弱相关Hubbard模型的均匀磁化率

本文利用温度格林函数技术和线性响应理论,得到了弱相关Hubbard模型的均匀磁化率。在HF近似下,高温时得到的均匀磁化率X=C/T;在梯形近似下,X_1=C/(T-θ)。后一结果和铁磁或反铁磁物质在高温时的居里-外斯定律相一致。     

分子连接性指数与对饱和一元醇物理化学性质的预测

提出计算饱和一元醇物理化学性质P的定量公式,预测了含10个碳原子以内的饱和一元醇的原子化热ΔHa,气相生成热ΔHgi,摩尔折射Rm,蒸发热ΔHv,摩尔磁化率Xm,沸点B.P.(℃),保留体积logVg和分配系数logP等8项物理化学性质.     

拓扑指数Gm与饱和一元醇物理化学性质的相关性研究

提出一种新的拓扑指数Gm，建立计算饱和一元醇物理化学性质的定量公式，预测了含10个碳原子以内的饱和一元醇的原子化热△Ha，气相生成热△Hgi，摩尔折射Rm，蒸发热△Hv，摩尔磁化率Xm，沸点B．P．（℃）和分配系数logP等7项物理化学性质．     

谐振法手持式智能磁化率仪设计

文章基于谐振原理设计了一款手持式智能磁化率仪,推导了谐振原理法测量岩石磁化率计算公式,仿真探究谐振法测量岩石磁化率的影响因素,结合仿真结果与实际探测需要对仪器进行整体设计。基于LDC1614搭建外围电路,设计了4层螺旋线圈等距并联的电感传感器、信号提取程序和上位机操作界面,完成了磁化率仪样机制作。该仪器轻便易携（重量仅0.2 kg）、操作简单,测量结果与国外同类仪器比较误差低于5%,仪器精度可达10-7。仪器适合野外及实验室测量,具有实际工程利用价值。     

准一维基于分子亚铁磁体自旋系统磁化率性质研究

基于交替自旋Ising—Hamiltonian模型,用量子转移矩阵方法,研究了不同外场条件下准一维基于有机分子亚铁磁体磁化率的结构序参量．对磁化率一的研究表明：双自由基和单自由基的交替有机自旋链的亚铁磁自旋排列等效于有效自旋S=1／2的铁磁相互作用链,双自由基有机高分子对具有单一成分的有机基于分子亚磁体具有绝对优势．量子Monte Carlo方法和精确对角化方法的计算结果两者相符,且与某些实验结果定性相符．     

长江镇扬河段不同时期河漫滩沉积物磁化率及其环境污染指示意义

为探讨河漫滩沉积物磁化率对环境污染的指示,采用重力浅钻法采集了长江下游镇江—扬州河段3个100 cm的河漫滩沉积岩芯,对岩芯沉积物进行质量磁化率和微量元素的测定。研究发现:老河漫滩沉积柱SY7的磁化率在12.11×10~(-8)～30.60×10~(-8) m~3/kg之间,平均值为20.79×10~(-8) m~3/kg;现代河漫滩沉积柱SY5和Z2的磁化率明显较高,是老的江心洲河漫滩沉积物磁化率的5～6倍,SY5的平均值最高,为123.20×10~(-8) m~3/kg。通过对研究区河漫滩沉积物重金属元素污染与长江流域水系沉积物背景值的对比研究发现,Cu、Ni、Cr的污染比较严重,新生成河漫滩明显比老河漫滩污染严重。简便、快速测定的磁化率分析可以作为河漫滩沉积物重金属污染诊断的重要手段之一。     

饱和一元醇物理化学性质的定量探讨

拓扑指数ｘｚ、路径数ｐ１和ｓ１、ｓ２是表征饱和一元醇分子大小、支化度、形状和羟基位置等结构特征的重要参量．本文提出计算饱和一元醇物理化学性质Ｐ的定量公式为：Ｐ＝ａ０＋ａ１ｐ１＋ａ２ｘ２／３ｚ＋ａ３ｓ１＋ａ４ｓ２式中ａ０、ａ１、ａ２、ａ３和ａ４为系数,对于某一物理化学性质为一定值．本文预测了含１０个碳原子以内的饱和一元醇的原子化热ΔＨａ、气相生成热ΔＨｇｔ、摩尔折射Ｒｍ、蒸发热ΔＨｖ、摩尔磁化率ＸＭ、液体密度Ｄ２０４、沸点Ｂ．Ｐ．、保留体积ｌｏｇＶｇ和分配系数ｌｏｇＰ等９项物理化学性质．     

