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Forward Modeling Results

The distribution coefficients of the parent and daughter nuclides are important in U-series disequilibria. If the parent has a higher distribution coefficient than the daughter, its extraction from the matrix is retarded and the daughter/parent activity ratio in the melt can be greater than 1. Experiments have shown that Dy Dj for garnet peridotites but Du Dj for spinel peridotites at low pressures. Due to experimental difficulties, Dro and Dpa are not directly known but are inferred to be very small. Therefore, it is reasonable to assume Dj, Di and Du Dp for both garnet peridotites and spinel peridotites. [Pg.91]

which is consistent with previous assessment by McKenzie (1985) about the effect of melting rate and porosity on However, the sensitivity of the daughter/parent activity ratio to the variations of and M is different for the above three activity ratios. Both and Pa/ C/) are sensitive to the variations of [Pg.92]


The amplitude of the SPICE model result has about a 1-V offset missing from the result. This is due to the forward drop of the zener diode, which is not typically modeled in zener diode models. It is not difficult to model this parameter, but since the purpose was to show the zero offset result, it is not important here. [Pg.230]

The approximations that have been implemented in the optimised forward model (OFM) have been validated comparing the results with a specially developed line-by-line code developed at Oxford University [18] and based on GENLN2 [19]. This code was compared with several existing codes and was elected as our reference forward model (RFM). The main results of the RFM / OFM intercomparisons are ... [Pg.342]

The results obtained so far indicate that both forward model error, i.e. error due to imperfect modeling of the atmosphere, and convergence error, i.e. error due to the feet that the inversion procedure does not find the real minimum of the %2 function, are much smaller than the measurement error due to radiometric noise. [Pg.343]

Application of the elastic forward modeling operator to the initial model with the background Lame velocities results in nothing more than the incident elastic field in the background model, u (r, w). The difference between this incident field and the observed total field dx, gives us the scattered elastic field (with a minus sign) ... [Pg.524]

There are many studies that imply numerical methods for the forward modelling of galvanic corrosion problem. These techniques are based mainly on boundary value problems (B VP) formulations in order to obtain or verify results, such as finite element method (FEM), finite difference method (FDM) or boundary element method (BEM). These methods are successfully used and showed to be very accurate to solve BVPs. Some of them are also implemented in commercial software. [Pg.174]

With the feed-forward model, Eqs. (1-3), derived from the graphical representation in Fig. 17.1-1, the experimental data in Fig. 17.1-3, connected to the model by Eqs. (5-7), and the numerical techniques to estimate the parameters, we arrive at the modeling results displayed in Fig. 17.1-4. [Pg.1053]

This paper describes the basic principles of 3-D DDA and puts forward models to account for groundwater pressure and thermal loading in 3-D DDA. The water force and thermal loading submatrices are derived by minimizing the total potential energy and added to the global matrices. These extensions to 3-D DDA have been implemented into a 3-D DDA computer program, and numerical results from three test cases are reasonable. [Pg.476]

This book seeks to untangle the competing visions of a hydrogen economy, explain the trade-offs and obstacles along the path, and offer recommendations for a path forward. The results are based on a detailed simulation model developed at Sandia National Laboratories "The Hydrogen Futures Simulation Model (HjSim)."... [Pg.4]

Forward modelling is intended for the forecast of changes in underground water and the host medium properties and composition as a result of changing the environment. They forecast change in water properties and content of its individual components as a result of dissolution or formation of specific minerals, evaporation, mixing, rise or fall of temperature, etc. Solution of these problems is based on specific concepts groimd water formation processes, and the input data characterize their properties and composition. [Pg.548]

In this Thesis the work performed during my PhD programme has been presented. During the first year, my efforts focused in the Cardiff-UCL FIRI testbed data analysis and forward modelling, which resulted in the publication of the article Demonstration of spectral and spatial interferometry at THz frequencies (Grainger et al. 2012) in the journal Applied Optics. [Pg.148]

The variables (wavelengths) associated with the IR emission spectra were highly correlated. Principal components analysis (PCA), linear and nonlinear PLS showed that at least 86% of the total variance could be explained by the two primary latent dimensions. The forward and reverse modelling results showed that dimensional reduction with a linear model (PLS) produced better models than a nonlinear model (multilayer perceptron neural network trained with the back propagation algorithm) without dimensional reduction. [Pg.450]

The model analyzer service forward analysis results only to the result cache function. [Pg.1436]

Models can be categorized in various ways. Predictive models forecast the future behavior of a system, whereas conceptual models are used to understand relationships between system parts and processes. Deterministic models are constructed from mathematical functions that imambiguously relate cause and effect so that a particular set of input parameters produces a clearly related set of predicted results. Probabilistic models use statistical data to estimate the chance that an event or condition will occur. Forward models predict the future behavior of a system, whereas inverse (or reverse) models are used to extract fundamental data or mathematical relationships from past observations. [Pg.3]

One of the difficulties in fuel cell contamination modeling is estimating the unknown ORR parameters. In the case of no toluene being present, we needed to know the forward and backward reaction rates or their ratios for reaction (6.36) to reaction (6.38). To do this, we simulated experimental baseline data free of toluene contamination. The parameters used for the simulation are listed in Table 6.1, and the modeling results and experimental polarization curves are shown in Figure 6.3. [Pg.194]


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