The Non-dominated Sorting Genetic Algorithm II (NSGA II) and Mult

The Non-dominated Sorting Genetic Algorithm II (NSGA II) and Multi-Objective Evolutionary Algorithm based on Decomposition (MOEA/D) have been applied to the multi-objective optimization problem, respectively. The Pareto solution set is obtained by a more effective and efficient manner of the two multi-objective optimization algorithms. A tradeoff optimal design point is selected from the Pareto solution set by means of a robust design based on Monte Carlo

simulations, and the optimal solution is further compared with the value of the 4 physical prototype test. The results show that the solution of the proposed multi-objective optimization method is in line with the experiment test. (C) 2014 Elsevier Ltd. All rights reserved.”
“Numerous studies have investigated the direct retrieval of soil properties, including soil texture, using remotely sensed images. However, few have considered how soil properties influence Metabolism inhibitor dynamic changes in remote Sapanisertib images or how soil processes affect the characteristics of the spectrum. This study investigated a new method for mapping regional

soil texture based on the hypothesis that the rate of change of land surface temperature is related to soil texture, given the assumption of similar starting soil moisture conditions. The study area was a typical flat area in the Yangtze-Huai River Plain, East China. We used the widely available land surface temperature product of MODIS as the main data source. We analyzed the relationships between the content of different particle soil size fractions at the soil surface and land surface day temperature, night temperature and diurnal temperature range (DTR) during three selected time periods. These periods occurred after rainfalls and between the previous harvest and the subsequent autumn sowing in 2004, 2007 and 2008. Then, linear regression models were developed between the land surface DTR and sand ( bigger than 0.05 mm),

clay ( smaller than 0.001 mm) and physical clay ( smaller than 0.01 mm) contents. The models for each day were used to estimate soil texture. The spatial distribution of soil texture from the studied area was mapped based on the model with the minimum RMSE. A validation dataset produced error estimates for the Fosbretabulin order predicted maps of sand, clay and physical clay, expressed as RMSE of 10.69%, 4.57%, and 12.99%, respectively. The absolute error of the predictions is largely influenced by variations in land cover. Additionally, the maps produced by the models illustrate the natural spatial continuity of soil texture. This study demonstrates the potential for digitally mapping regional soil texture variations in flat areas using readily available MODIS data.”
“5-Hydroxycytosine (5-OHC) is a stable oxidation product of cytosine associated with an increased frequency of C -> T transition mutations.

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