. All NH4 +-N as well as NO3 –-N values were lognormally distributed, before and after the grazing season. At the end of the grazing season the largest part of the variability of NO3 –-N was found for NO3 –-N concentrations measured within a distance of a few metres. A high variability for NO3 –-N over very short distances was also indicated by a large nugget variance. During the grazing season, observed mean Nmin values increased from 22 to 132 kg N ha–1. Regions with clearly higher NO3 –-N concentrations could be identified. These zones matched with the drinking place and the entrance of the pasture, places which were more frequently visited than others. High residual N levels in autumn led to relatively high losses of N, mostly by leaching, during the subsequent drainage period. Knowing the variability of Nmin, the number of samples needed to estimate the average Nmin in a field could be calculated for different probabilities and various degrees of precision. From the spatial distribution of the Nmin concentrations and the restrictions imposed by the new European decree, adapted fertilizer strategies can be proposed at least for places where systematically higher Nmin concentrations can be expected.
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Biology and fertility of soils 28 (1999), S. 393-396 
    ISSN: 1432-0789
    Keywords: Key words Nitrous oxide ; Emission ; Rye grass
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract  The possibility of an additional N2O emission pathway via plants was investigated in a soil-rye-grass (Lolium perenne L.) system. The N2O emission rate of the system varied between 0.8 and 13.3 mg N2O-N m–2 day–1. Comparing the N2O emission rate of the system before and immediately after cutting the rye grass allowed us to calculate the contribution of the rye grass to the N2O emission from the soil-plant system. It was found that, depending on the type of fertilization and the growing period of the plants, the N2O released from the rye grass varied between 0 and 2.8 mg N2O-N m–2 day–1. N 2 O emission mediated by the rye grass increased towards the end of the growing period. An exponential correlation [R2=0.93, y=(8×10–6 x 2 )–(2×10–5 x)+0.21] was observed between the N2O emission (y) from the rye grass and its NO3 ––N content (x). However, it was not clear whether N2O was produced by the plants themselves or whether the rye grass served as a conduit for N2O produced in the soil.
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  • 7
    ISSN: 1432-0789
    Keywords: Key words Dry biomass production ; Maize ; 15N isotope ; Nitrite toxicity ; Nitrogen recovery
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract  When comparing nitrite (NO2 –) and nitrate (NO3 –) toxicity to maize (Zea mays L.) growth, it is important to know the fate of applied nitrogen (N). A pot experiment, using potassium nitrite (K15NO2) and potassium nitrate (K15NO3) was conducted to determine the fate of N (0, 75, 150, and 225 mg N kg–1 soil) applied to a sandy loam soil collected from Gistel (Belgium). The total dry weight of the plants treated with NO2 – was lower than that of the plants treated with NO3 – at 15 and 26 days after N application (harvest 1 and harvest 2, respectively). Shoot and root biomass reduction started at a relatively low NO2 – application rate (75 mg NO2 –-N kg–1). Biomass reduction increased, at both harvests with increasing amounts of NO2 – to more than 55% at the highest application rate (225 mg NO3 –-N kg–1). In the NO3 – treatment, a reduction of 16% in total plant dry biomass was recorded only at the highest application rate (225 mg NO2 –-N kg–1), at both harvest times. The 15N plant uptake (shoots plus roots) at harvest 1 decreased with increasing N application rates of both N forms (KNO2 and KNO3). Twenty-six days after the N application, the total 15N taken up by the plant increased in all treatments in comparison with 15 days after the N application. However, only at higher rates of N application (150 and 225 mg N kg–1) was the 15N uptake by the NO2 – fed plants significantly lower than by the NO3 – fed plants. The percentage of immobilized N from the applied N was low (0–17.7%) at both harvests, irrespective of the N source. However, with relatively low N application rates (75 mg N kg–1), the immobilized N in the soil decreased with time. This may be due to the re-mineralization of the applied N. The percentage of inorganic 15N in the soil in NO2 – treatments was slightly lower than in equivalent doses of NO3 –. This might be due to higher losses of N as N-oxides. Unaccounted for N from the applied N ranged from 21% to 52% for the NO2 – treatments and from 3% to 38% for the NO3 – treatments.
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Biology and fertility of soils 28 (1999), S. 321-328 
    ISSN: 1432-0789
    Keywords: Key words Mineral nitrogen ; Morocco ; Plant available nitrogen ; Vertisol ; Wheat
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract  The evoluion of NH4 +-N and NO3 –-N was monitored during three growing seasons, 1992–1993, 1993–1994, 1994–1995 in the soil profile (0–60 or 0–90 cm) under bare fallow and wheat on a vertisol site of the Sais plateau, Morocco. The aim of this study was to relate the soil mineral N dynamics to crop N uptake and soil N transformation processes. The efficacy of the current N fertilisation rate (100 kg N ha–1) for wheat production in the region was evaluated. The high level of residual mineral N in the soil profile resulted from a low N plant uptake relative to the soil N supply and N fertilisation, and masked the effect of N fertilisation on dry matter accumulation. NH4 +-N was present in considerable amounts, suggesting a low nitrification rate under the given pedo-climatic conditions. An artefact due to the sampling procedure was encountered shortly after the application of N fertiliser. Losses through leaching and denitrification occurred after heavy rainfall, but were limited. At least part of the exchangeable NH4 +-N seemed to be barely taken up by the crop. NO3 –-N was therefore considered to be a better indicator of plant-available N than total mineral N for this type of soil. The low N fertiliser use efficiencies demonstrated clearly that the current fertilisation rate (100 kg N ha–1) for wheat production in this region is unsustainable. The maximum N uptake ranged from 40 kg N ha–1 to 180 kg N ha–1. The estimation of the seasonal production potential is considered to be the main prerequisite for the determination of the best rates and timing of N fertiliser application in this region.