变电子原子的抗磁性磁化率与康普顿线的形状

在本文中应用了葛林(Green),姆尔达(Mulder),莱维士(Lewis)及武尔(Woll)四人于最近建立的变分波函数来计算双电子原子的抗磁性磁化率、动量分布、及康普顿线的形状.计算结果比前人用简单变分波函数计算的结果都好,特别是对氦原子的抗磁性磁化率、计算的结果为-1.85×10~(-6),与实验值-1.88×10~(-6)很接近.     

磁化率测定实验的误差分析和实验改进

结合磁化率测定实验教学中存在的问题,在误差分析的基础上,提出了实验改进方法。改进后实验结果较好,可以满足物理化学实验的教学要求。     

许昌市清潩河表层沉积物磁化率特征及其环境意义

磁学参数作为环境污染的一项重要指标,在现代环境污染研究中发挥着重要作用.通过对许昌市清潩河表层沉积物磁化率进行测定,结果显示:在清潩河北段磁化率均值为36.8×10-8m3·kg~(-1),中段均值为29.8×10-8m3·kg~(-1),南段均值为44×10-8m3·kg~(-1).南段磁化率最高,北段次之,中段最低.受到污染严重的区域磁化率值较高,污染轻的区域磁化率值较低,磁化率对环境污染具有指示性.城市河流表层沉积物磁化率的测定,可以为城市河流污染监测、城市污染空间判断提供一种便捷手段.     

弱磁性材料磁化率测量技术的研究

弱磁性材料磁化率的数值很小,精确测量非常困难。在磁极头设计、励磁电路及计算机在测量中的应用等各方面进行研究,对传统的法拉第磁天平法加以改进,大大提高测量精度。     

Test of magnetic susceptibility and grain-size age models of loess

Ages of the stratigraphic boundary MIS1/2 and MIS3/4 of the Yuanbu loess section in Linxia are used as the basis of the nodal control age. The age of MIS1/2 and MIS3/4 are obtained from the latest international research result—the climatic events recorded in the stalagmite in the Hulu Cave in Nanjing, that MIS1/2 is 11.5 kaB.P. and MIS3/4 is 59.8 kaB.P.. The ages of the two climatic events contain three nodal age control models (Model 1: 0 kaB.P.—59.8 kaB.P.; Model 2: 0 kaB.P.—11.5 kaB.P. and 11.5 kaB.P.—59.8 kaB.P.; Model 3: 11.5 kaB.P.—59.8 kaB.P.), which are used as the nodal control age separately. The deposition times of various stratigraphic horizons are calculated by using the magnetic susceptibility age model and grain-size age model, and then compared with each other. In addition, the AMS14C age, OSL age and the ages of YD and H events are compared with the ages of the corresponding horizons calculated by the three models of nodal control ages. From the analyses of lithologic characters and climatic stages it has been found that both the magnetic susceptibility age model and the grain-size age model have some defects. Because the accurate control ages are selected as the nodal points of the glacial period or interglacial period, the stratigraphic deposition times determined by the high resolution of magnetic susceptibility age model and grain-size age model approximate to the actual ages. As for the relative accuracy of the two age models, the magnetic susceptibility age model is more accurate than the grain-size age model.     

