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Correcting field data

Restraints due to artifacts may, by chance, be completely consistent with the correct structure of the molecule. However, the majority of incorrect restraints will be inconsistent with the correct structural data (i.e., the correct restraints and information from the force field). Inconsistencies in the data produce distortions in the structure and violations in some restraints. Structural consistency is often taken as the final criterion to identify problematic restraints. It is, for example, the central idea in the bound-smoothing part of distance geometry algorithms, and it is intimately related to the way distance data are usually specified The error bounds are set wide enough that all data are geometrically consistent. [Pg.264]

Compute the dip angle of the magnetic field vector after correction for the drill collar field, it should check with the local magnetic field data. What do you conclude if it does not ... [Pg.919]

The two deliverables from the field residue trial will be the samples, properly labeled, packed and shipped, and the field notebook, filled out correctly and completely. It is important that the Principal Investigator realize that all notations and calculations are made directly in the field notebook, not transcribed, and in ink. Multiple events, such as calibrations, applications, and harvests, must be documented on sequential individual forms. The field data in the notebook are not sent to the EPA as part of a submission package. These data must conform... [Pg.208]

There are a number of ways to display and correct field and analytical data, and a few will be discussed here. However, the omission of any technique for handling data does not imply that the techniques may be faulty. [Pg.1024]

Dennis, R. L., J. N. McHenry, W. R. Barchet, F. S. Binkowski, and D. W. Byun, Correcting RADM s Sulfate Underprediction Discovery and Correction of Model Errors and Testing the Corrections through Comparisons against Field Data, Atmos. Environ., 27A, 975-997 (1993). [Pg.340]

There is a paucity of reliable, consistent data for hydrate elastic properties. Since these properties depend on crystal structures, many of them can be estimated reliably. However, since 1998, there have been significant efforts to perform accurate measurements of these properties in order to help facilitate correct interpretation of sonic or seismic velocity field data obtained on hydrates in the natural environments. [Pg.96]

The Smith et al. correlation (20, Fig. 6.11). This is another early entrainment flooding prediction method that has sometimes been recommended (11). Compared to Fair s correlation, the Smith et al. correlation is claimed (20) to be less conservative. It was derived from a small base of field data for sieve, valve, and bubble-cap trays. Similar to Fair s correlation, Smith s correlation uses CSB versus a flow parameter plot, but here the dependence of CSB on the flow parameter is weaker, and there is no surface tension correction factor. CSB and flood 316 both based on the net area AN, and are evaluated from Fig. 6.11 and Eq. (6,9), respectively. The height over the weir, how, is obtained from Eq, (6.49). [Pg.279]

Table 1 The measured value and corrections for data point 6. The energy was 100 keV, the field separation 5.06(5) cm and the full width at half maximum 40.1 MHz. All the entries are in MHz. Table 1 The measured value and corrections for data point 6. The energy was 100 keV, the field separation 5.06(5) cm and the full width at half maximum 40.1 MHz. All the entries are in MHz.
Driver and partly aerosol feedbacks, for ACTMs or for NWP (data exchange with a limited time period) off-line or on-line access coupling, with or without the following iterations with corrected fields)... [Pg.9]

Fig. 1. Magnetization versus temperature for C6o(TDAE),f measured upon cooling and subsequent warming in an applied field of — 1 Oe (O) and 100 Oe ( ). The 1-Oe data were multiplied by 10 to give the same ordinate values as the lOO-Oe data. Note disappearance of curvature below 10 K at high field. Data were not corrected for the sample holder or for demagnetizing effects. Fig. 1. Magnetization versus temperature for C6o(TDAE),f measured upon cooling and subsequent warming in an applied field of — 1 Oe (O) and 100 Oe ( ). The 1-Oe data were multiplied by 10 to give the same ordinate values as the lOO-Oe data. Note disappearance of curvature below 10 K at high field. Data were not corrected for the sample holder or for demagnetizing effects.
Table 6. UV, CD, and corrected MCD data of purified apo-erythrocuprein. The employed magnetic field was 49.5 kG applied parallel to the light beam. The corrected MCD data are expressed in molar magnetic ellipticity values at 49.5 kG the values are corrected for natural CD (78)... Table 6. UV, CD, and corrected MCD data of purified apo-erythrocuprein. The employed magnetic field was 49.5 kG applied parallel to the light beam. The corrected MCD data are expressed in molar magnetic ellipticity values at 49.5 kG the values are corrected for natural CD (78)...
One of the most important aspects of using a fesf facility to obtain experimental data is having the ability to check and verify fhe accuracy of fhe dafa being collected. In a test facility with properly calibrated instrumentation mass and energy balance closures within a few percentages are frequently achieved. When field data is obtained from commercial fhermal oxidizers fhe quality of the data is often questionable. This is because there is seldom time to obtain steady-state conditions, means to verify fhe accuracy of the instrumentation, or even complete data to close a mass and energy balance around the process to see if the measured data appears to be correct. [Pg.693]

The attempt to correct experimental data to zero ionic strength is fundamental to the treatment, even though often this can be done only approximately. The model of non-conjugative substituent effects which is used is a combination of Lewis s model of the inductive effect as a through-bonds displacement of electrons, and the electrostatic model of the field effect as devised by Bjerrum in his treatment of the first and second ionization constants of aliphatic dicarboxylic acids in water. As Wepster acknowledges, these models have their limitations, but he claims that their combination has nevertheless led to a very successful treatment. [Pg.271]

The model for the present condition is simulated and compared with the field data measured by HMTC during typhoon Tim in July 1994. The model results and field data at station 22 and 8 are presented in Fig. 25.16. It shows the amplification factor as a function of the incident wave period. It is seen that the comparison is quite good with respect to resonant periods, resonant bandwidth, and peak amplification factors. The results clearly indicate that there exists a broadband of resonant response for wave periods between 100 and 160 s and the computer model results appear to have captured the resonant modes correctly. [Pg.714]


See other pages where Correcting field data is mentioned: [Pg.605]    [Pg.1024]    [Pg.342]    [Pg.318]    [Pg.241]    [Pg.524]    [Pg.334]    [Pg.208]    [Pg.838]    [Pg.269]    [Pg.65]    [Pg.363]    [Pg.284]    [Pg.3255]    [Pg.338]    [Pg.60]    [Pg.456]    [Pg.431]    [Pg.190]    [Pg.192]    [Pg.309]    [Pg.246]    [Pg.186]    [Pg.864]    [Pg.175]    [Pg.153]    [Pg.21]    [Pg.106]   
See also in sourсe #XX -- [ Pg.1024 ]




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