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  • 1
    Online Resource
    Online Resource
    Wiley ; 2005
    In:  Agronomy Journal Vol. 97, No. 6 ( 2005-11), p. 1493-1501
    In: Agronomy Journal, Wiley, Vol. 97, No. 6 ( 2005-11), p. 1493-1501
    Abstract: Forage sorghum–sudangrass [ Sorghum bicolor (L.) Moench] is a relatively new crop to eastern Canada and the effects of additions of fertilizer N on yield, N accumulation, and N use efficiency are not available for this region. In 1998, 1999, and 2000 the response of forage sorghum–sudangrass to additions of fertilizer N rates (0, 50, 100, 150, 200, and 250 kg N ha −1 ) either applied as a single sidedress application or split into two sidedress applications was evaluated on a Fox loamy sand (Psammentic Hapludalf). Although timing of N application had little effect on DM production, splitting the N application into two equal applications may be of benefit by enhancing the NUE and ANR of individual cuts. Maximum yield was estimated at 5.95 Mg ha −1 at an N rate of 125 kg N ha −1 and the most economic rates of N ranged from 83 to 107 kg N ha −1 dependent on the cost of N fertilizer and value of hay. Nitrogen concentration increased linearly with increasing N application and the maximum N accumulation was 161 kg N ha −1 at an N rate of 196 kg N ha −1 . Total N use efficiency and apparent N recovery decreased with increasing N rates ranging from 36 to 11 kg DM kg −1 and 90 to 24%, respectively. Optimum yield and N efficiency occurred when 100 kg N ha −1 was applied as a split application. Producers in southern Ontario require N fertilizer additions to optimize sorghum–sudangrass yields but need to avoid overfertilization with N to maximize N use efficiency and apparent N recovery.
    Type of Medium: Online Resource
    ISSN: 0002-1962 , 1435-0645
    Language: English
    Publisher: Wiley
    Publication Date: 2005
    detail.hit.zdb_id: 1471598-3
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  • 2
    Online Resource
    Online Resource
    Elsevier BV ; 2007
    In:  Geoderma Vol. 138, No. 1-2 ( 2007-2), p. 133-143
    In: Geoderma, Elsevier BV, Vol. 138, No. 1-2 ( 2007-2), p. 133-143
    Type of Medium: Online Resource
    ISSN: 0016-7061
    RVK:
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2007
    detail.hit.zdb_id: 281080-3
    detail.hit.zdb_id: 2001729-7
    SSG: 13
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  • 3
    Online Resource
    Online Resource
    Wiley ; 2002
    In:  Agronomy Journal Vol. 94, No. 4 ( 2002-07), p. 767-774
    In: Agronomy Journal, Wiley, Vol. 94, No. 4 ( 2002-07), p. 767-774
    Abstract: Minimum tillage has been shown to slow early corn ( Zea mays L.) growth and reduce grain yields in some soil types and under some climatic conditions. To overcome these limitations, the no‐till (NT) system can be modified by incorporating residues and loosening the soil in a zone over the center of the row while leaving the interrow area untilled. This study compares soil temperatures and corn growth and productivity under zone till (ZT), NT, and conventional tillage (CT) systems in a coarse‐textured soil (Psammentic Hapludalf) located in southwestern Ontario, Canada. Soil temperature at the 4‐cm depth decreased with decreasing tillage intensity from CT to NT during warmer years but was similar in CT and ZT during a cooler year. This resulted in reduced growing degree days in the seed zone with decreasing tillage. Lower soil temperatures in NT did not delay the initiation of corn seedling emergence but did reduce the rate of emergence compared with CT plots. Corn growth rates were found to be similar among tillage systems in the early part of the growing system but were higher for both the ZT and NT systems during late vegetative and early reproductive growth. Grain yields increased as tillage intensity decreased in a year with drier conditions at tasseling but were similar across tillage systems in the other 2 yr. These results suggest that converting a NT system to a ZT system would neither result in significantly higher yields, nor cause a serious grain yield reduction relative to CT.
