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Temporal distribution

The rhizosphere lacks physically precise delimitation (18). The volume of rhizosphere depends on the rate of exudation and impact utilization of rhizodeposits (Chap. 6). The spatial and temporal distribution of exudates as well as their metabolism is related to the concentration of CO (Chap. 6). However, according to Darrah (Chap. 11), the layer of soil where microbial growth is affected by exudates can be 1-2 mm wide. [Pg.4]

Data on weather conditions, especially temperature and rainfall (temporal distribution and intensity) in the study area are essential for the evaluation of the dissipation data. It is very important to understand the water balance in the paddy field as accurately as possible when calculating the rate of outflow. Records of changes in water temperature and sediment temperature are also helpful for modeling the behavior of a chemical in the rice paddy field. [Pg.897]

The first step in a wildlife exposure assessment is to document the occurrence and persistence of a pesticide in the study area throughout the study duration. Several articles in this book describe the experimental designs and best practices to conduct field crop and environmental dissipation (air, soil and water) studies. This article presents methods to quantify spatial and temporal distributions of pesticide presence in ecosystems following normal application and resultant exposure of nontarget wildlife. [Pg.936]

At another level, certain KBS approaches provide the mechanisms for decomposing complex interpretation problems into a set of smaller, distributed and localized interpretations. Decomposition into smaller, more constrained interpretation problems is necessary to maintain the performance of any one interpreter and it makes it possible to apply different interpretation approaches to subparts of the problem. It is well recognized that scale-up is a problem for all of the interpretation approaches described. With increases in the number of input variables, potential output conclusions, complexity of subprocess interactions, and the spatial and temporal distribution of effects, the rapidity, accuracy, and resolution of interpretations can deteriorate dramatically. Furthermore, difficulties in construction, verification, and maintenance can prohibit successful implementation. [Pg.72]

Environmental fate models require information on the distribution of releases over time and space. Basically, sources can be described in terms of their dimensionality and releases in terms of their temporal distribution. [Pg.10]

There are also several possibilities for the temporal distribution of releases. Although some releases, such as those stemming from accidents, are best described as instantaneous release of a total amount of material (kg per event), most releases are described as rates kg/sec (point source), kg/sec-m (line source), kg/sec-m (area source). (Note here that a little dimensional analysis will often indicate whether a factor or constant in a fate model has been inadvertently omitted.) The patterns of rates over time can be quite diverse (see Figure 3). Many releases are more or less continuous and more or less uniform, such as stack emissions from a base-load power plant. Others are intermittent but fairly regular, or at least predictable, as when a coke oven is opened or a chemical vat... [Pg.10]

Steinhausler, F., W. Hofmann, E. Pohl, and J. Pohl-Ruling, Local and Temporal Distribution Pattern of Radon and Daughters in an Urban Environment and Determination of Organ Dose Frequency Distributions With Demoscopical Methods, in Proceedings of the Symposium on Natural Radiation Environment. III. Houston. Conf-780422, DOE Sym. Ser. 51, Vol. II, pp. 1145-1161, Houston NM,... [Pg.502]

Vryzas Z, Vassiliou G, Alexoudis C, Papadopoulou-Mourkidou E (2009) Spatial and temporal distribution of pesticide residues in surface waters in northeastern Greece. Water Res 43(1) 1—10... [Pg.161]

