In this paper,a probe method for nonlinear programming wiht equality and inequality is given. Its iterative directions at an arbitrary point x can be obtained through solving a liear system. The terminate conditions a...In this paper,a probe method for nonlinear programming wiht equality and inequality is given. Its iterative directions at an arbitrary point x can be obtained through solving a liear system. The terminate conditions and choices of the parameters are given. The global convergence of the method is proved. Further more,some well known gradient projection type algorithms [1-15] and new gradient projection type algorithms from the linear system are given in this paper.展开更多
The authors presented a new measuring method of the soil thermal conductivity,the probe method,which is designed and made based on the theory of line heat source. This method is used to measure thermal conductivity of...The authors presented a new measuring method of the soil thermal conductivity,the probe method,which is designed and made based on the theory of line heat source. This method is used to measure thermal conductivity of coarse sand,fine sand and silty clay in different water contents. The results that measured by the probe method are well consistent with those of QTM-D_2. The soil thermal conductivity increases in different levels with the increase of the water content. Compared the soil thermal conductivity measured by the probe method in laboratory with in-situ experiment,it shows that the measuring gap gradually increases with the increase of the depth. The reason is that the in-situ measuring thermal conductivity can reflect the actual situation of the soil mass.展开更多
A combined method for the fast 3-D finite element modeling of defect responses in nondestructive testing of electromagnetics is presented. The method consists of three numerical techniques: zoom-in technique, differen...A combined method for the fast 3-D finite element modeling of defect responses in nondestructive testing of electromagnetics is presented. The method consists of three numerical techniques: zoom-in technique, difference field technique and iterative solution technique. Utilizing the zoom-in technique, the computational zone focuses on a relatively small domain around the defect. Employing the difference field technique, the axisymmetrical field solution corresponding to the case with no defect can be used to simplify the mesh generation and obtain the modeling results quickly. Using the iterative solution technique, the matrix equation system in the 3-D finite element modeling of nondestructive probe signals can easily be solved. The sample calculation shows that the presented method is highly effective and can consequently save significant computer resources.展开更多
为解决原子力显微镜(Atomic Force Microscope,AFM)系统更换探针后光路调整复杂耗时、精度不足的问题,本文首次提出通过精密控制探针与探针夹装配位置来实现更换的探针相对AFM系统原光路位置的一致,进而实现免去AFM系统换针后调整光路...为解决原子力显微镜(Atomic Force Microscope,AFM)系统更换探针后光路调整复杂耗时、精度不足的问题,本文首次提出通过精密控制探针与探针夹装配位置来实现更换的探针相对AFM系统原光路位置的一致,进而实现免去AFM系统换针后调整光路步骤。该系统的光路一致性组件采用光束偏转法对探针位置与偏转进行放大与监测,并使用高精度位移与角度调节平台进行探针相对于探针夹的方位调整。通过实物搭建对探针一致性效果进行了验证,并对紫外光(Ultraviolet,UV)胶水固化过程导致探针位置偏移影响;探针不同偏移量时产生的探测器噪音对AFM系统成像质量影响进行了系统分析。实验结果表明:经由该系统装配的探针平均位置精度接近1.1μm;并且在AFM系统中更换一致性探针仅需8 s。该系统实现了高精度且质量稳定的探针一致性装配,极大地简化了AFM系统重新校准光路的操作步骤,其与自动换针装置配合可有效提升工业计量型AFM的操作与测量性能。展开更多
实现土壤失水过程的原位监测,对红壤区水土资源管理、自然灾害预警及防灾减灾具有重要意义。热脉冲法是目前土壤水热特性原位测量的常用方法,但红壤土失水时极易产生裂缝,单探针热脉冲法能否准确测定失水过程目前尚不清楚。通过室内模...实现土壤失水过程的原位监测,对红壤区水土资源管理、自然灾害预警及防灾减灾具有重要意义。热脉冲法是目前土壤水热特性原位测量的常用方法,但红壤土失水时极易产生裂缝,单探针热脉冲法能否准确测定失水过程目前尚不清楚。通过室内模拟土壤从饱和到干燥的连续失水过程,用时域反射法(TDR)作为标准对照,验证热脉冲方法测定土壤失水过程的准确性,并评估土壤裂缝产生后对单探针热脉冲法的影响。结果表明:随着土壤失水,土壤热导率K值由1.8 W/(m·K)减小到1.1 W/(m·K),热扩散率α值由1.0×10^(-8)m^(2)/s增加到3.0×10-8 m 2/s,比热容C值由1.8×108 J/(kg·K)减小到0.4×10^(8)J/(kg·K);接触热导率H值随着土壤失水具有台阶状变化特征,与土壤含水率变化速率的转折相吻合;与TDR测定结果相比,MAE和RMSE值分别为1.66和1.94 cm 3/cm^(3),R^(2)值为0.96;单探针热脉冲法能提供可靠的红壤土失水过程测定结果,且H值的变化能指征土壤裂隙的产生,可为土壤干湿循环过程、边坡和堤坝稳定性的动态监测提供技术和理论支撑。展开更多
文摘In this paper,a probe method for nonlinear programming wiht equality and inequality is given. Its iterative directions at an arbitrary point x can be obtained through solving a liear system. The terminate conditions and choices of the parameters are given. The global convergence of the method is proved. Further more,some well known gradient projection type algorithms [1-15] and new gradient projection type algorithms from the linear system are given in this paper.
