Origin of sector trilling in cordierite in Daimonji hornfels,Kyoto, Japan     

Masao Kitamura  Hirohisa Yamada 《Contributions to Mineralogy and Petrology》1987,97(1):1-6

Sector trilling of cordierite in hornfels in the inner part of a contact aureole at Daimonji, Japan is a new type which consists not only of six (100) sectors (a-sectors) forming trilling, but also of (001) sectors (c-sectors) and high-index sectors (h-sectors). Complex twins within and among these sectors were studied from a viewpoint of a pseudo twin. The complex texture originated from both growth and transformation processes. The c-sector consists of three groups of domains which are related by a pseudo twin. This intrasector pseudo twin indicates that the initial phase of the c-sector was hexagonal cordierite (indialite) which later transformed to orthorhombic. The a-sector is related to adjacent sectors by a rotation of 120° around the c axis, resulting in an intersector pseudo twin. The a-sector is interpreted to have formed by overgrowth of orthorhombic cordierite on prism faces of indialite. The h-sector with the dendritic texture is also interpreted to have grown as orthorhombic cordierite. In hornfels in the middle part of the aureole, cordierites with sector trilling often coexist with single crystals of cordierite, and the sector trilling has no c- and h-sectors. This trilling type suggests that nucleation of indialite was subsequently followed by growth of orthorhombic cordierite in its stable field.  相似文献   

The effects of crystallographic orientation,interface type and growth kinetics on Ni distribution between olivine and its melt     

A. Kouchi  S. Hosoya  M. Kitamura  H. Takei  I. Sunagawa 《Physics and Chemistry of Minerals》1983,9(3-4):167-172

The effective distribution coefficient K _eff of Ni between solid and liquid has been experimentally determined as a function of growth rates and crystallographic orientations for (Mg, Ni)₂SiO₄ crystals grown by the floating-zone method. Crystals were grown by the continuous mechanism at slow rates, but were faceted at high rates, which enables us to determine the dependence of K _eff on orientations and on smooth versus rough interfaces. It has been verified that K _eff of Ni becomes larger than the equilibrium value K _o as the growth rate increases and that K _eff of faceted «110» directions is larger than that of non-faceted higher index directions. The results can be qualitatively explained by the theories which treat the distribution of elements in relation to growth kinetics. Element distribution during the recovery process from rounded to faceted morphology is also analysed in detail.  相似文献   

Interannual and interdecadal variabilities in the Pacific in an MRI coupled GCM   总被引：4，自引：0，他引：4  

S. Yukimoto  M. Endoh  Y. Kitamura  A. Kitoh  T. Motoi  A. Noda  T. Tokioka 《Climate Dynamics》1996,12(10):667-683

Interannual and interdecadal variabilities in the Pacific are investigated with a coupled atmosphere-ocean GCM developed at MRI, Japan. The model is run for 70 years with flux adjustments. The model shows interannual variability in the tropical Pacific which has several typical characteristics shared with the observed ENSO. A basin-scale feature of the principal SST variation for the ENSO time scale shows negative correlation in the central North Pacific with the tropical SST, similar to that of the observed one. Associated variation of the model atmosphere indicates an intensification of the Aleutian Low and a PNA-like teleconnection pattern as a response to the tropical warm SST anomaly. The ENSO time scale variability in the midlatitude ocean consists of the westward propagation of the subsurface temperature signal and the temperature variation within the shallow mixed layer forced by the anomalous atmospheric heat fluxes. For the interdecadal time scale, variation of the SST is simulated realistically with a geographical pattern similar to that for the ENSO time scale, but it has a larger relative amplitude in the northern Pacific. For the atmosphere, spatial structure of the variation in the interdecadal time scale is also similar to that in the ENSO time scale, but has smaller amplitude in the northern Pacific. Long oceanic spin-up time (>∼10 y) in the mid-high latitude, however, makes oceanic response in the interdecadal time scale larger than that in the ENSO time scale. The lagged-regression analysis for the ocean temperature variation relative to the wind stress variation indicates that interdecadal variation of the ocean subsurface at the mid-high latitudes is considered as enhanced ocean gyre spin-up process in response to the atmospheric circulation change at the mid-high latitudes, remotely forced by the interdecadal variation of the tropical SST. Received: 6 November 1995 / Accepted: 19 April 1996  相似文献   

Remote structural health monitoring with serially multiplexed fiber optic acoustic emission sensors     

