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Magnetostriction varieties and stress relief caused by pulsed magnetic field
Zhipeng CAI, Xinjie DUAN, Jian LIN, Haiyan ZHAO
《机械工程前沿(英文)》 2011年 第6卷 第3期 页码 354-358 doi: 10.1007/s11465-011-0123-4
Magnetostriction is investigated to evaluate the stress relief caused by pulsed magnetic field treatment, because this physical property is closely associated with residual stress. Magnetostriction of different stressed samples is measured in this paper. The stress variations caused by pulsed magnetic treatment are also compared. It is found that magnetostriction variations are closely associated with stress changes. Thermodynamic potential is used to find the relationship between them. Based on several assumptions, we find that the product of magnetostriction amplitude and stress magnitude is nearly a constant during magnetic field treatment, which is valuable for stress relief evaluation and optimizing processing parameters. This conclusion is testified by stress measurements, and the calculated values are in accordance with the experiment results.
关键词: magnetostriction pulsed magnetic field treatment stress relief
Hai-Bang LY; Huong-Lan Thi VU; Lanh Si HO; Binh Thai PHAM
《结构与土木工程前沿(英文)》 2022年 第16卷 第2期 页码 224-238 doi: 10.1007/s11709-022-0812-6
关键词: soil consolidation coefficient machine learning random forest Relief
CHE Pengchao, HE Yaning, WANG Xiaogong
《化学科学与工程前沿(英文)》 2007年 第1卷 第4期 页码 360-364 doi: 10.1007/s11705-007-0065-x
关键词: inscription 4-cyanoaniline orientation peripheral photoswitch
利用机载激光雷达和近地表地球物理方法空间识别复杂低幅度第四纪硅质碎屑岩层——以美国得克萨斯滨海平原为例 Article
Jeffrey G. Paine,Edward W. Collins,Lucie Costard
《工程(英文)》 2018年 第4卷 第5期 页码 676-684 doi: 10.1016/j.eng.2018.09.005
保存在全球滨海平原上的沉积单元控制着浅地层岩性分布,这对基础设施的设计和建设至关重要,同时也是许多第四纪冰期—间冰期循环中发生大规模气候变化的重要信息库。我们对这些沉积单元的横纵向岩性、地层复杂性及其对气候和海平面变化的响应知之甚少,因此很难预测岩性分布,以及将发展历史、未来气候和海平面变化置于同一自然地质环境中。传统上在低幅度滨海平原上描绘的第四纪硅质碎屑沉积单元建立在航拍图和低分辨率地形图的基础上。低幅度和低曝光率影响了观测的准确性和精确性。高分辨率机载激光雷达探测、地表地球物理勘探和地球物理测井正被用于识别得克萨斯州滨海平原上第四纪地层岩性单元的精确横纵向边界。地表和井中电导率测量能从泥质泛滥平原、三角洲平原和河道沉积中区分出砂质障壁岛、河流和三角洲河道沉积物。井中电导率和自然伽马测井记录同样可以区分地下不同的岩性单元,并识别出可能在不同冰期- 间冰期阶段分离的沉积单元的侵蚀不整合面。从机载激光雷达探测获得的高分辨率数字高程模型揭示了以前不为人知的地形细节,有助于识别地表特征,如砂质通道、富含黏土的河间沉积和更新世障壁岛上的堆积特征。在低幅度滨海平原环境中识别岩性和地层分布的最佳方法是:①首先使用激光雷达探测生成详细的高程模型;②基于激光雷达数据和航拍图的初步定位,选择性进行地表采样和地球物理探测;③在激光雷达和地表探测完成后,选择关键位置进行钻孔取样、测井和分析。
标题 作者 时间 类型 操作
Magnetostriction varieties and stress relief caused by pulsed magnetic field
Zhipeng CAI, Xinjie DUAN, Jian LIN, Haiyan ZHAO
期刊论文
Dimensionality reduction and prediction of soil consolidation coefficient using random forest coupling with Relief
Hai-Bang LY; Huong-Lan Thi VU; Lanh Si HO; Binh Thai PHAM
期刊论文
Photoinduced dichroism and surface-relief-gratings of hyperbranched azo polymers synthesized by azo-coupling
CHE Pengchao, HE Yaning, WANG Xiaogong
期刊论文