Kernal factor analysis （KFA） with vafimax was proposed by using Mercer kernel function which can map the data in the original space to a high-dimensional feature space, and was compared with the kernel principle com...Kernal factor analysis （KFA） with vafimax was proposed by using Mercer kernel function which can map the data in the original space to a high-dimensional feature space, and was compared with the kernel principle component analysis （KPCA）. The results show that the best error rate in handwritten digit recognition by kernel factor analysis with vadmax （4.2%） was superior to KPCA （4.4%）. The KFA with varimax could more accurately image handwritten digit recognition.展开更多
环境敏感因子是沉积环境演化研究中的重要参数,其提取方法有多种,不同方法在海湾内应用成果相对较少。文章根据山东半岛威海湾WH-05岩心(钻探深度18.2 m)高分辨率(2 cm)粒度分析结果,采用基本端元模拟算法(BasEMMA)、粒级—标准偏差法...环境敏感因子是沉积环境演化研究中的重要参数,其提取方法有多种,不同方法在海湾内应用成果相对较少。文章根据山东半岛威海湾WH-05岩心(钻探深度18.2 m)高分辨率(2 cm)粒度分析结果,采用基本端元模拟算法(BasEMMA)、粒级—标准偏差法和粒级旋转主成分分析法(V-PCA)提取了环境敏感因子,结合AMS14C数据,对不同方法提取的环境敏感因子进行了对比分析,探讨了其对季风强度变化的响应关系。结果表明:8.4 ka B.P.以来威海湾沉积物类型均为粉砂,粉砂含量为主、黏土含量次之、砂含量较少,以跳跃组分为主,悬浮组分次之。BasEMMA和粒级—标准偏差法提取的3个敏感粒级范围(2.6~11.0μm、31.3~63.4μm、256.9~500.0μm)总体一致,能较好地反映东亚季风长周期变化事件(8.4~6.5 ka B.P.东亚季风强度减弱;6.5 ka B.P.至今东亚季风强度增强);V-PCA提取的环境敏感因子,能较好地反映东亚季风短周期变化事件(如明清小冰期、西汉小冰期事件等)。以上三种方法提取的环境敏感因子指示了研究区气候变化,对研究区沉积环境具有较好的指示作用。展开更多
The Cretaceous Mamu Formation coal samples located within the Northern Anambra Basin were collected, analysed and interpreted using multivariate statistical approach to determine the major, trace and rare elements ass...The Cretaceous Mamu Formation coal samples located within the Northern Anambra Basin were collected, analysed and interpreted using multivariate statistical approach to determine the major, trace and rare elements association with a view to determine the source of the terrestrial rocks, palaeoweathering/climatic conditions and tectonic setting. The dominant oxides such as SiO2, A12O3, Fe2O3, TiO2 and CaO were identified in the coal to suggest terrigenous origin. The ratio of SiO2/Al2O3 of 4.8 suggests that the coal was formed from low land peat associated with freshwater continental marine or blackish water with low salinity as indicated by Sr/Ba and CaO + MgO/K2O + Na2。ratios. The major oxides also revealed stable condition of deposition, low degree of tectonic setting but constant subsidence in the basin. The condition of deposition was acidic in nature as indicated by TiO2/Zr plot. Based on the abundance of Zr, Zn, Ba, Ni, Co, Sr, V, and Y, moderate salinity, sub-oxic to oxic bottom water condition was prevalent and also indication of marine influence. Based on the ratios of La/Yb;La/Sm and Gd/Yb, LREE has higher enrichment than HREE. Humid climatic conditions were observed at the coal formation stage while weak laterization to kaolinization was also evidence.展开更多
This section uses the results of a survey to find out how consumers evaluate banking services in the State of Libya.The survey contained a large number of variables,most of which are correlated.This paper tries to exa...This section uses the results of a survey to find out how consumers evaluate banking services in the State of Libya.The survey contained a large number of variables,most of which are correlated.This paper tries to examine the relationships among the interrelated variables and represent them in terms of a few underlying factors.This is done through the use of the technique of Factor Analysis.This study represents an inquiry into consumers’evaluation of the banking system in Libya.A survey was conducted to collect information on a number of issues relating to the consumer’s views on various aspects of the structure and performance of commercial banks operating in the State of Libya.The survey results were subjected to multivariate statistical analysis.The technique of factor analysis was used to analyze the relationships among the interrelated variables affecting consumers’choice of a particular commercial bank.The principal component method,with varimax rotation,is utilized to reduce the large number of explanatory variables to a few underlying factors.展开更多
The regional characteristics of precipitation anomalies of total summer precipitation of June, July and August and individual monthly precipitation are analyzed by using the method of Varimax EOF and correlation analy...The regional characteristics of precipitation anomalies of total summer precipitation of June, July and August and individual monthly precipitation are analyzed by using the method of Varimax EOF and correlation analysis.The data set used is the precipitation of a 5°Lat.×5°Long.spatial uniform network over China in the period of 1959 to 1994. The analysis of total summer precipitation shows that the most significant regional characteristic is the existence of negative correlation in precipitation anomalies between the lower reaches of the Changjiang River and the Huaihe River Valley(the LRCH region)and the middle reaches of the Huanghe River Valley(the MRH region),and between the LRCH region and South China.The precipitation anomaly over the Sichuan Basin is negatively correlated with that over eastern part of Qinghai-Xizang Plateau and that over the LRCH region.The regional characteristics of summer precipitation anomalies in western China are that there exists negative correlation between the summer precipitation anomalies over the southern part of the central and eastern Qinghai-Xizang Plateau and that over its northern part.There also exists positive correlation between the southern part of the central and eastern Qinghai-Xizang Plateau and the eastern part of North China and the southern part of Northeast China.The above spatial correlation modes have significant periods of about 3 years and ten years.The analysis of the monthly precipitation shows that in June there exists positive correlation among the precipitation anomalies over the LRCH region,the eastern part of North China and Northeast China.In July, the precipitations in the MRH region and the LRCH region are negatively correlated.The regional characteristic of precipitation anomalies in August is very similar to that of the total summer precipitation anomalies.展开更多
基金The National Defence Foundation of China (No.NEWL51435Qt220401)
文摘Kernal factor analysis （KFA） with vafimax was proposed by using Mercer kernel function which can map the data in the original space to a high-dimensional feature space, and was compared with the kernel principle component analysis （KPCA）. The results show that the best error rate in handwritten digit recognition by kernel factor analysis with vadmax （4.2%） was superior to KPCA （4.4%）. The KFA with varimax could more accurately image handwritten digit recognition.
