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  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Biology and fertility of soils 29 (1999), S. 201-206 
    ISSN: 1432-0789
    Keywords: Key words Corn-forage rotation ; NO3-N ; No till ; Conventional till
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract  Efficient N-fertiliser management during the corn (Zea mays L.) phase in corn-forage rotation requires information on temporal dynamics of N release from forage biomass. The influence of forage phase, in corn-forage rotation, and no- versus conventional-till on (1) in situ temporal dynamics of soil nitrate-N (NO3-N) during corn phase and (2) corn grain yield was investigated in this study. The data used were collected from a crop rotation (corn-forage) experiment, with superimposed tillage treatments, established on a silt loam soil in 1988 and continued until 1994. The cropping treatments were continuous conventionally cultivated (CT) corn, rotations involving corn and forages (alfalfa, Medicago sativa L.; and bromegrass, Bromus inermis L.) and continuous minimally tilled corn with under-seeded red clover (Trifolium pratense L.). The forages were grown for 6 years and corn was re-introduced in these plots under no- and conventional-till systems. Soil NO3-N in the top 30 cm depth, determined six times during the corn phase, was significantly influenced by previous forage species and tillage system. Regression analysis indicated soil NO3-N under continuous CT corn did not show significant temporal changes. In the rotations, soil NO3-N after tillage or herbicide treatment, i.e. in no-till, increased with time until 45 days after tillage (DAT), reached a plateau between 45 and 65 DAT, and then decreased with time. During the plateau, soil NO3-N in rotation plots ranged from 17 to 33 mg kg–1 compared to 15.7 mg kg–1 in the continuous CT corn. Tillage increased soil NO3-N concentration in alfalfa plots whereas an opposite trend existed in the bromegrass plots. Soil NO3-N in the rotation plots increased at rates ranging from 0.71 to 1.63 mg kg–1 day–1. The interaction involving forage species and the temporal dynamics of soil NO3-N accounted for 68–77% of variability in corn grain yield.
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Soil Technology 3 (1990), S. 145-152 
    ISSN: 0933-3630
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Soil Technology 3 (1990), S. 167-172 
    ISSN: 0933-3630
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Soil & Tillage Research 31 (1994), S. 187-198 
    ISSN: 0167-1987
    Keywords: Aggregate size distribution ; Crushing energy ; Fractal dimension ; Fragmentation ; Tillage
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Soil & Tillage Research 32 (1994), S. 135-148 
    ISSN: 0167-1987
    Keywords: Compression ; Crop rotation ; Fragmentation ; Wet sieving
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Soil Science Society of America journal 62 (1998), S. 1197-1202 
    ISSN: 1435-0661
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: us ) at microscale in soil, experimental determination of this property is difficulty. The objectives of this study were to: (i) seek a simple, but reliable, procedure for the estimation of Kus at microscale and (ii) determine the sensitivity of the estimates to wetting-induced changes in selected structural parameters (porosity, ɛ, surface fractal dimension, D, and pore continuity, PC). Using computer-assisted tomography (CAT), spatial distributions of soil water content (θ) and changes in ɛ that occurred during wetting were monitored at 2 by 2 mm resolution at 1-cm depth increments in water-stable (WSA) and unstable aggregate (USA) columns. The Fuentes theoretical equation, which requires data on saturated hydraulic conductivity (Kɛ), θ, ɛ, and D, was used for the estimation of the spatial distribution of Kus. The spatial distribution of θ in WSA columns ranged from 0.113 to 0.327 cm3 cm-3 and from 0.175 to 0.567 cm3 cm-3 in the USA columns. The spatial distribution of ɛus ranged from 0.46 to 0.74 and was used in the computation of D and PC. Values of Kɛ ranged from 0.006 to 0.745 cm h-1. The spatial distribution of Kus ranged from 6.87 X 10-4 to 1.49 X 10-2 cm h-1 in WSA compared with 7.3 X 10-4 to 4.11 X 10-2 cm h-1 in USA. Pore continuity, θ, D, and initial aggregate diameter (x) accounted for 94 to 95% of the variability in Kus distributions. The results indicate that reliable estimates of Kus distributions at microscale can be computed from single-source CAT-derived data on θ and ɛ.
