外商直接投资与经济增长的关系研究——基于分省和分区数据的检验   总被引：1，自引：0，他引：1  

杨柳勇  陈立慧  楼惠新 《地球信息科学学报》2008,10(3):350-356

论文分别以分省和分区（东、中、西部）1992～2004年的面板数据,利用我们修正过的De Mello模型和更为稳健的模型检验方法,研究了我国利用外商直接投资对经济增长的影响作用。研究结果发现,利用分省数据的模型证明了FDI对我国经济增长的正向积极作用,这一点与其他研究结果相同,但是利用分区数据的研究表明,虽然我国西部仍然是FDI作用最弱的区域,但是东部与中部比较,GDP增长率变动对FDI增长率变动的敏感性不明显,有别于中部,这在一定程度上可以说明东部地区存在FDI过密和外商投资产业的过度竞争问题。  相似文献   

Observations on shell growth and morphology of the bivalve Ruditapes philippinarum     

范德江  张爱滨  杨作升  孙效功 《中国海洋湖沼学报》2007,25(3):322-329

The bivalve Ruditapes philippinarum is not only one of the main mollusc species in the west Pacific Ocean, but also one of the main species for aquaculture in China. Knowledge of growth of the R. philippinarum shell will improve our understanding of the shell as an environmental archive. It is also useful for the aquaculture of R. philippinarum. In this research, a hanging box culture method was introduced in the culture of R. philippinarum. The bivalves were cultured for 126 days, from March 31 to August 3, 2002. The average growth rates of shell width, height, and thickness were 0.069, 0.046, and 0.032 mm/d, respectively. The mean increase of average individual wet mass was 0.028 g/d. The largest growth rates of both shell and average individual wet mass occurred in June, indicating that water temperature and bivalve reproduction were 2 important factors. The shell morphology underwent significant changes with shell growth. The ratio of height to thickness (value of B/C) shifted 1.58 in the first 60 days to 1.54 in the last 30 days, which was resulted from the change in major shell growth direction. Periodic changes in the B/C ratio led to corrugated shell form, which could be used to determine the age of the shell.  相似文献   

饲料中添加胜肽和益生菌对大黄鱼生长性能和体组成的影响          下载免费PDF全文

柯巧珍  余训凯  张永兴  潘滢  陈秋平  黄匡南  陈佳  翁华松  包欣源  韩坤煌  刘永裕  刘家富 《应用海洋学学报》2018,37(1):141-145

以初始体重为48.23±1.25 g的大黄鱼(Larimichthys crocea)为试验对象,研究饲料中添加胜肽和益生菌对大黄鱼生长性能、体组成的影响.添加胜肽试验组所用饲料为添加500mg/kg胜肽产品配制成软颗粒饲料;添加胜肽-益生菌试验组所用饲料为添加500mg/kg胜肽产品和500mg/kg益生菌产品配置成的软颗粒饲料;对照组所用饲料为未添加胜肽和益生菌产品而以相同配方配制成的软颗粒饲料.整个养殖试验的周期为12周,并于海水浮式网箱中进行.结果表明,饲料中添加胜肽和胜肽-益生菌均显著提高大黄鱼的终末体质重(FW)、特定生长率(SGR)、鱼体增重率(WGR)、饲料效率(FE)和粗脂肪含量(p0.05);饲料中添加胜肽对大黄鱼水分、粗蛋白、灰分、肝脏指数(HSI)、内脏指数(VSI)和肥满度(CF)的影响不显著(p0.05);添加胜肽-益生菌饲料组VSI显著高于添加胜肽饲料组和对照组(p0.05).  相似文献   

Anchor ice formation in streams: a field study     

Morten Stickler  Knut T. Alfredsen 《水文研究》2009,23(16):2307-2315

In northern steep streams anchor ice is commonly observed during winter, and plays a key role when considering in‐stream conditions. The understanding, however, of the nature of anchor ice formation is less understood, in particular, under natural conditions. In the following, observations of anchor ice formation in three stream environments with different physical characteristics are presented. Results demonstrate that anchor ice not only form in riffle areas, but also in shallow and slow running stream sections. No linkage between spatial distribution of anchor ice and calculated dimensionless numbers (Froude and Reynolds number) was found. Furthermore, analyses on growth and density showed that anchor ice may be distinguished by two main types. (1) Type I: Lower density forming on top of substrata. (2) Type II: Higher density forming between the substrata filling interstitial spaces. Distribution of anchor ice Types I and II suggests a relation between intensity of turbulence expressed by the Reynolds number, growth pattern and density. As anchor ice has both physical and biological implications on in‐stream environments, findings from the present study may be of particular interest to cold region freshwater stream management. Copyright © 2009 John Wiley & Sons, Ltd.  相似文献   

STUDY ON EMBRYONIC DEVELOPMENT AND EARLY GROWTH OF TRIPLOID AND GYNOGENETIC DIPLOID LEFT-EYED FLOUNDER, PARALICHTHYS OLIVACEUS (T. et S.)     

