数字校园系统构建研究——以西安建筑科技大学为例

在综述数字化校园系统构建发展的基础上,以西安建筑科技大学校园为例,基于组件式地理信息系统二次开发库SuperMap Objects 5.0及Visual Basic 6.0程序开发工具,探讨了在组成"数字建大校园"的体系构架、系统功能、数据组织模型等基础上,最终构建了西安建筑科技大学校园地理信息系统。     

点带石斑鱼的精子活力及超低温冷冻前后精子超微结构的比较

研究了盐度、pH对点带石斑鱼(Epinephelus malabaricus)精子活力的影响;同时对超低温冷冻前后点带石斑鱼精子的超微结构进行了比较观察。研究结果表明:(1)该鱼精子活力的适宜盐度范围为15-35,盐度为15时,精子寿命最长为26 min;最适pH值范围为6.5-8.0,当pH值为7.5时,精子的寿命最长为4 min;(2)超低温冷冻保存前,正常的点带石斑鱼精子由头部、中段和尾部3部分组成,精子头部呈球圆形或近圆形,直径约1.8 m;中段不明显,可见线粒体;鞭毛细长,约15 m,尾部主要结构是轴丝,为典型"9+2"微管结构;(3)超低温冷冻保存后,点带石斑鱼精子的形态结构损伤明显,主要表现为质膜褶皱、破裂,细胞质外漏,线粒体膨胀破损,脱落和鞭毛断裂等特征。     

土—结构相互作用对煤矿采动损伤建筑的抗震性能影响分析

为了探讨土—结构相互作用对煤矿采动损伤建筑地震动力破坏的影响,基于损伤力学和能量耗散理论,研究采动区土—基础—上部结构的协同作用,通过建立考虑土—结构相互作用的煤矿采动损伤建筑的动力学方程,重点分析了煤矿采动损害影响下的建筑物地震动力灾变演化过程。计算结果表明:土—结构的相互作用对煤矿采动建筑的地震动力响应影响较大,不考虑土—结构相互作用是偏于安全的;煤矿采动作用明显改变了建筑物的结构动力特性,建筑结构的薄弱层位置改变明显、塑性铰和层损伤分布规律发生改变,严重降低了建筑物的抗震性能,对于煤矿采动区建筑应当开展安全损伤评估工作,以保证矿区工程建设的安全性和可靠性。     

适合于AR应用的姿态、位置综合测量系统

本文分析了AR技术的发展需求,提出适合于AR智能导航的姿态、位置综合测量系统.该系统由双频GPS接收机、陀螺仪和车辆里程计组合,采用卡尔曼滤波方法实现位置姿态测量.文章估计了滤波器实时为动态AR智能导航系统输出的位置姿态信息的精度.并通过实验验证了系统的可靠性、适用性和稳定性.     

地质岩心钻孔人工造斜方法实践

在岩心钻探施工过程中,钻遇岩（矿）心脱落需要补取岩心,或钻具脱落、埋钻和烧钻需要绕障时,人工造斜方法是解决问题的有效手段。钻孔较浅,造斜孔段刚好在变径后的位置,且上部孔壁稳定,易于扩孔和下套管,宜选用异径偏心楔人工造斜;钻孔较深,不能改变口径,造斜孔段岩层硬度较大,宜选用同径偏心楔人工造斜;钻孔较深,造斜孔段岩层硬度不大（如煤系地层中的煤层、泥岩等）,宜选用同径自然造斜。选用偏斜楔造斜时,偏斜楔长度、偏斜角大小和导斜槽直径的合理选择,偏斜楔下入钻孔过程中的正确操作;选用同径自然造斜,水泥浆灌注孔段位置确定、水泥浆凝固后达到一定的强度和造斜过程中合理的钻进参数,是造斜成功的关键。     