文摘环境敏感因子是沉积环境演化研究中的重要参数,其提取方法有多种,不同方法在海湾内应用成果相对较少。文章根据山东半岛威海湾WH-05岩心(钻探深度18.2 m)高分辨率(2 cm)粒度分析结果,采用基本端元模拟算法(BasEMMA)、粒级—标准偏差法和粒级旋转主成分分析法(V-PCA)提取了环境敏感因子,结合AMS14C数据,对不同方法提取的环境敏感因子进行了对比分析,探讨了其对季风强度变化的响应关系。结果表明:8.4 ka B.P.以来威海湾沉积物类型均为粉砂,粉砂含量为主、黏土含量次之、砂含量较少,以跳跃组分为主,悬浮组分次之。BasEMMA和粒级—标准偏差法提取的3个敏感粒级范围(2.6~11.0μm、31.3~63.4μm、256.9~500.0μm)总体一致,能较好地反映东亚季风长周期变化事件(8.4~6.5 ka B.P.东亚季风强度减弱;6.5 ka B.P.至今东亚季风强度增强);V-PCA提取的环境敏感因子,能较好地反映东亚季风短周期变化事件(如明清小冰期、西汉小冰期事件等)。以上三种方法提取的环境敏感因子指示了研究区气候变化,对研究区沉积环境具有较好的指示作用。
文摘The Cretaceous Mamu Formation coal samples located within the Northern Anambra Basin were collected, analysed and interpreted using multivariate statistical approach to determine the major, trace and rare elements association with a view to determine the source of the terrestrial rocks, palaeoweathering/climatic conditions and tectonic setting. The dominant oxides such as SiO2, A12O3, Fe2O3, TiO2 and CaO were identified in the coal to suggest terrigenous origin. The ratio of SiO2/Al2O3 of 4.8 suggests that the coal was formed from low land peat associated with freshwater continental marine or blackish water with low salinity as indicated by Sr/Ba and CaO + MgO/K2O + Na2。ratios. The major oxides also revealed stable condition of deposition, low degree of tectonic setting but constant subsidence in the basin. The condition of deposition was acidic in nature as indicated by TiO2/Zr plot. Based on the abundance of Zr, Zn, Ba, Ni, Co, Sr, V, and Y, moderate salinity, sub-oxic to oxic bottom water condition was prevalent and also indication of marine influence. Based on the ratios of La/Yb;La/Sm and Gd/Yb, LREE has higher enrichment than HREE. Humid climatic conditions were observed at the coal formation stage while weak laterization to kaolinization was also evidence.
文摘This section uses the results of a survey to find out how consumers evaluate banking services in the State of Libya.The survey contained a large number of variables,most of which are correlated.This paper tries to examine the relationships among the interrelated variables and represent them in terms of a few underlying factors.This is done through the use of the technique of Factor Analysis.This study represents an inquiry into consumers’evaluation of the banking system in Libya.A survey was conducted to collect information on a number of issues relating to the consumer’s views on various aspects of the structure and performance of commercial banks operating in the State of Libya.The survey results were subjected to multivariate statistical analysis.The technique of factor analysis was used to analyze the relationships among the interrelated variables affecting consumers’choice of a particular commercial bank.The principal component method,with varimax rotation,is utilized to reduce the large number of explanatory variables to a few underlying factors.
基金The research is supported by the 96-908-04-03 grant of the Chinese State Commission of Sciences and Technology.
文摘The regional characteristics of precipitation anomalies of total summer precipitation of June, July and August and individual monthly precipitation are analyzed by using the method of Varimax EOF and correlation analysis.The data set used is the precipitation of a 5°Lat.×5°Long.spatial uniform network over China in the period of 1959 to 1994. The analysis of total summer precipitation shows that the most significant regional characteristic is the existence of negative correlation in precipitation anomalies between the lower reaches of the Changjiang River and the Huaihe River Valley(the LRCH region)and the middle reaches of the Huanghe River Valley(the MRH region),and between the LRCH region and South China.The precipitation anomaly over the Sichuan Basin is negatively correlated with that over eastern part of Qinghai-Xizang Plateau and that over the LRCH region.The regional characteristics of summer precipitation anomalies in western China are that there exists negative correlation between the summer precipitation anomalies over the southern part of the central and eastern Qinghai-Xizang Plateau and that over its northern part.There also exists positive correlation between the southern part of the central and eastern Qinghai-Xizang Plateau and the eastern part of North China and the southern part of Northeast China.The above spatial correlation modes have significant periods of about 3 years and ten years.The analysis of the monthly precipitation shows that in June there exists positive correlation among the precipitation anomalies over the LRCH region,the eastern part of North China and Northeast China.In July, the precipitations in the MRH region and the LRCH region are negatively correlated.The regional characteristic of precipitation anomalies in August is very similar to that of the total summer precipitation anomalies.
