任意形状地质体数值积分法重磁场三维可视化反演   总被引：9，自引：1，他引：8  

杨宇山  刘天佑  李媛媛 《地质与勘探》2006,42(5):79-83

任意形状地质体数值积分法重磁场三维可视化反演,采用辛普生积分和梯形积分实现三度体磁场三重积分的近似计算,模型修改在剖面内完成,对x,y不同方向剖面逐条修改拟合,克服了模型难以修改和细化的困难.在Windows环境下,用Visual C语言、OpenGL函数实现了复杂立体模型的三维可视化反演.该方法适合于开采阶段的交互反演解释,将该方法运用于大冶铁矿,取得了很好的地质效果.  相似文献   

试论地震行业电算化会计信息系统的内部控制     

宁翠荣 《华北地震科学》2006,24(3):61-63

会计电算化和会计信息处理的网络化,给地震行业内部控制带来了影响。本文结合会计电算化和网络化业务应用的具体情况,对会计处理信息方式的改变给内部控制带来的影响和如何完善内部控制制度进行讨论,确保内部会计业务管理系统工作的真实性、可靠性和单位资金、财产的安全。  相似文献   

Volume and Surface Distribution Heterogeneity of Nano-pore in Coal Samples by CO2 and N2 Adsorption Experiments     

ZHANG Junjian  WEI Chongtao  LUO Jinhui  LU Guanwen  QUAN Fangkai  ZHENG Kai  PENG Yujie 《《地质学报》英文版》2020,94(5):1662-1675

In this paper, the heterogeneity of adsorption pores in middle and high rank coal samples were analyzed by using low temperature N2 and CO2 adsorption technology and fractal theory. The following results were achieved. 1) According to the results of volume and surface fractal dimension, meso-pores can be classified into Mep-1, Mep-2, and Mep-3, respectively. Micro-pore can be classified into Mip-1, Mip-2, and Mip-3, respectively. 2) Pore types play an important role in affecting the heterogeneity of meso-pores. The volume heterogeneity (VHY) of Mep-1 is simpler than that of Mep-2 and Mep-3 in type A samples. However, the VHY of Mep-1 becomes gradually larger than that of Mep-2 and Mep-3 from type A to type B and C. The VHY of open pore in the same diameter is higher than that of semi-open or closed pore. Meanwhile, the surface heterogeneity (SHY) of types A and B samples is significantly larger than that of type C, the SHY of semi-open or closed pores is more complicated than that of open pores. 3) Coal rank mainly affects the heterogeneity of micro-pores. The heterogeneity of type A is always smaller than that of type B and C. The VHY of Mip-1 is more complicated than that of Mip-2 and Mip-3 in the same samples, and the sensitivity of the VHY of Mip-1 and Mip-2 to the degree of coal rank is smaller than that of Mip-3. Meanwhile, the SHY of Mip-1 and Mip-2 is simpler than that of Mip-3 in the same sample, the SHY of micro-pores remains stable as the pore size decreases, and the affect of coalification level on SHY decreases with the decrease in pore diameter. Full-scale fractal characterization has enabled quantitative characterization of adsorption pore properties and provided useful information with regards to the similarity of pore features in different coal reservoirs.  相似文献   

加荷条件下软黏土的孔隙演化特征     

孙红  宋春雨  滕慕薇  葛修润 《岩土力学》2020,41(1):141-146

开展上海软黏土的宏微观三轴剪切试验,研究软黏土受荷状态下孔隙的演化特征。结果表明：局部变形在加荷初期就开始发生。随着荷载的增加,细碎团聚体增多,孔隙不断地扩展,生成大的贯通孔隙,孔隙定向排列明显,剪切带形成。微观结构参数与剪应力比呈非线性正相关关系,最大孔隙面积、孔隙比、孔隙各向异性率及分布分维数在受荷初期缓慢地增大,后期快速增大。应变为8%时,最大各向异性率达到0.68,最大孔隙比为1.96。剪切带附近的微观结构参数都大于带外值。在受荷过程中,土的微观结构发生劣化,软黏土变形过程分为损伤开始、损伤发展剪切带形成和土体破坏3阶段,微观结构的劣化与土的宏观力学特性紧密相联系。  相似文献   

粗粒料级配缩尺后最大干密度试验研究     

褚福永  朱俊高  翁厚洋  叶洋帆 《岩土力学》2020,41(5):1599-1604

对某级配粗粒料,采用剔除法、等量替代法、相似级配法和混合法等4种不同缩尺方法,依据规范要求进行缩尺。缩尺后替代级配料的最大颗粒粒径分别为20、40、60 mm。对各替代级配料采用振动台法进行了最大干密度试验,基于试验成果,结合分形理论,提出了一种将最大干密度与级配及细粒含量之间关系归一化的方法,并拟合了最大干密度与试验前级配的分形维数、小于5 mm颗粒的含量及最大粒径之间的关系,据此可推求出原型级配料的最大干密度,探讨了缩尺方法对替代料试验前后粒径分布曲线变化幅度的影响,总结出颗粒破碎分形维数与试验前级配的分形维数、小于5 mm颗粒含量及最大粒径之间的关系式,据此可推求出填筑后原型级配料的颗粒破碎分形维数。  相似文献   