多环芳烃生物恢复技术的研究进展

多环芳烃是一大类广泛存在于环境中的有机污染物，本文介绍了多环芳烃生物恢复的三种不同方法：就地耕作法，场外耕作法和塞流式污泥生物反应器，并对其研究现状和最新研究成果进行了归纳，总结和探讨。     

Plant water use strategies in the Shapotou artificial sand-fixed vegetation of the southeastern margin of the Tengger Desert,northwestern China

Stable oxygen and hydrogen isotopic compositions(δ~(18)O and δD) of plant xylem water and its potential water sources can provide new information for studying water sources, competitive interactions and water use patterns of plants. The contributions of different water sources to three plants, Hedysarum scoparium(HS), Caragana Korshinskii(CK) and Artemisia ordosica(AO), were investigated in the artificial sand-fixed vegetation of Shapotou, the southeastern margin of the Tengger Desert of northwestern China, based on meteorological data and δ~(18)O and δD values of precipitation, groundwater, soil water and xylem water of HS, CK and AO. Our results indicated that soil water infiltration through precipitation was the main water source of the artificial sand-fixed vegetation. Obvious differences in soil water content and in δ~(18)O of soil water and xylem water were found among different seasons. No relationship was found between the δ~(18)O in plant xylem water and in soil water in January. The same water use patterns were found in CK, HS and AO in May, suggesting they have the same water sources. The different water sources of CK, HS and AO in August indicate that water competition occurred. In addition, the main water sources of CK, HS and AO in August mainly come from shallow soil water, while they use relatively deep soil water in May. This phenomenon is related to the differences of soil water content throughout soil profile, precipitation, transpiration and water competition under different growth periods. The water use patterns of CK, HS and AO respond to soil water content throughout the soil profile and their competition balance for water uptake during different growth season. The results indicate that these sandfixed plants have developed into a relatively stable stage and they are able to regulate their water use behavior as a response to the environmental conditions, which reinforces the effectiveness of plantation of native shrubs without irrigation in degraded areas.     

蔗渣浆厂废水对地下水影响的研究

我国造纸业废水中的污染因子危及地下水水质安全,通过对野外实地勘察和地下水取样的过程及结果进行分析研究,各地下水取样点的水质均符合国家饮用水卫生标准.用B·M舍斯塔科夫公式计算浸没过程,洪水时期地下水水位升高,研究区废水不会造成地下水的污染.     

西准阿克巴斯陶铝质A型花岗岩厘定及意义

岩石学和元素地球化学研究表明,阿克巴斯陶岩体属铝质A型花岗岩.该岩体以富硅(SiO2=74.51%～78.39%)、富碱(Na2O+K2O=7.87%～8.53%)和铝(Al2O3=11.8%～13.33%)、贫镁(MgO=0.15%～0.46%)、贫钙(CaO=0.45%～1.02%)和磷(P2O5=0.01%～0.06%),氧化指数变化较大(W=0.22～0.57),高FeOt/MgO比值(2.76～9.24,平均5.83)为特征.其K2ONa2O,NK/A=0.60～0.68,A/NCK=1.00～1.06,均大于1,属弱过铝质岩石.微量和稀土元素组成上,岩石富高场强元素(Zr和Hf等),亏损Ba,Nb,Ta,Y等元素.Zr+Nb+Ce+Y元素组合平均值(368.3×10-6)大于A型花岗岩下限值(350×10-6).在FeOt/MgO-Zr+Nb+Ce+Y和Rb/Ba-Zr+Ce+Y两类地球化学判别图解上均落入A型花岗岩区.δEu为0.038～0.130,铕强烈亏损,稀土分布曲线为"V"字型.上述特征表明,阿克巴斯陶岩体与国内外铝质A型花岗岩十分相似.在Nb-Y-Ce、AR-R1和R1-R2构造环境判别图上,显示出后造山花岗岩特征.阿克巴斯陶铝质A型花岗岩的厘定,对探讨西准噶尔地区构造演化问题具有重要意义.