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  • 9
    ISSN: 1432-0789
    Keywords: Key words Arbuscular mycorrhizal fungi ; Mucuna pruriens ; Nitrogen balance ; Relay cropping ; Indigenous rhizobial populations
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract  Leguminous cover crops such as Mucuna pruriens (mucuna) have the potential to contribute to soil N and increase the yields of subsequent or associated cereal crops through symbiotic N fixation. It has often been assumed that mucuna will freely nodulate, fix N2 and therefore contribute to soil N. However, results of recent work have indicated mucuna's failure to nodulate in some farmers' fields in the derived savanna in Benin. One of the management practices that can help to improve mucuna establishment and growth is the use of rhizobial inocula to ensure compatibility between the symbiotic partners. Experiments were conducted in 1995 and 1996 on 15 farmers' fields located in three different villages (Eglimé, Zouzouvou and Tchi) in the derived savanna in Benin. The aim was to determine the response of mucuna to inoculation and examine the factors affecting it when grown in relay cropping with maize. The actual amount of N2 fixed by mucuna in the farmers' fields at 20 weeks after planting (WAP) averaged 60 kg N ha–1 (range: 41–76 kg N ha–1) representing 55% (range: 49–58%) of the plant total N. The result suggested that mucuna in these farmers' fields could not meet its total N demand for growth and seed production only by N2 fixation. It was estimated that after grain removal mucuna led to a net N contribution ranging from –37 to 30 kg N ha–1. Shoot dry weight at 20 WAP varied between 1.5 and 8.7 t ha–1 and N accumulation ranged from 22 to 193 kg N ha–1. Inoculation increased shoot dry matter by an average of 28% above the uninoculated treatments, but the increase depended on the field, location and year. For the combinations of inoculated treatments and farmers' fields, the response frequency was higher in Eglimé and Tchi than in Zouzouvou. The response to inoculated treatments was dependent on the field and inversely related to the numbers of rhizobia in the soil. Soil rhizobial populations ranged from 0 to 〉188 cells g–1 soil, and response to inoculation often occurred when numbers of indigenous rhizobia were 〈5 cells g–1 soil. In two farmers' fields at Zouzouvou where extractable P was below 10 μg g–1 soil, mucuna did not respond to rhizobial inoculation despite a higher population of rhizobia. Significant relationships between mycorrhizal colonization, growth and nodulation of mucuna were observed, and inoculated plants with rhizobia had a higher rate of colonization by arbuscular mycorrhizal fungi (%AMF) than uninoculated ones. Therefore, it was shown that mucuna will establish and fix N2 effectively in those fields where farmer's management practices such as good crop rotation and rhizobial inoculation allow a build up of AMF spores that might lead to a high degree of AMF infection and alleviate P deficiency.
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  • 10
    Electronic Resource
    Electronic Resource
    Springer
    Biology and fertility of soils 27 (1998), S. 293-298 
    ISSN: 1432-0789
    Keywords: Key words Methane oxidation ; Land use ; Fertilization ; Pesticide
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract  In a first experiment, the effect of land use on the uptake rate of atmospheric CH4 was studied in laboratory incubations of intact soil cores. A soil under deciduous forest showed the highest CH4 oxidation. Its overall CH4 uptake during the measuring period (202 days) was 1.03 kg CH4 ha–1. Natural grassland showed the second highest CH4 oxidizing capacity (0.71 kg CH4 ha–1). The overall amount of CH4 uptake by fertilized pasture was 0.33 kg CH4 ha–1. CH4 oxidation in arable soils with different fertilizer treatments varied between 0.34 and 0.37 kg CH4 ha–1. Undisturbed soils had a higher CH4 uptake capacity than agricultural soils. The moisture content of the soil was found to be an important parameter explaining temporal variations of CH4 oxidation. Different methods of fertilization which had been commenced 10 years previously were not yet reflected in the total CH4 uptake rate of the arable soil. In a second experiment, a number of frequently used pesticides were screened for their possible effect on CH4 oxidation. In a sandy arable soil lenacil, mikado and oxadixyl caused significantly reduced CH4 oxidation compared to the control. Under the same conditions, but in a clayey arable soil, mikado, atrazine and dimethenamid caused a reduction of the CH4 uptake. In a landfill cover soil, with a 100-fold higher CH4 oxidation rate, no inhibition of CH4 oxidation was observed, not even when the application rate of pesticides was tenfold higher than usual.
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