Test of magnetic susceptibility and grain-size age models of loess

Ages of the stratigraphic boundary MIS1/2 and MIS3/4 of the Yuanbu loess section in Linxia are used as the basis of the nodal control age. The age of MIS1/2 and MIS3/4 are obtained from the latest international research result—the climatic events recorded in the stalagmite in the Hulu Cave in Nanjing, that MIS1/2 is 11.5 kaB.P. and MIS3/4 is 59.8 kaB.P.. The ages of the two climatic events contain three nodal age control models (Model 1: 0 kaB.P.—59.8 kaB.P.; Model 2: 0 kaB.P.—11.5 kaB.P. and 11.5 kaB.P.—59.8 kaB.P.; Model 3: 11.5 kaB.P.—59.8 kaB.P.), which are used as the nodal control age separately. The deposition times of various stratigraphic horizons are calculated by using the magnetic susceptibility age model and grain-size age model, and then compared with each other. In addition, the AMS14C age, OSL age and the ages of YD and H events are compared with the ages of the corresponding horizons calculated by the three models of nodal control ages. From the analyses of lithologic characters and climatic stages it has been found that both the magnetic susceptibility age model and the grain-size age model have some defects. Because the accurate control ages are selected as the nodal points of the glacial period or interglacial period, the stratigraphic deposition times determined by the high resolution of magnetic susceptibility age model and grain-size age model approximate to the actual ages. As for the relative accuracy of the two age models, the magnetic susceptibility age model is more accurate than the grain-size age model.     

低磁化率锆合金的研究进展

金属植入物在磁共振成像（magnetic resonance imaging,MRI）诊断中常产生较大的伪影,严重降低MRI图像的质量,进而影响病理诊断分析。降低金属植入物的磁化率是降低MRI伪影的有效途径。医用锆合金以其优良的生物相容性,优越的综合力学性能和较低的磁化率成为近年来的研究热点。回顾了锆合金的发展历史,分析了相组成和合金元素对锆合金磁化率的影响,详细介绍了Zr-Nb合金、Zr-Mo合金、Zr-Ru合金等低磁化率锆合金的研究现状,展望了锆合金作为医疗器械候选材料的发展前景。     

磁化率对大地电磁响应影响异常规律研究

为探究地下介质的磁化率性质对大地电磁观测数据的影响,本文在常规大地电磁的正演过程中引入磁化率这一物性参数,利用有限单元法实现了同时考虑电阻率和磁化率的二维大地电磁正演算法。通过建立不同模型进行正演计算,详细分析了磁性体的磁化率值、背景电阻率值、埋深等参数对大地电磁正演结果的影响,总结出两种判定地下磁性体是否会对大地电磁数据产生影响的方法：若已知地下磁性体的规模,可根据磁性体的埋深与边长的比值系数判定;若未知地下磁性体的规模,可根据地磁测资料磁异常的幅值变化判定。     

基于分子磁化率性质的电磁流量计误差

采用电磁学和结构化学原理剖析了用于石油"三采"聚合物液流的电磁流量计计量误差原因,从分子磁化性质的角度解释了由于不同溶液的磁化率性质不同所造成的电磁流量计计量误差的现象.结合公式和实验说明了不同溶液在电磁流量计励磁磁场的作用下发生磁化而导致电磁流量计原励磁磁场强度发生变化的误差机理.通过论证和实验证明,不同磁化率性质的溶液在通过励磁磁场时将会不同程度的改变原磁场强度,因此不同溶液在同一电磁流量计磁场的作用下其感应电动势的响应值是不同的.     

Optimal procedure for fitting the magnetic susceptibility vs J couplings

To provide efficiency in calculating the energy-levels of paramagnetic spin clusters with high nuclear -ity, a fitting program of irreducible tensor operator is developed for the calculation of / couplings. An optimal data-access process is given, which greatly enhances the computational aspects of such modeling. Upon the program's application, the coupling constants of the moderate-sized clusters are fitted automatically by the least-squares calculations in PCs.     

伊犁盆地晚更新世黄土—古土壤磁化率特征

新疆伊犁河谷海拔高度不同的两个晚更新世黄土剖面磁化率特征存在显著差异:位于海拔1400 m处的库尔德能布拉黄土剖面,其磁化率特征与黄土高原黄土相同,而海拔850 m处塔勒德黄土剖面的磁化率特征则与黄土高原相反.对两个剖面黄土-古土壤磁化率特征等分析研究认为,造成两个剖面S1古土壤磁化率差异的主要原因是末次间冰期土壤发育时期前者降水量大于后者.