尤锋  刘静  王新成  徐永立  黄瑞东  张培军 《中国海洋湖沼学报》2001,(2)

ＩＮＴＲＯＤＵＣＴＩＯＮＴｒｉｐｌｏｉｄｙｉｎｄｕｃｔｉｏｎａｎｄｇｙｎｏｇｅｎｅｔｉｃｄｉｐｌｏｉｄｉｎｄｕｃｔｉｏｎａｓｍａｉｎｐａｒｔｓｏｆｃｈｒｏｍｏｓｏｍａｌｍａｎｉｐｕｌａ ｔｉｏｎｈａｖｅｂｅｅｎｐｌａｙｉｎｇｍｏｒｅａｎｄｍｏｒｅｉｍｐｏｒｔａｎｔｒｏｌｅｓｉｎｍｏｄｅｒｎｆｉｓｈｂｒｅｅｄｉｎｇ .Ｍｏｓｔｔｒｉｐｌｏｉｄｆｉｓｈａｒｅｓｔｅｒｉｌｅａｎｄｔｈｅｉｒｒｅｄｕｃｅｄｇｏｎａｄａｌｄｅｖｅｌｏｐｍｅｎｔｒｅｓｕｌｔｓｉｎｉｍｐｒｏｖｅｍｅｎｔｏｆｇｒｏｗｔｈｒａｔｅａ…  相似文献   

Crack-fill porphyroblastesis     

Andrew J. Barker 《Journal of Metamorphic Geology》2002,20(2):283-294

Garnet‐mica schists from the Scottish Highlands provide new insight into an important mechanism of phyllosilicate growth, termed ‘crack‐fill porphyroblastesis’. It is shown that grain boundary dilatancy, microcracking and porphyroblast‐matrix decoupling all play a significant role in facilitating growth in regimes of noncoaxial shear. With respect to chlorite porphyroblasts, there are three growth stages. Following nucleation, the initial phase of growth is by progressive matrix replacement, to preserve inclusion trails of fine carbonaceous material. The second growth stage produced new optically continuous inclusion‐free chlorite on the {001} margins of those crystals at a high angle to the schistosity. This growth results from decoupling at the porphyroblast–matrix contact on those margins at a high angle to the principal axis of extension. The development of dilatant cracks at porphyroblast margins provides a sink for material migrating down P_f and chemical potential gradients. This causes precipitation of new optically continuous ‘clear’ chlorite on the pre‐existing, heavily included core. The porphyroblast–matrix boundary continues to dilate after porphyroblast growth had terminated, producing plano‐convex quartz‐rich strain shadows. Similar growth behaviour is recognised in biotite porphyroblasts, indicating that ‘crack‐fill porphyroblastesis’ is an important growth mechanism for phyllosilicates in actively deforming metamorphic rocks. It also indicates that decoupling and crack‐fill development at porphyroblast margins could be important in controlling the pattern of material transfer, and may have significant implications for matrix permeability and fluid‐flow characteristics.  相似文献   

THE PEATLAND/ICE AGE HYPOTHESIS REVISED, ADDING A POSSIBLE GLACIAL PULSE TRIGGER     

LARS G. FRANZÉN  ROGER A. CROPP 《Geografiska Annaler: Series A, Physical Geography》2007,89(4):301-330

Carbon sequestering in peatlands is believed to be a major climate‐regulating mechanism throughout the late Phanerozoic. Since plant life first evolved on land, peatlands have been significant carbon sinks, which could explain significant parts of the large variations in atmospheric carbon dioxide observed in various records. The result is peat in different degrees of metamorphosis, i.e. lignite, hard coal and graphite. During phases of extensive glaciations such as the 330–240 Ma Pangea Ice Age, atmospheric carbon dioxide was critically low. This pattern repeats itself during the Pleistocene when carbon dioxide oscillates with an amplitude of c. 200–300 ppmv. This paper suggests that the ice age cycles during the Pleistocene are generated by the interglacial growth of peatlands and the subsequent sequestering of carbon into this terrestrial pool. The final initiation of ice age pulses towards the end of inter‐glacials, on the other hand, is attributed to the cyclic influx of cosmic dust to the Earth surface, which in turn regulates cloud formation and the incoming shortwave radiation. These shorter cycles have a frequency of c. 1000‐1250 years and might be connected to sunspot or other low frequency solar variations. In a wider context the ice age cycling could be regarded as an interplay between terrestrial life on the high latitudes of the northern hemisphere and the marine subsurface life in the southeast. If the results presented here are correct, the present global warming might just be the early part of a new warm period such as the Bronze Age and the Roman and Medieval Warm periods. This could be caused by entry into another phase of decreasing influx rates of cosmic dust. The increasing concentrations of atmospheric carbon dioxide might have contributed to this warming but, most important of all, it might temporarily have saved us from a new ice age pulse.  相似文献   