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Water, air & soil pollution 65 (1992), S. 143-151 
    ISSN: 1573-2932
    Source: Springer Online Journal Archives 1860-2000
    Topics: Energy, Environment Protection, Nuclear Power Engineering
    Notes: Abstract Biodegradation rates of oily waste in soil can be limited by mineral nutrients, particularly N and P. A laboratory incubation experiment was carried out to investigate the influence of N forms, nitrate (NO− 3-N) vs ammonium nitrogen (NH+ 4-N), and sources, i.e., the conjugate cations/anions, on C mineralization rate (CMR) was determined daily by measuring the CO2 evolved using gas chromatography. The CMR and the cumulative C mineralized (CCM) varied with the form and/or the source of N applied. The greatest enhancement in CMR occurred in the NO− 3-treatments in which the source conjugate cation was Ca+2. The addition of P fertilizer further enhanced C mineralization rates irrespective of the form and/or the source of N added. The results show that up to 45% of the added oily waste mineralized as CO2-C in 28 d. The residual P and N (NO− 3-N plus NH+ 4-N) data showed that approximately 90% of the added P and N were utilized for oil decomposition. The amount of residual NO− 3-N appeared to have an inverse relationship with CCM. The NO− 3-N utilization occurred at the expense of NH+ 4-N and this was particularly high in the treatments which received P.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Water, air & soil pollution 63 (1992), S. 179-186 
    ISSN: 1573-2932
    Source: Springer Online Journal Archives 1860-2000
    Topics: Energy, Environment Protection, Nuclear Power Engineering
    Notes: Abstract Stabilization of oily waste organics (OWO) in soils of land treatment farms (LTF) can limit the availability of the OWO for biodegradation. The effect of physical dispersion on bioavailability and biodegradation of OWO in a soil from a LTF was investigated. Soil samples from the LTF were ultrasonically dispersed at increasing energy levels (EL), ranging from 0 to 30 kJ kg−1 at 5 kJ kg−1 increments, and incubated in glass jars for 12 weeks. The headspace CO2 concentration in the jars was monitored weekly by gas chromatography and expressed as C mineralization rates (CMR). The CMR and the cumulative C mineralized (CCM) increased with increasing EL. The CCM from the oily waste treated soil dispersed at 30 kJ kg−1 was 710% higher compared to that from the untreated soil dispersed at the same EL. Compared to the treated soil dispersed at zero EL, 48% more C mineralized from that dispersed at 30 kJ kg−1. The size of the potentially mineralizable C (C0) increased with increasing EL. The C0 for the treated soil dispersed at 30 kJ kg−1 was 66% larger compared to that at zero EL. The C0's for the treated soil dispersed at different EL were similar, suggesting the chemistry of the C0 exposed by dispersion were similar. The results show that substantial amounts of potentially biodegradable OWO were physically protected in soil aggregates.
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Water, air & soil pollution 71 (1993), S. 347-355 
    ISSN: 1573-2932
    Source: Springer Online Journal Archives 1860-2000
    Topics: Energy, Environment Protection, Nuclear Power Engineering
    Notes: Abstract A laboratory incubation experiment to assess (a) the effectiveness of six surfactants as emulsifiers in enhancing oily waste carbon mineralization rates (CMR), (b) the influence of ion charge of the surfactants on CMR, and (c) the biodegradation of the surfactants in soil, is described. The CMR and the net cumulative C mineralization (CCM) data indicated that among the six surfactants evaluated two were significantly effective in enhancing CMR through emulsification. They were CEDEPHOS FA-600, an anionic surfactant mixture of mono- and di- organo phosphate esters and IGEPAL CO-603, a nonionic ethoxylated alkylphenol.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Springer
    Water, air & soil pollution 59 (1991), S. 249-259 
    ISSN: 1573-2932
    Source: Springer Online Journal Archives 1860-2000
    Topics: Energy, Environment Protection, Nuclear Power Engineering
    Notes: Abstract A laboratory incubation experiment was carried out to investigate the effects of N fertilizer forms, NO in3 sup− ,-N vs NH in4 sup+ -N, and rates of application on C mineralization of an oily waste in a clay-loam soil. Carbon mineralization rates (CMR) were determined from CO2 (measured routinely by gas chromatography) evolved during a seven week incubation. The CMR and cumulative C mineralized (CCM) increased with increasing levels of fertilizer N added. The greatest enhancement in waste C mineralization occurred when the waste-C: fertilizer-N (WC:FN) ratio was in the range 18 to 22:1. Variabilities in estimates of the potentially mineralizable C pool sizes and specific mineralization rate constants showed that these decomposition parameters were altered by N amendment. Of the three fertilizer N sources evaluated, amendment with calcium nitrate produced the greatest enhancement in waste C mineralization, at each WC:FN ratio, followed by urea and ammonium nitrate, respectively.
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