基于尺寸效应的粗粒土单颗粒破碎试验及数值模拟     

孟敏强  王磊  蒋翔  汪成贵  刘汉龙  肖杨 《岩土力学》2020,41(9):2953-2962

在外荷载等因素作用下,粗粒土易发生颗粒破碎。对泥岩和砂岩颗粒进行了一系列的单颗粒破碎试验,基于尺寸效应和颗粒破碎分形模型,研究了单颗粒破碎强度、破碎能量及Weibull模量等与分形维数间的关系。利用PFC3D对单颗粒破碎过程进行分析,并与试验数据对比,验证了数值程序的可靠性;随后扩展到大颗粒粒径,分析了其单破碎强度及破碎能量。结果表明：在同类试验条件下,不同材料所得的分形维数是不同的;不同粒径砂岩的破碎程度均大于泥岩;单颗粒破碎强度具有明显的尺寸效应;单颗粒破碎强度与破碎能量均可通过分形维数与颗粒粒径预测得出;修正后的Weibull模量也可通过分形维数得出;数值模拟结果与试验结果及预测结果基本一致;大颗粒粒径单颗粒破碎强度模拟结果与预测结果基本一致,破碎能量稍有差异,需进一步试验验证。研究成果可为获取大粒径粗粒土的单颗粒强度与变形特性提供参考。  相似文献   

梯级水库作用下的长江流域水文设计成果修订研究     

徐长江  徐高洪  陈剑池 《水文》2018,38(6):89-95

长江流域水文成果复核选取了48个水文站点作为研究对象,考虑站点上游已建具有较强调节能力的大型水库调蓄影响,对径流、洪水进行还原分析计算以保证系列的一致性,并对径流、洪水设计成果的变化进行对比分析。径流成果分析表明,延长系列后干支流主要控制站点的径流成果较为稳定,多年平均年径流量和各站点20%、50%和75%频率年径流设计值的相对变化均在5%以内;洪水成果分析表明,延长洪水系列后的百年一遇设计洪水成果与前期不同阶段采用成果相比变化不大,基本均在4%以内。  相似文献   

江苏省无资料山丘区洛阳河流域径流模拟方法探讨     

纪小敏  陈颖冰  谢海文  石朋  李国芳  陈鑫 《水文》2018,38(3):57-61

近年来,无资料或资料缺乏地区汇流计算成为水文研究热点。基于地形参数的地貌瞬时单位线(GIUH)方法凭借其对历史降雨径流实测资料的不依赖性,已然成为径流模拟研究中被普遍采用且效果较好的方法之一。为探讨江苏省无资料山丘区的径流模拟方法,选取具有典型地形地貌特征的镇江通胜洛阳河小流域展开研究。根据地貌特征值等数据提取出该流域的地貌单位线,采用地貌单位线计算径流过程,利用2016、2017年汛期实测的4场洪水进行方法验证,将计算径流与实测数据进行对比分析,结果表明:基于地貌特征的地貌单位线法在该流域洪水模拟中具有较高精度,又因该流域于江苏省乃代表性区域,初步判定可将该方法推广至其他无资料山丘区流域。  相似文献   

Fractal interrelationships between topography and structure     

Thomas H. Wilson  Jovita Dominic 《地球表面变化过程与地形》1998,23(6):509-525

Factal interrelationships between topography and structure are investigated in two areas of the North American central Appalachian Mountains: one in the intensely deformed Valley and Ridge province and the other in the relatively undeformed foreland area of the Appalachian Plateau province. In the Valley and Ridge province the fractal dimensions of topographic and structural relief vary systematically along the strike of major folds following a second-order polynominal trend. Cross-correlation of the fractal dimensions of topography to structure indicates that there is a significant positive correlation between the two. Fractal analysis of topography in the relatively undeformed foreland area of the Appalachian Plateau revealed no significant variation in the fractal characteristics of topography across the study area, consistent with the lack of near-surface structure. However, fractal analysis of deeper structures beneath the Plateau area undertaken using reflection seismic data revealed step-wise increases in fractal dimension from the deeply buried Precambrian basement to the near-surface. These vertical changes in fractal dimension can be related to the tectonic history of the area. Taken together, these studies indicate that fractal analysis provides a means to quantify and compare the influence of near-surface structure on topographic development and lateral and vertical structural variability. Fractal analysis provides a means to characterize the systematic changes in the complex patterns formed by topography and structure and the interrelationships between them. Similarity in their fractal characteristics implies similarity in the relative amplitude and abundance of different wavelength features in the topographic or structural profile. © 1998 John Wiley & Sons, Ltd.  相似文献   

泥页岩储层全孔径毛管压力曲线的建立及孔隙结构特征研究     

曹茜  戚明辉  张烨毓  丁舒婷 《地质论评》2020,66(S1):104-106

  相似文献