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Sampling solids variables

Figure 1 Scbematic representation of the dynamics rf a response variable, c.g., concentration of rbizodeposited C, in the rhizosphere (das/ied line) and ihe measured concentrations in rhizosphere and nonrhizosphere samples solid lines). The vertical airow indicates the separation of rhizosphere and nonrhizosphere soil the effect of soil moisture is indicated by horizontal arrows. Figure 1 Scbematic representation of the dynamics rf a response variable, c.g., concentration of rbizodeposited C, in the rhizosphere (das/ied line) and ihe measured concentrations in rhizosphere and nonrhizosphere samples solid lines). The vertical airow indicates the separation of rhizosphere and nonrhizosphere soil the effect of soil moisture is indicated by horizontal arrows.
Therefore, the challenge in sampling solids for environmental analysis is to collect a relatively small portion of the sample that accurately represents the composition of the whole. This requires that sample increments be collected such that no piece, regardless of position (or size) relative to the sampling position and implement, is selectively collected or rejected. Optimization of solids sampling is a function of the many variable constituents of coal and is reflected in the methods by which an unbiased sample can be obtained, as is required by coal sampling (ASTM D197). [Pg.165]

Figure 12.29 Time-series plot of the y-residuals obtained from a PLS model developed using the process spectroscopy calibration data set (solid line), after removal of sample and variable outliers as discussed earlier. The measured y-values (dashed line) are also provided for reference. Figure 12.29 Time-series plot of the y-residuals obtained from a PLS model developed using the process spectroscopy calibration data set (solid line), after removal of sample and variable outliers as discussed earlier. The measured y-values (dashed line) are also provided for reference.
The time dependence of desorption remains a little-explored but potentially useful approach for mechanistic studies. Cotter (33) has monitored secondary ion kinetic energies in a laser desorption (LD) time-of-flight instrument. Laser pulses 40 ns wide were used to desorb K+ ions from solid KC1, and the ions were sampled at variable times after the laser pulse. Emission persists for several microseconds after excitation, and secondary ion kinetic energies were found to decrease when examined at longer times after excitation. This result supports a thermal model for... [Pg.14]

Generally, extraction is carried out at warm temperatures to increase the recovery of phenolic acids. The incubation temperature should not exceed the boiling point of the extraction solvent. Incubation time is variable from 1 hour to overnight and depends on the characteristics of the sample. During incubation, the extraction solution should be agitated frequently to increase contact between the solvent and sample. After extraction, the next step is to separate the extraction solvent from the sample solid residue. Either a centrifugation or filtration method can be applied in this step. The method selection usually depends on the... [Pg.76]

Discuss with those in your laboratory section the consequences of incorrect sample loading, variable sample size, and rates of heating and how these factors might lead you to obtain an incorrect value of the melting point for your solid sample. [Pg.122]

Perhaps the most common use for REELS is to monitor gas—solid reactions that produce surface films at a total coverage of less than a few monolayers. When Eq is a few hundred eV, the surface sensitivity of REELS is such that over 90% of the signal originates in the topmost monolayer of the sample. A particularly powerfiil application in this case involves the determination of whether a single phase of variable composition occurs on the top layer or whether islands occur that is, whether... [Pg.327]

To evaluate the fibrillation behavior of dispersed TLCP domains according to the - 5 relation discussed previously, different - 5 graphs were calculated by eliminating the thickness variable x. The result is reported in Fig. 18. It is obvious that all the points obtained are found to be relatively close to the critical curve by Taylor. The Taylor-limit is also shown in the figure with a solid curve. One finds that all the values calculated on sample 1 are completely above the limit, while all those determined on sample 4 are completely below the limit. The other two samples, 2 and 3, have the We - 5 relation just over the limit. [Pg.695]

Discussion. The turbidity of a dilute barium sulphate suspension is difficult to reproduce it is therefore essential to adhere rigidly to the experimental procedure detailed below. The velocity of the precipitation, as well as the concentration of the reactants, must be controlled by adding (after all the other components are present) pure solid barium chloride of definite grain size. The rate of solution of the barium chloride controls the velocity of the reaction. Sodium chloride and hydrochloric acid are added before the precipitation in order to inhibit the growth of microcrystals of barium sulphate the optimum pH is maintained and minimises the effect of variable amounts of other electrolytes present in the sample upon the size of the suspended barium sulphate particles. A glycerol-ethanol solution helps to stabilise the turbidity. The reaction vessel is shaken gently in order to obtain a uniform particle size each vessel should be shaken at the same rate and the same number of times. The unknown must be treated exactly like the standard solution. The interval between the time of precipitation and measurement must be kept constant. [Pg.729]

Fig. 3.7.1 Schematic of the DDIF effect in porous medium. The black areas are solid grains and the white areas are pore space. Diffusing spins in permeating fluid sample the locally variable magnetic field B(r) (solid contours sketched inside pore space) as it diffuses. Fig. 3.7.1 Schematic of the DDIF effect in porous medium. The black areas are solid grains and the white areas are pore space. Diffusing spins in permeating fluid sample the locally variable magnetic field B(r) (solid contours sketched inside pore space) as it diffuses.

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See also in sourсe #XX -- [ Pg.358 , Pg.359 , Pg.360 , Pg.361 , Pg.362 , Pg.363 ]




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