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There is a growing attention to the bio and renewable energies due to fast depletion of fossil fuels as well as the global warming problem. Here, we developed a modeling and simulation method by means of artificial intelligence (AI) for prediction of the bioenergy production from vegetable bean oil. AI methods are well known for prediction of complex and nonlinear process. Three distinct Adaptive Boosted models including Huber regression, LASSO, and Support Vector Regression (SVR) as well as artificial neural network (ANN) were applied in this study to predict actual yield of Fatty acid methyl esters (FAME) production. All boosted utilizing the Adaptive boosting algorithm. The important influencing parameters on the biodiesel production such as the catalyst loading (CAO/Ag, wt%) and methanol to oil (Soybean oil) molar ratio were selected as the input variables of models while the yield of FAME production was selected as output. Model hyper-parameters were tuned to maintain generality while improving prediction accuracy. The models were evaluated using three distinct metrics Mean Absolute Error (MAE), Root Mean Square Error (RMSE), and R2. Error rates of 8.16780E-01, 4.43895E-01, 2.06692E + 00, and 3.92713 E-01 were obtained with the MAE metric for boosted Huber, SVR, LASSO and ANN models. On the other hand, the RMSE error of these models were about 1.092E-02, 1.015E-02, 2.669E-02, and 1.01174E-02, respectively. Finally, the R-square score were calculated for boosted Huber, boosted SVR, and boosted LASSO as 0.976, 0.990, 0.872, and 0.99702, respectively. Therefore, it can be concluded that although the boosted SVR and ANN models were better models for prediction of process efficiency in terms of error, but all algorithms had high accuracy. The optimum yield of 83.77% and 81.60% for biodiesel production were observed at optimum operating values from boosted SVR and ANN models, respectively.  相似文献   
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We consider a stochastic search model with resetting for an unknown stationary target aR with known distribution μ. The searcher begins at the origin and performs Brownian motion with diffusion constant D. The searcher is also armed with an exponential clock with spatially dependent rate r=r(), so that if it has failed to locate the target by the time the clock rings, then its position is reset to the origin and it continues its search anew from there. Denote the position of the searcher at time t by X(t). Let E0(r) denote expectations for the process X(). The search ends at time Ta=inf{t0:X(t)=a}. The expected time of the search is then R(E0(r)Ta)μ(da). Ideally, one would like to minimize this over all resetting rates r. We obtain quantitative growth rates for E0(r)Ta as a function of a in terms of the asymptotic behavior of the rate function r, and also a rather precise dichotomy on the asymptotic behavior of the resetting function r to determine whether E0(r)Ta is finite or infinite. We show generically that if r(x) is of the order |x|2l, with l>1, then logE0(r)Ta is of the order |a|l+1; in particular, the smaller the asymptotic size of r, the smaller the asymptotic growth rate of E0(r)Ta. The asymptotic growth rate of E0(r)Ta continues to decrease when r(x)Dλx2 with λ>1; now the growth rate of E0(r)Ta is more or less of the order |a|1+1+8λ2. Note that this exponent increases to when λ increases to and decreases to 2 when λ decreases to 1. However, if λ=1, then E0(r)Ta=, for a0. Our results suggest that for many distributions μ supported on all of R, a near optimal (or optimal) choice of resetting function r in order to minimize Rd(E0(r)Ta)μ(da) will be one which decays quadratically as Dλx2 for some λ>1. We also give explicit, albeit rather complicated, variational formulas for infr0Rd(E0(r)Ta)μ(da). For distributions μ with compact support, one should set r= off of the support. We also discuss this case.  相似文献   
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《Physics letters. A》2020,384(19):126411
New features of noise-induced climate variability are revealed on the basis of the three-dimensional model derived by Saltzman and Maasch. It is shown that the climate system can be highly noise excitable and it possesses the large-amplitude fluctuations even in those regions where its akin deterministic model does not contain any self-sustained oscillations. Intermittency in small- and large amplitude climate fluctuations between different basins of attraction of a limit cycle and stable equilibria substantially influencing the climate state (from warm to cold and vice versa) are found at various noise intensities. Suddenly occurring jumps between the basins of attraction of two stable equilibria corresponding to the warm and cold climate states are statistically confirmed under a certain diapason of noise intensities. The climate system undergoes transitions between its equilibria in the presence of noise in its prognostic variables. In addition, such transitions become more likely with increasing the noise intensity.  相似文献   
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