真实自回避行走中晶体生长界面结构的分形行为     

彭年刘永顺  聂保锋刘宁强 《岩石矿物学杂志》2007,26(5):449-452

晶体生长过程实际上就是生长基元从周围环境中不断地通过界面而进入晶格座位的过程。一般认为,研究生长基元以何种方式以及如何通过界面进入晶格座位是晶体生长界面结构研究中的关键。在生长基元以分子或者原子的微粒子形式在生长环境中进行无规游走的前提下,本文运用真实自回避行走(TSAW)模型,通过重整化群思想来研究晶体生长界面结构的分形行为。研究发现:晶体生长界面结构的分形行为与生长基元的游走路径形态密切相关,并且在理想状况下真实自回避行走与标准Koch曲线的分形维极为接近。  相似文献   

Three Stages of Zircon Growth in Magmatic Rocks from the Pingtan Complex, Eastern China          下载免费PDF全文

WANG Xiang W. L. GRIFFIN S. Y. O＇REILLY LI Wuxian 《《地质学报》英文版》2007,81(1):68-80

Morphological and chemical studies on zircon grains from gabbro and granite of the Pingtan magmatic complex, Fujian Province, eastern China, show that there are three stages of zircon growth. The early stage of zircon growth is characterized by colorlessness, high transparence and birefringence, low and dispersive Ipr and Ipy, weak and homogeneous BSE brightness, lower Hf content and depletion of U, Th and Y; the middle stage is characterized by abruptly increasing lpy, progressively strong and sectoral-zoning BSE brightness, higher Hf content and enrichment of U, Th and Y with Th/U 〉 1; the late stage of growth is characterized by brownish color, poor transparence, low birefringence, highest Ipr and Ipy, middle and oscillatorily-zoning BSE brightness, highest contents of Hf, U and Y with Th/U 〈 1. The stages are considered to be formed in a deep magma chamber, ascent passage and emplacement site, respectively. Due to the more or less long residual time of the magma chamber, the difference in age between the early and late stages of zircon might be great enough to be distinguished, which can be attributed to tectonic constraint for the magnlatism.  相似文献   

大别地体超高压变质岩石锆石Lu-Hf同位素研究   总被引：2，自引：3，他引：2  

陈道公倪涛  谢烈文 《岩石学报》2007,23(2):331-342

对大别山南部超高压变质带双河和黄镇地区的榴辉岩、片麻岩和硬玉石英岩中变质锆石进行了原位LA-MC-ICP- MS的Lu-Hf同位素分析。双河和黄镇的榴辉岩及双河的硬玉石英岩有低~(176)Lu/~(177)Hf和低~(176)Hf/~(177)Hf组成,两地的片麻岩有高~(176)Hf/~(177)Hf比和高且分散的~(176)Lu/~(177)Hf组成。锆石Hf同位素分布主要受变质原岩的形成时代控制,增生锆石基本上继承了原岩锆石的Hf同位素特征,既有增生锆石相对有低~(176)Lu/~(177)Hf和高~(176)Hf/~(177)Hf、继承重结晶锆石相对有高~(176)Lu/~(177)Hf和低~(176)Hf/~(177)Hf的特征,也有二者相互重叠没有区别的,它主要受原岩性质和变质过程中锆石遭受的溶蚀程度控制。增生锆石的低Lu/Hf是锆石在变质过程中Lu含量下降和Hf含量增高造成的,增生锆石的高~(176)Hf/~(177)Hf继承自岩石中其它高Lu/Hf比矿物的长期演化。继承锆石的初始Hf同位素组成ε_(Hf)值和亏损地幔模式年龄T_(DM)示踪表明,各超高压变质原岩的时代和成因是复杂的:双河榴辉岩原岩物质源自25亿年的亏损地幔和至少27亿年以上的古老晚太古地壳混合。双河片麻岩原岩年龄相同,但有不同的壳幔混合物源。黄镇榴辉岩原岩主要源于亏损幔源岩浆形成的初生地壳的重循环,很少的地壳混染。黄镇片麻岩和榴辉岩的物源区年龄相同。两地片麻岩原岩物源主要来自弱亏损地幔,存在古老地壳物质和地幔物质的混合。大别地区超高压变质岩锆石的Lu-Hf同位素特征主要反映了7～8亿年和18～19亿年时扬子克拉通北缘地区的岩浆活动特点和大地构造环境。  相似文献