基金Supported by Project of National Natural Science Foundation of China(No.41372239)
文摘The authors presented a new measuring method of the soil thermal conductivity,the probe method,which is designed and made based on the theory of line heat source. This method is used to measure thermal conductivity of coarse sand,fine sand and silty clay in different water contents. The results that measured by the probe method are well consistent with those of QTM-D_2. The soil thermal conductivity increases in different levels with the increase of the water content. Compared the soil thermal conductivity measured by the probe method in laboratory with in-situ experiment,it shows that the measuring gap gradually increases with the increase of the depth. The reason is that the in-situ measuring thermal conductivity can reflect the actual situation of the soil mass.
文摘A combined method for the fast 3-D finite element modeling of defect responses in nondestructive testing of electromagnetics is presented. The method consists of three numerical techniques: zoom-in technique, difference field technique and iterative solution technique. Utilizing the zoom-in technique, the computational zone focuses on a relatively small domain around the defect. Employing the difference field technique, the axisymmetrical field solution corresponding to the case with no defect can be used to simplify the mesh generation and obtain the modeling results quickly. Using the iterative solution technique, the matrix equation system in the 3-D finite element modeling of nondestructive probe signals can easily be solved. The sample calculation shows that the presented method is highly effective and can consequently save significant computer resources.
文摘为解决原子力显微镜(Atomic Force Microscope,AFM)系统更换探针后光路调整复杂耗时、精度不足的问题,本文首次提出通过精密控制探针与探针夹装配位置来实现更换的探针相对AFM系统原光路位置的一致,进而实现免去AFM系统换针后调整光路步骤。该系统的光路一致性组件采用光束偏转法对探针位置与偏转进行放大与监测,并使用高精度位移与角度调节平台进行探针相对于探针夹的方位调整。通过实物搭建对探针一致性效果进行了验证,并对紫外光(Ultraviolet,UV)胶水固化过程导致探针位置偏移影响;探针不同偏移量时产生的探测器噪音对AFM系统成像质量影响进行了系统分析。实验结果表明:经由该系统装配的探针平均位置精度接近1.1μm;并且在AFM系统中更换一致性探针仅需8 s。该系统实现了高精度且质量稳定的探针一致性装配,极大地简化了AFM系统重新校准光路的操作步骤,其与自动换针装置配合可有效提升工业计量型AFM的操作与测量性能。
文摘实现土壤失水过程的原位监测,对红壤区水土资源管理、自然灾害预警及防灾减灾具有重要意义。热脉冲法是目前土壤水热特性原位测量的常用方法,但红壤土失水时极易产生裂缝,单探针热脉冲法能否准确测定失水过程目前尚不清楚。通过室内模拟土壤从饱和到干燥的连续失水过程,用时域反射法(TDR)作为标准对照,验证热脉冲方法测定土壤失水过程的准确性,并评估土壤裂缝产生后对单探针热脉冲法的影响。结果表明:随着土壤失水,土壤热导率K值由1.8 W/(m·K)减小到1.1 W/(m·K),热扩散率α值由1.0×10^(-8)m^(2)/s增加到3.0×10-8 m 2/s,比热容C值由1.8×108 J/(kg·K)减小到0.4×10^(8)J/(kg·K);接触热导率H值随着土壤失水具有台阶状变化特征,与土壤含水率变化速率的转折相吻合;与TDR测定结果相比,MAE和RMSE值分别为1.66和1.94 cm 3/cm^(3),R^(2)值为0.96;单探针热脉冲法能提供可靠的红壤土失水过程测定结果,且H值的变化能指征土壤裂隙的产生,可为土壤干湿循环过程、边坡和堤坝稳定性的动态监测提供技术和理论支撑。
