Changes in wind speed over China during 1956–2004     

Ying Jiang  Yong Luo  Zongci Zhao  Shuwang Tao 《Theoretical and Applied Climatology》2010,99(3-4):421-430

Based on two observational data sets in China from 1956 to 2004, wind speed changes are analyzed. The annual mean wind speed (MWS), days of strong wind (SWDs), and maximum wind (MW) all show declining trends over broad areas of China. Only in the southeastern Tibetan Plateau and the regions from the Great Bend of the Yellow River southward to Yunnan and Guangxi Provinces wind speeds are not significantly reduced, but rather, in partial, these regions’ winds speeds are slightly increased. The regions with declining trends match the areas with relatively strong observed winds and the regions without significant declining trends match the areas with light observed winds. In the meantime, the regions with relatively strong winds correspond to areas of reduced days of SWDs. Trends for both increasing intensities and for the number of days of light winds both impact the installation of wind energy facilities. These may be advantageous to the development of wind energy in different regions. Urbanization, the change of anemometers, or relocation of stations are factors that are mildly responsible for the decreasing trend of MWS. The main reason for the decreasing trend is that under the background of global warming, the contrasts of the sea level pressure, and near-surface temperature between the Asian continent and the Pacific Ocean have become significantly smaller, and the east Asian trough has shifted eastward and northward, and has weakened as well. Both East Asian winter and summer monsoons are decreasing, and all of these impacts have resulted in declines of MWS in China.  相似文献   

广西龙州地区双层含铝岩系地质特征与找矿意义     

韦访  黄文芳  罗家元 《江苏地质》2023,47(4):358-368

对龙州地区合山组和都安组铝土岩（矿）层进行系统采样分析，并与堆积铝土矿进行对比研究，结合含铝岩系岩性与矿物特征发现，合山组、都安组铝土岩（矿）矿石矿物无显著差异，主要为一水硬铝石、高岭石、（鲕）绿泥石，其次为赤铁矿（针铁矿）集合体和碎屑物（岩屑、玻屑、砾屑），普遍存在大量（铁）凝胶。常量、微量、稀土元素特征及相关图解显示，合山组、都安组铝土岩（矿）均可能为该区堆积铝土矿的矿源层。Ni-Cr图解显示合山组铝土岩（矿）可能来自与火山物质有关的玄武岩，都安组铝土岩（矿）来源于卡斯特岩溶，堆积铝土矿除部分落入玄武岩、碳酸盐岩区以外，大多位于页岩、板岩内，表明该区堆积铝土矿存在多源性。微量元素Be、Ga、Sr、Ba含量与Sr/Ba、V/Zr、Zr/Cu含量比值等沉积环境元素特征表明该区原生铝土岩（矿）沉积环境为陆相；δCe分析显示铝土岩（矿）沉积环境有所差异，合山组表现为氧化环境，都安组则表现为还原环境。Th、U含量及Th/U含量比值显示该区铝土岩（矿）成矿以混合作用为主，并经历了较强的风化作用；δEu分析表明合山组、都安组铝土岩（矿）分别形成于被动大陆边缘与活动大陆边缘。合山组、都安组含铝岩系均发育不同程度的铝土岩（矿）层，都安组铝土岩（矿）部分样品已达工业边界指标，可作为沉积铝土矿勘查的主要目的层。  相似文献   

THE PROGRESS IN URBAN SOCIAL SPACTIAL DIFFERENTIATION STUDY OF CHINA     

吴启焰  罗俊彦 《中国地理科学(英文版)》1999,9(3):206-212

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基于光纤自相位调制多波长全光再生的色散管理优化     

张婧  潘炜  闫连山  罗斌 《海洋学报》2010,32(10):7002-7007

针对基于光纤自相位调制效应的多波长全光再生系统,分析了光纤平均色散对再生器品质因子改进量的影响,提出一种色散管理优化方法.由于波长间色散差异会导致再生系统性能的稳定性下降,通过选择色散补偿光纤和单模光纤的长度,使其合成的色散曲线与各波长分别达到最优再生性能时对应的色散曲线近似拟合,同时保证该色散曲线落在性能满意度高的色散区域,然后调整信号输入功率和滤波器的偏移量,可有效改善多波长再生性能的稳定性,实现再生器的色散管理优化.  相似文献   

The color properties of compact groups of main galaxies from the SDSS Data Release 4     

Xin-Fa Deng  Ji-Zhou He  Peng Jiang  Cong-Gen He  Cheng-Hong Luo  Ping Wu 《Astrophysics》2007,50(1):18-25

