波峰型低损耗负群时延微波电路研究

本文提出了一种波峰形状的低损耗微波负群时延微带电路，该电路主要由四条相同的微带传输线，两条相同的耦合微带线以及T形连接器组成.依据等效电路拓扑结构，基于微波电路理论推导出电路的S参数模型以及负群时延公式.利用ADS仿真软件对电路结构进行优化，并进行了实物的加工与测试.测试结果表明：在中心频率1.017 GHz时，电路的最大群时延为-2.46 ns，插入损耗为-2.1 dB以及反射损耗为-13 dB.实测结果与仿真结果以及理论模型结果具有很好的一致性.     

初始群体飘移遗传算法用于解混和整数非线性规划问题

目前对混合整数非线性规划问题做的工作甚少，这里在研究了混舍整数非线性规划和遗传算法各自特点的基础上，提出初始群体飘移思想和变尺度整型细密网格技术，构造了一种求解混合整数非线性规划的新的遗传算法～初始群体飘移遗传算法。经理论分析和数值试验表明：该算法对大范围、多峰、非光滑非线性规划问题有较好的全局求解能力，在解的精度、稳定性和收敛速度方面均优于一般的算法。     

Excel软件优化基坑降水的井群设计

针对目前应用广泛的基坑降水井群设计方法,利用优化理论和Excel方法,以总排水量最小为目标函数,以控制点水位降深建立约束条件,对基坑降水井群的设计进行优化。并通过实例说明了该方法在基坑设计中的有效性。     

宜阳县露宝寨铜金矿区构造控矿作用探讨

论述了露宝寨铜金矿的矿区构造特点和含矿断裂特点，并对构造与成矿的关系和构造控矿机制进行了探讨。根据矿体严格受构造控制的特点，指出在该区的找矿重点应放在太华群和熊耳群之间的拆离断层附近。     

Single beam analogy for describing soil–pile group interaction

Most laterally loaded piles are flexible in the sense that they are not deformed over their entire lengths. Instead, pile deflections become negligible below an ‘active pile length’ L_a. This L_a is an important parameter that governs the overall behavior of a rigidly capped pile group. In the present approach, piles closely grouped together beneath a superstructure are viewed as a single equivalent upright beam whose stiffness matrix determines L_a. This idea is verified for different cases of pile spacing, and is further extended for nonlinear behavior of soils surrounding grouped piles.     

河北元氏丘陵山区农业生态地质类型

农业生态地质类型是农业生态地质调查研究综合性成果之一，是其调查填图的基本单位，利用把地质环境与农业生态作为一整体系统的思路，确定了农业生态地质类型划分的原则；整体系统中的主导因素，地上农业生态质量差异和宏观识别特征明显，研究区区有农业生态地质类3个、型16个，而且不同类型上农业生态质量特征差异显著。     

学习型组织与生态经济研究团队建设

信息社会和知识经济时代,科学研究整体化趋势日益加强,以个人为主的单干式科学研究已不能适应科技一体化发展趋势. 多学科交叉与应用,不仅能够创造性地丰富科学知识体系,推动经济和社会不断进步,而且还可以形成相关领域科研人员的研究团队群体创新实力. 要发挥多学科专业人员团队科研整体潜力,迫切需要与之相适应的新型组织形式和管理模式. 学习型组织作为当前的一种全新管理理念,正日益引起社会各界的广泛关注和普遍认同. 介绍了学习型组织的产生背景、发展趋势以及彼得*圣吉的五项训练的学习型组织模型,并以学习型组织为理论基础和管理原则,详细介绍了将这一管理原则在生态经济研究团队建设、具体的科研任务中的应用.     

内蒙古海拉尔～二连盆地群含煤地层层序和聚煤盆地类型的划分

海拉尔～二连盆地群蕴藏着丰富的煤、石油,是内蒙古乃至全国能源资源供应的重要基地之一。本文对盆地群的含煤地层层序和聚煤盆地类型进行分析研究,得出以下结论:海拉尔～二连盆地群早白垩世含煤地层层序自下而上划分为底砂砾岩段、粉砂泥岩含煤段、泥岩段、上粉砂岩含煤段、上砂砾岩段;海拉尔～二连盆地群的盆地类型分为半地堑盆地、地堑盆地、断陷—坳陷型盆地。     

The effect of metasomatism on the Cr-PGE mineralization in the Finero Complex, Ivrea Zone, Southern Alps

The magmatic metasomatism that was responsible for producing chromitite–dunite bodies in the unusual phlogopite peridotite of the Finero Complex in Permian to Triassic times also influenced the Cr-platinum group elements (PGE) mineralization. At least the end stages of this metasomatism are recorded in compositional zoning of chromite grains in the podiform chromitite. Metasomatic melt, with or without vapor, reacted with chromite to produce core-to-rim Cr enrichment of extant chromite grains and was concurrent with pyroxene crystallization. Under conditions of lower melt/rock ratio, metasomatism resulted in core-to-rim Al enrichment in chromite and crystallization of amphibole between chromite and clinopyroxene. This early, high-temperature metasomatism is unrelated to the later and pervasive K-metasomatism that crystallized phlogopite and was associated with the intrusion of clinopyroxenite dikes that cut the peridotite. Much later, serpentinization of olivine locally depleted chromite in Al and enriched it in Fe and formed minor amounts of magnetite.The PGE, which are present mainly as laurite inclusions in chromite, were remobilized by the early metasomatism. This resulted in substantial variation in the PGE contents of chromitites and imposed a characteristic PGE pattern in which chondrite-normalized Os, Ir, Ru and Rh contents are high but Pt and Pd contents are low. The slopes of PGE chondrite-normalized concentration patterns are systematically related to absolute PGE abundance and to rock mode. Chromitites with low modal orthopyroxene, clinopyroxene, and amphibole exhibit negative PGE slopes and contain relatively high PGE concentrations, whereas chromitites rich in these silicate minerals have positive slopes and low PGE contents.