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Summary Observations on the rate of sorption of phosphate by four samples of Danish soils have been re‐examined. A previously reported lag phase in plots of log concentration against log time could be ascribed to the use of large solution:soil ratios rather than to the inclusion of short periods of reaction.  相似文献   
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The effect of heterogeneous resource distribution in soil has seldom been studied under controlled laboratory conditions, even though this type of distribution is the rule rather than the exception in both agricultural and undisturbed soil systems. We use distribution trials to test the effect of stratified distribution of chopped maize, sheep faeces derived from maize, and chopped rape stems compared with even distribution. In all treatments, CO2 mineralization decreased initially in the stratified experiments and in the rape treatment less (39 versus 43%) of the added carbon was mineralized even after 202 days of incubation at 15°C. In both maize and rape residue treatments, we observed much less immobilization of Nmin and less microbial growth in the stratified experiments. The data set for rape was sufficiently detailed to allow a model interpretation using a spreadsheet version of the soil organic matter module from DAISY, a soil‐plant‐atmosphere system model. This indicated that the observed differences between the stratified and evenly distributed experiments could be largely understood by assuming diffusion limitation of nitrate from the bulk soil to the residuesphere. The residuesphere is the part of soil that is immediately affected by the decomposition of residue, and was assumed to be included in the first 10 mm of soil surrounding the residues in the stratified experiments at all times. Only a very small part of the variation in CO2 respiration, Nmin and soil microbial biomass N (SMB‐N) could be explained by additionally assuming less substrate utilization efficiency of the less decomposable fraction of rape in the stratified experiment. We observed greater N mineralization in the evenly distributed experiment with faeces, and smaller concentrations of soil microbial biomass nitrogen extracted by chloroform fumigation. We assume that most of the additional SMB‐N determined in the faeces treatments was from microorganisms present in the faeces at the time they were added to soil, and that these were less susceptible to microbial predation in the stratified than in the distributed experiment. We conclude that the spatial distribution of decomposing litters in soil significantly affects the C and N dynamics. Diffusion limitation of available N in the active zone of decomposition was the main causal agent, which induced a decrease in microbial growth and substrate utilisation.  相似文献   
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Net N mineralization from plant materials represents the difference between the two opposing processes of gross N mineralization and immobilization. This complicates the derivation of useful relationships between rates of net mineralization and litter quality indices. The purpose of the current paper is to present a model for net N mineralization from plant material that is based on relationships between (1) gross N mineralization and respiration and (2) gross N immobilization and respiration found in studies applying 15N dilution techniques. Together these relationships produce an overall relationship between net N mineralization and C mineralization that can be used to predict net N mineralization from respiration. The applicability of the model was tested by applying it to the mineralization dynamics of 75 plant materials with widely differing qualities. In a model validation on eight independent plant materials, the relations between net N mineralization and C mineralization resulted in good predictions of observed net N mineralization patterns from the C mineralization pattern, depending only on the C/N ratio of the plant material (R2=0.90). This suggests that the relationship between net N mineralization and respiration is largely unaffected by the chemical composition of the plant material other than the C/N ratio. This means that the chemical composition of the plant material may primarily influence N mineralization through its effect on C mineralization. Furthermore, the relationship between net N mineralization and C mineralization is useful for predictions of net N mineralization because C mineralization is generally much easier to predict than net N mineralization.  相似文献   
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Products made from Herba Santa (Eriodictyon californicum (H. & A.) Torr.) have been used as bitter remedies for some pharmaceutical applications for many years, but they are actually too aromatic to be useful for many food or pharmaceutical applications. In sensory studies flavanones homoeriodictyol (1), its sodium salt (1-Na), sterubin (2), and eriodictyol (4) could significantly decrease the bitter taste of caffeine without exhibiting intrinsic strong flavors or taste characteristics. Further investigations on 1-Na elicited a broad masking activity between 10 and 40% toward different chemical classes of bitter molecules (e.g. salicin, amarogentin, paracetamol, quinine) but not toward bitter linoleic acid emulsions. For caffeine and amarogentin, dose-response studies were performed; the masking activity toward bitter taste for both compounds reached a plateau at higher concentrations of 1-Na. Due to these facts, homoeriodictyol sodium salt (1-Na) seems to be a very interesting new taste modifier for food applications and pharmaceuticals.  相似文献   
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European Journal of Plant Pathology - Claviceps purpurea causing ergot maintains to be a problem in commercial cytoplasmic male sterile (CMS)-based hybrid rye growing. The fungal spores compete...  相似文献   
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