In order to compare color statistical properties of member galaxies in compact groups with those of field galaxies, we use a compact group (CG) sample which contains 4217 CGs extracted from the MAIN galaxy sample of the SDSS Data Release 4 (SDSS4), and construct a random group sample which has the same distributions of redshift and number of member galaxies as those of the CG sample. It turns out that the mean colors of galaxies in CGs are redder than those of galaxies in random groups. Additionally, we also find that member galaxies in real CGs have a smaller dispersion of colors than those in random groups-at least for g-r, r-i, and i-z colors. Published in Astrofizika, Vol. 50, No. 1, pp. 29–37 (February 2007).  相似文献   

Collocation-PECE�㷨�ڵ͹����Ǿ��ܶ����е�Ӧ��   总被引：1，自引：1，他引：0  

洪樱  欧吉坤  罗孝文 《大地测量与地球动力学》2007,27(4):72-76

???????????У?PECE????????????????????????????Collocation????????????????幫??????????μ?PECE???????????????????ж??????????????????????????????????????????????????????????????????????????????????????????????????????????????????????Adams-PECE????????PECE?????????????????????????????,???????????Collocation-PECE??????????????н???????????????Ч??  相似文献   

辐照条件下绿柱石通道中顺磁配合物的ESR行为   总被引：2，自引：3，他引：2  

亓利剑  向长金  刘国根  裴景成  罗永安 《地质科技情报》2001,20(2):59-64

四川平武贫铁富碱型无色绿柱石通道中主要存在碱氢化物（NaH)、[Fe2(OH)4]^2 多聚合离子及OH自由基，在电子辐照作用下，通道中顺磁配合物的结构、带电性质及化学键易发生转型、裂解和变价，并形成自旋浓度不等的[H^0]i心（裂距为500G,g值分别为2．175，1．8774的二重超精细结构线）、[Fe^3 ]OH(g=2.0031)和[Fe4^3 ]s(g=4.3172)等辐照损伤心。[Fe^3 ]OH心属一种有效的电子陷阱，其热稳定性大于[Fe4^3 ]s心。绿柱石杂质铁离子的占位方式，与成矿物理、化学条件及成矿流体的pH值密切相关。由电子辐照作用而导致杂质离子价态的转变，属一种可逆的动态平衡过程。  相似文献   

一维渗透固结中排水边界生成与识别的初步探讨     

黄松华  侯龙清  潘小青  罗嗣海 《上海国土资源》2001,(Z1):68-71

本文首先分析了内部与表部土层生成排水边界时的渗流方向并提出了绝对与相对排水边界的概念;然后分别讨论了绝对与相对排水边界的识别标准.  相似文献   

碎屑岩输导层内油气运聚非均一性的定量分析   总被引：29，自引：7，他引：29  

李铁军  罗晓容 《地质科学》2001,36(4):402-413

油气在以连通孔隙为流体储、流空间的碎屑岩输导层中的运移具明显的非均一性。在实际盆地中,输导层往往是非均质的,在宏观上表现为岩性、岩相在盆地范围内的频繁变化,在微观上则主要受粒度大小、胶结物含量、成岩作用等的影响。利用BasinMod所做的定量模拟试验发现,即便在宏观均质孔隙介质中,油气运移的动力也往往是非均一的,表现为受控于构造形态的空间变化。在非均质输导层中,运移动力的非均一性与所处的地质背景有关:在毛细管力梯度小于浮力梯度时,流体势的梯度方向与浮力梯度方向相同,油气运移仍沿浮力降低的方向进行;当毛细管力梯度大于浮力梯度情况下,流体势梯度方向发生改变,岩性变化带成为油气运移的封挡层。将数值模拟分析的认识应用于准噶尔盆地腹部侏罗系三工河组,在假设输导层侧向延伸性良好的条件下,分析了输导层油气运移路线,认为石西1井区、盆4井区及陆1井区等构造高部位为重要的油气运移指向区。  相似文献   

The Cenozoic mantle magmatism and motion of lithosphere on the north margin of the Tibetan Plateau     

Luo Zhaohua  Xiao Xuchang  Cao Yongqing  Mo Xuanxue  Su Shangguo  Deng Jinfu  Zhang Wenhui 《中国科学D辑(英文版)》2001,44(1):10-17

Geodynamic properties and evolution of the lithosphere on the north margin of the Tibetan Plateau are recently hot topics to geoscientists in the world. Have the northern plates been subducting underneath the Plateau? It is still an unsolved problem. One of the keys to solving this problem is to understand the genetic processes of Cenozoic magmas on the north margin of the Tibetan Plateau. However, there is no enough evidence supporting the subduction model. In contrast, a series of evidence indicates that collision-induced huge shearing faults and large-scale crust shortening played a main role in lithosphere motion on the north margin of the Tibetan Plateau. The mantle-derived igneous rocks strictly distribute at the intersections of large strike-slip faults on the north margin of the Plateau. Generation of magmas may be related to local extensional condition induced by strike-slipping faults, which lead to lithosphere gravitational instability and collapse, as well as upwelling of the deep hot material. Heat induced by shearing and carried by upwelling hot material may cause partial melting on H₂O-bearing mantle.  相似文献