    Type of Medium: Online Resource
    ISSN: 0002-1962 , 1435-0645
    Language: English
    Publisher: Wiley
    Publication Date: 2002
    detail.hit.zdb_id: 1471598-3
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  • 4
    In: Global Change Biology, Wiley, Vol. 23, No. 4 ( 2017-04), p. 1725-1734
    Abstract: Widespread global changes, including rising atmospheric CO 2 concentrations, climate warming and loss of biodiversity, are predicted for this century; all of these will affect terrestrial ecosystem processes like plant litter decomposition. Conversely, increased plant litter decomposition can have potential carbon‐cycle feedbacks on atmospheric CO 2 levels, climate warming and biodiversity. But predicting litter decomposition is difficult because of many interacting factors related to the chemical, physical and biological properties of soil, as well as to climate and agricultural management practices. We applied 13 C‐labelled plant litter to soil at ten sites spanning a 3500‐km transect across the agricultural regions of Canada and measured its decomposition over five years. Despite large differences in soil type and climatic conditions, we found that the kinetics of litter decomposition were similar once the effect of temperature had been removed, indicating no measurable effect of soil properties. A two‐pool exponential decay model expressing undecomposed carbon simply as a function of thermal time accurately described kinetics of decomposition. ( R 2  = 0.94; RMSE  = 0.0508). Soil properties such as texture, cation exchange capacity, pH and moisture, although very different among sites, had minimal discernible influence on decomposition kinetics. Using this kinetic model under different climate change scenarios, we projected that the time required to decompose 50% of the litter (i.e. the labile fractions) would be reduced by 1–4 months, whereas time required to decompose 90% of the litter (including recalcitrant fractions) would be reduced by 1 year in cooler sites to as much as 2 years in warmer sites. These findings confirm quantitatively the sensitivity of litter decomposition to temperature increases and demonstrate how climate change may constrain future soil carbon storage, an effect apparently not influenced by soil properties.
    Type of Medium: Online Resource
    ISSN: 1354-1013 , 1365-2486
    URL: Issue
    Language: English
    Publisher: Wiley
    Publication Date: 2017
    detail.hit.zdb_id: 2020313-5
    SSG: 12
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  • 5
    Online Resource
    Online Resource
    Wiley ; 2007
    In:  Soil Science Society of America Journal Vol. 71, No. 4 ( 2007-07), p. 1363-1370
    In: Soil Science Society of America Journal, Wiley, Vol. 71, No. 4 ( 2007-07), p. 1363-1370
    Abstract: Greater knowledge of the dynamics of organic matter in different locations in the soil matrix can provide valuable information for implementing tillage practices that may favor C sequestration and improve soil quality. The objective of this study was to investigate the effect of tillage practices on the dynamics and turnover of organic matter located outside (free light fraction [FLF]) and inside (occluded light fraction [OLF] ) aggregates, and in intimate association with soil minerals (heavy fraction [HF]). Composite soil samples from 11‐yr‐old corn ( Zea mays L.) plots under no‐till (NT) and conventional tillage (CT) practices, and from 〉 60‐yr‐old tobacco ( Nicotiana tabacum L.)–rye ( Secale cereale L.) plots under CT were fractionated into these fractions, and changes in the amounts of total soil organic C (SOC), corn‐derived (C 4 ) C, and native (C 3 ) C and the turnover of native C as a consequence of tillage were estimated. Adoption of NT increased ( P 〈 0.05) standing SOC and C 4 −C stocks in whole soil and all its density fractions in the 0‐ to 5‐cm depth, but it did not alter these in the plow layer (0–20‐cm soil depth), indicating that NT primarily redistributed C within the profile without necessarily increasing SOC storage. Relative to CT, NT slowed the turnover of native C by 1.5 times and marginally ( P = 0.1) increased the sequestration of C 4 −C by 23% in the plow layer in OLF only; however, C 3 − and C 4 −C of OLF accounted for only small (6–10%) proportions of the soil's C 3 − and C 4 −C. Therefore, NT did not result in increased SOC sequestration in the plow layer.
    Type of Medium: Online Resource
    ISSN: 0361-5995 , 1435-0661
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 2007
    detail.hit.zdb_id: 241415-6
    detail.hit.zdb_id: 2239747-4
    detail.hit.zdb_id: 196788-5
    detail.hit.zdb_id: 1481691-X
    SSG: 13
    SSG: 21
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  • 6
    In: European Journal of Immunology, Wiley, Vol. 49, No. 10 ( 2019-10), p. 1457-1973
    Abstract: These guidelines are a consensus work of a considerable number of members of the immunology and flow cytometry community. They provide the theory and key practical aspects of flow cytometry enabling immunologists to avoid the common errors that often undermine immunological data. Notably, there are comprehensive sections of all major immune cell types with helpful Tables detailing phenotypes in murine and human cells. The latest flow cytometry techniques and applications are also described, featuring examples of the data that can be generated and, importantly, how the data can be analysed. Furthermore, there are sections detailing tips, tricks and pitfalls to avoid, all written and peer‐reviewed by leading experts in the field, making this an essential research companion.
    Type of Medium: Online Resource
    ISSN: 0014-2980 , 1521-4141
    URL: Issue
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 2019
    detail.hit.zdb_id: 1491907-2
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