Fig. 10 Composition and spatial distribution of the main patterns of contamination identified in sediment of the Ebro River basin from year 2004 to 2006. Different temporal distribution of the PAHs pattern of contamination over the territory and constant distribution in time of the APs and heavier PAHs as well as the OCs pattern. Big circles representing higher levels of pattern contribution than small circles. Variables identification 1, naphthalene 2, acenaphtylene 3, acenapthene 4, fluorene 5, phenanthrene 6, anthracene 7, fluoranthene 8, pyrene 9, benzo(a) anthracene 10, chrysene 11, benzo(b)fluoranthene 12, benzo(k)fluoranthene 13, benzo(a)pyr-ene 14, indeno(l,2,3-cd)pyrene 15, dibenzo(a,h)anthracene 16, benzo(g,h,i)perylene 17, octyl-phenol 18, nonylphenol 19, tributylphosphate 20, a-HCH 21, HCB 22,2,4-DDE 23,4,4-DDE 24, 2,4-DDD 25, 4,4-DDD 26, 2,4-DDT 27, 4,4-DDT... Fig. 10 Composition and spatial distribution of the main patterns of contamination identified in sediment of the Ebro River basin from year 2004 to 2006. Different temporal distribution of the PAHs pattern of contamination over the territory and constant distribution in time of the APs and heavier PAHs as well as the OCs pattern. Big circles representing higher levels of pattern contribution than small circles. Variables identification 1, naphthalene 2, acenaphtylene 3, acenapthene 4, fluorene 5, phenanthrene 6, anthracene 7, fluoranthene 8, pyrene 9, benzo(a) anthracene 10, chrysene 11, benzo(b)fluoranthene 12, benzo(k)fluoranthene 13, benzo(a)pyr-ene 14, indeno(l,2,3-cd)pyrene 15, dibenzo(a,h)anthracene 16, benzo(g,h,i)perylene 17, octyl-phenol 18, nonylphenol 19, tributylphosphate 20, a-HCH 21, HCB 22,2,4-DDE 23,4,4-DDE 24, 2,4-DDD 25, 4,4-DDD 26, 2,4-DDT 27, 4,4-DDT...
Fig. 13 Contamination patterns identified (MCR-ALS resolved loading profiles) in the Ebro River delta from May to August 2005. On the left loadings in the second mode (normalized for variables to unit norm) describing the composition of the contamination patterns. Variable identification in Table 1. On the right loadings in the first and third modes (mixed) describing spatial and temporal distribution of the contamination patterns. Sampling sites ordered from North to South, for the four analyzed months displayed consecutively (May 1-11 June 12-22 July 23-33 August 34 4)... Fig. 13 Contamination patterns identified (MCR-ALS resolved loading profiles) in the Ebro River delta from May to August 2005. On the left loadings in the second mode (normalized for variables to unit norm) describing the composition of the contamination patterns. Variable identification in Table 1. On the right loadings in the first and third modes (mixed) describing spatial and temporal distribution of the contamination patterns. Sampling sites ordered from North to South, for the four analyzed months displayed consecutively (May 1-11 June 12-22 July 23-33 August 34 4)...
Bowditch, T.G. and Madden, J.L. 1996. Spatial and temporal distribution of Ephestia cautella (Walker) (Lepidoptera Pyralidae) in a confectionery factory Causal factors and management implications. J. Stored Prod. Res. 32, 123-130. [Pg.283]

The overall formation mechanism of PS must involve the fundamental electrochemical reactions in three essential aspects 1. nature of reactions, reactants, products, intermediates, number of steps, and their sequences, 2. nature and rate of charge transport in the different phases at silicon/electrolyte interface, 3. spatial and temporal distributions of reactions and the cause of such distributions. The first and second aspects, which governs the properties of a uniform and flat surface and do not involve geometric factors, have been characterized in previous Sections and the major characteristics are summarized in Table 5. This Section deals with the third aspect, that is, spatial and temporal... [Pg.183]

The fundamental reason for the uneven distribution of reactions is that the rate of electrochemical reactions on a semiconductor is sensitive to the radius of curvature of the surface. This sensitivity can either be associated with the thickness of the space charge layer or the resistance of the substrate. Thus, when the rate of the dissolution reactions depends on the thickness of the space charge layer, formation of pores can in principle occur on a semiconductor electrode. The specific porous structures are determined by the spatial and temporal distributions of reactions and their rates which are affected by the geometric elements in the system. Because of the intricate relations among the kinetic factors and geometric elements, the detail features of PS morphology and the mechanisms for their formation are complex and greatly vary with experimental conditions. [Pg.210]

Imboden, D. M., and R. P. Schwarzenbach (1985), "Spatial and Temporal Distribution of Chemical Substances in Lakes Modeling Concepts", in W. Stumm, Ed., Chemical Processes in Lakes, John Wiley and Sons, New York, 1 -30. [Pg.405]

In the quasi-statie approximation, Eq.(2.9) has been solved numerieally by the FD-BPM for eaeh stationary eomponent of temporal distribution of the light beam. Amplitudes of the stationary eomponents were speeified by the form of pulse temporal envelope. The initial pulse envelope was assumed Gaussian. [Pg.173]


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See also in sourсe #XX -- [ Pg.81 ]

See also in sourсe #XX -- [ Pg.165 ]




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Temporal Power-Law Distribution

Temporal and geographical distribution of fossil organic carbon

Temporal distribution of clusters

Temporality

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