图解法和矩值法计算西台吉乃尔盐湖沉积物粒度参数的差异     

曾方明  张萍 《盐湖研究》2015,(3):1-4, 22

柴达木盆地西部的西台吉乃尔盐湖既是研究成盐演化的典型湖泊,也是一个重要的盐湖资源产地。盐湖沉积物的粒度组成记录了湖泊沉积环境和动力条件的变化,对于理解盐湖的形成演化具有指示意义。目前有关盐湖沉积物粒度参数(平均粒径、标准偏差、偏度和峰度)计算的报道较少。采用Beckman Coulter LS 13320激光粒度仪测定了西台吉乃尔盐湖沉积剖面(XT剖面,240 cm厚)121个样品的粒度组成,并对图解法和矩值法计算出来的粒度参数进行了比较。分析结果表明,1)图解法和矩值法得出的平均粒径和标准偏差非常一致,二者可以相互替代;2)两种方法得出的偏度和峰度存在显著差别,二者不可替代;3)矩值法计算整体考虑了样品粒度的频率分布特征,得到的粒度参数比图解法更全面。  相似文献   

40m天线面板调试与精度分析     

金旺  汪敏  张巨勇  赵辉  张萍  宋俊峰  许春 《天文研究与技术》2006,3(4):401-407

总结了40m天线面板安装调试及检测的过程，分析了反映望远镜面板指标的吨性能检测结果。结果表明天线面板精度优于原设计要求。  相似文献   

长周期变星的脉冲     

Gong  ZG Li  Y 《紫金山天文台台刊》1994,13(2):168-173

Supergiant and AGB LPVs are investigated by calculating both their evolution and pulsations. The fundamental mode is thought to be the most possible pulsation mode for supergiant LPVs, and the first overtone for AGB LPVs. The mixing length and mass loss may result in some effects on the pulsations. A very large mass loss rate is demanded in the late stage of intermediate mass stellar evolution, however, the mass loss rate may not be quite large in the massive stars before their red supergiant phase. There may exist a strong stellar wind which is related with pulsation for long-period variables.  相似文献   

行道树研究——城市生物地理学的课题     

C.Y.Jim  赵抱力 《地理科学进展》1989,8(2):57-60

导言城市自然地理学的研究在气候学、地貌学和水文学方面已经有很大进展。但是,地理学家对于城市生物区系的研究尚未给予应有的注意。极其丰富多彩的城市植物区系,它与同样是变化多端的生境的联系,以及——更重要地——城市植物区系显著的空间变化,为地理探索提供了有价值的、富于创造性的课题。世界许多地区日益城市化的人类种群以及随之而来的与自然界的隔离,要求在城市区域加强生物学研究。人与环境的相互作用这一地理学的基本课题,在城市植被中鲜明地体现出来。  相似文献   

使用一种基于MgMn2O4的新型离子筛吸咐剂回收海水中的锂     

Miyai  Y  张素琴 《盐湖研究》1989,(3):145-151

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世界有效生烃岩沿地层时序的分布及其控制因素     

Klen.  HD 张萍 《国外石油地质》1992,(3):1-13

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从规划设计到实施—干旱环境中新住宅区的规划     

Gradus  Y 陈桂香 《世界沙漠研究》1991,(2):52-55

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A WIND-DRIVEN YELLOW SEA WARM CURRENT?     

Y.Hsueh 《中国海洋湖沼学报》1987,(4)

Observations of current velocity, pressure, and temperature in the eastern Yellow Sea during January 10 to April 12, 1986, and geostrophic winds calculated from surface pressure distributions, are analyzed for a study of the synoptic band response of the Yellow Sea to the wintertime winds. Currents in shallow coastal waters along a straight portion of the coast are mostly downwind to the south. Along the northern coast sheltered by a large bay, the current is persistently northward. This could be the result of a domination by geostrophic currents associated with an offshore-directed density gradient which is known to form in areas around this location. In the Yellow Sea trough, strong upwind flows are found to follow closely surges in the north wind. Co-spectral analyses show that these events are driven by a longitudinal pressure gradient associated with the sea-level set-up along the west coast of South Korea under a prevailing north wind.  相似文献   

用DTA和TG法研究MgCl2.6H2O的热脱水和水解动力学     

Kirsh.  Y  邢丕峰 《盐湖研究》1989,(3):69-78

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Transboundary aquifers: conceptual models for development of international law   总被引：2，自引：1，他引：1  

Eckstein Y  Eckstein GE 《Ground water》2005,43(5):679-690

More than one-half of the world's population is dependent on ground water for everyday uses such as drinking, cooking, and hygiene. In fact, it is the most extracted natural resource in the world. As a result of growing populations and expanding economies, many aquifers today are being depleted while others are being contaminated. Notwithstanding the world's considerable reliance on this resource, ground water resources have long received only secondary attention as compared to surface water, especially among legislatures and policymakers. Today, while there are hundreds of treaties governing transboundary rivers and lakes, there is only one international agreement that directly addresses a transboundary aquifer. Given that many of the aquifers on which humanity so heavily relies cross international borders, there is a considerable gap in the sound management, allocation, and protection of such resources. In order to prevent future disputes over transboundary aquifers and to maximize the beneficial use of this resource, international law must be clarified as it applies to transboundary ground water resources. Moreover, it must be defined with a firm basis in sound scientific understanding. In this paper we offer six conceptual models is which ground water resources can have transboudary consequences. The models are intended to help in assessing the applicability and scientific soundness of existing and proposed rules governing transboundary ground water resources. In addition, we consider the development of international law as it applies to ground water resources and make recommendations based on the models and principles of hydrogeology. The objective is the development of clear, logical, and science-based norms of state conducts as they relate to aquifers that traverse political boundaries.  相似文献