期货交易量和现货交易量在发电公司计划中的经济分配

首先运用投资组合理论和线性规划的方法，建立了发电公司在完成计划交易电量下的利润模型，应用函数求导的单调性判别法，分析讨论期货电量和现货电量之间的不同比例对发电公司利润的影响，并对成本价格进行了相关的探讨。     

承台大体积混凝土冬期施工实例分析

以洛阳市兴隆花园153号高层商住楼承台大体积混凝土冬期施工为实例，介绍了承台大体积混凝土冬期施工的技术要求、浇筑方法、保护措施、温度的控制及养护等，为同类工程的施工提供了宝贵经验     

氧同位素标准样品的研制

使用高纯同位素物质精确配制同位素混合物,作为标准物,确定质谱仪器的系统误差。本工作用天然丰度水定量稀释高浓重氧水,制取从0.1982至96.92原子％~(18)O的氧同位素标准水样,用来校准质谱仪器。 实验采用BrF_5将水样转化成O_2。用质谱峰高法测定(18)~O和(17)~O丰度。比较质谱测定值和计算得到的丰度值C,求出质谱仪固有偏差校正系数K、并得到K与C的线性相关关系。 共得到16个具有准确丰度值的氧同位素标准水样。     

耦合Gross-Pitaevskii方程的高效保质量守恒格式

该文为耦合Gross-Pitaevskii方程提出了一个新的保质量守恒格式.首先对空间导数利用高阶紧致格式离散得到半离散格式;然后在时间方向上利用基于外推的Crank-Nicolson格式离散,得到一个半显式的数值格式,然而此格式不能保持GP方程固有的质量守恒,因此,对格式得到的数值解利用投影方法进行修正,使其满足离散质量守恒;最后通过数值实验验证了该格式具有高精度以及保持质量守恒.     

人工干预压采条件下东风湖泉域地下水环境响应研究

为掌握我国北方典型岩溶泉域在人工干预条件下地下水的动态响应规律,以涉县东风湖泉域为研究对象,结合区内地质、水文地质、2011-2021年地下水位动态监测和地下水压采资料,在分析该地区地下水动态变化特征的基础上,运用GMS软件构建了在人工压采干预作用下的地下水流数值模拟模型,对地下水位变化趋势进行了预测。结果表明：①研究区地下水动态变化明显,具有周期性、滞后性,具体表现为4个变化阶段;②研究区内岩溶地下水整体呈现回升的状态,但是空间分布特征不同,上升区主要分布于下游地区;;③地下水类型为降水入渗-开采型,低水位期基本在5-6月,高水位期在1-2月;④在干预条件下,区内地下水位有着不同程度的回升,南部(下游)浅层水位响应特征值超过15m,中游地下水位响应特征值达到了5-10m,北部(上游)地下水位响应特征值为3-5m;上游和中游地下水位影响整体小于下游,下游水位响应尤为突出。该研究对于泉域内泉的保护以及地下水开发利用和保护具有重要的理论和实际意义。     

试论群众体育与终身体育的接轨

本文从当今国际、国内逐渐兴起的终身体育教育出发,根据我国现阶段群众体育发展的现状,阐述了以终身体育为指导,使群众体育与终身体育接轨,才能更好地、广泛地开展群众体育活动,丰富人民群众的业余文化生活,实现建设体育强国的目标．     

High-precision timing of the Quaternary standard samples with thermal ionization mass spectrometry (TIMS) U-series method

Two national stalagmite standard (GBW04412, GBW04413) and one international coral standard (RKM_4) have been determined by using thermal ionization mass spectrometry (TIMS) method. The values of ( 234 U/ 238 U) act , ( 230 Th/ 234 U) act and age are all consistent in error range with the standard values obtained by using α spectrometry.     

Leakage of mantle helium from the Liaodong Peninsula, China

The isotopic cumpositions of helium have been investigated in hot spring gases sampled from the Liaodong Peninsula. China. The³He/⁴He ratios range from 0.14 Ra (0.14 times the atmospheric³He/⁴He ratio of 1.40 × 10^-6 to 0.72 Ra.³He/⁴He versus⁴He/²⁰Ne ratios and He contents suggest that a small amount of mantle-derived helium reaches the earth’s surface. Helium iwtope ratios of the hot spring gases show a distribution pattern similar to the regional heat flow values, indicating that the positive thermal anomaly occurring in the rtrea is closely associated with the presence of mantle-derived helium. The observations described above provide some significant evidence that the molten magma originating from partial melting of the upper mantle may have intruded into the continental crust along the activity fault. The coupling of the presence of mantle He and heat flow anomalies to seismic activity in studied region seem to imply that there is an internal relationship between mantle degassing and seismic activity.     

Osmium isotope determination on mantle-derived peridotite xenoliths from Panshishan with N-TIMS

The¹⁸⁷Os/¹⁸⁸Os ratios of spinel lherzolite xenoliths from Panshishan determined with N-TIMS are lower than that of the primitive mantle, which shows depleted mantle characteristics. Their positive correlation with Al₂O₃/MgO suggests that the geochemical behavior of trace elements Re and Os is similar to that of Al₂O₃ and MgO respectively during the magmatic evolution and Re-Os isotopic system is largely immune to mantle metasomatism. A model age of 2.8–3.4 Ga obtained by¹⁸⁷Os/¹⁸⁸Os-Al₂O₃/ MgO correlation might represent the homogeneous age of the mantle lithosphere beneath the area.