陈仲裕  梁玉进  Farhad Ansari 《地震工程与工程振动(英文版)》2003,2(1):141-146

Development and testing of a serially multiplexed fiber optic sensor system is described. The sensor differs from conventional fiber optic acoustic systems, as it is capable of sensing AE emissions at several points along the length of a single fiber. Multiplexing provides for single channel detection of cracks and their locations in large structural systems. An algorithm was developed for signal recognition and tagging of the AE waveforms for detection of crack locations. Laboratory experiments on plain concrete beams and post-tensioned FRP tendons were performed to evaluate the crack detection capability of the sensor system. The acoustic emission sensor was able to detect initiation, growth and location of the cracks in concrete as well as in the FRP tendons. The AE system is potentially suitable for applications involving health monitoring of structures following an earthquake Supported by: National Science Foundation, Grant number CMS-9900338  相似文献   

Evapotranspiration from citrus trees growing in sandy soil under drip irrigation with saline water     

Shengli Yang  Takeuchi Shin-ichi  Yano Tomohisa  Kitamura Yoshinobu 《中国科学D辑(英文版)》2002,45(1):41-46

An experiment on evapotranspiration from citrus trees under irrigation with saline water was carried out for 4 months. Two lysimeters planted with a citrus tree in the green house were used. One lysimeter was irrigated with saline water (NaCl and CaCl₂ of 2000 mg/L equivalence,EC = 3.8 dS/m, SAR = 5.9) and the other was irrigated with freshwater using drip irrigation. The applied irrigation water was 1.2 times that of the evapotranspiration on the previous day. Evapotranspiration was calculated as the change in lysimeter weight recorded every 30 minutes. The lysimeters were filled with soil with 95.8% sand. The results of the experiment were as follows. (i) The evapotranspiration from citrus tree was reduced after irrigation with saline water. The evapotranspiration returns to normal after leaching. However it takes months to exhaust the salt from the tree. (ii) To estimate the impact of irrigation with saline water on the evapotranspiration from citrus trees, the reduction coefficient due to salt stress (K_s) was used in this experiment. Evapotranspiration under irrigation with saline water (ET _s ) can be calculated from evapotranspiration under irrigation with freshwater (ET) by the equationET _s =K _s × ET. K_s can be expressed as a function ofEC _sw . (iii) The critical soil-water electrical conductivity (EC _sw ) is 9.5 dS/m, beyond which adverse effects on evapotranspiration begin to appear. IfEC _sw can be controlled at below 9.5 dS/m, saline water can be safely used for irrigation.  相似文献   

Radium uptake during barite recrystallization at 23 ± 2 °C as a function of solution composition: An experimental Ba and Ra tracer study     

E. Curti  K. Fujiwara  J. Tits  A. Kitamura  W. Müller 《Geochimica et cosmochimica acta》2010,74(12):3553-5422

High-purity synthetic barite powder was added to pure water or aqueous solutions of soluble salts (BaCl₂, Na₂SO₄, NaCl and NaHCO₃) at 23 ± 2 °C and atmospheric pressure. After a short pre-equilibration time (4 h) the suspensions were spiked either with ¹³³Ba or ²²⁶Ra and reacted under constant agitation during 120-406 days. The pH values ranged from 4 to 8 and solid to liquid (S/L) ratios varied from 0.01 to 5 g/l. The uptake of the radiotracers by barite was monitored through repeated sampling of the aqueous solutions and radiometric analysis. For both ¹³³Ba and ²²⁶Ra, our data consistently showed a continuous, slow decrease of radioactivity in the aqueous phase.Mass balance calculations indicated that the removal of ¹³³Ba activity from aqueous solution cannot be explained by surface adsorption only, as it largely exceeded the 100% monolayer coverage limit. This result was a strong argument in favor of recrystallization (driven by a dissolution-precipitation mechanism) as the main uptake mechanism. Because complete isotopic equilibration between aqueous solution and barite was approached or even reached in some experiments, we concluded that during the reaction all or substantial fractions of the initial solid had been replaced by newly formed barite.The ¹³³Ba data could be successfully fitted assuming constant recrystallization rates and homogeneous distribution of the tracer into the newly formed barite. An alternative model based on partial equilibrium of ¹³³Ba with the mineral surface (without internal isotopic equilibration of the solid) could not reproduce the measured activity data, unless multistage recrystallization kinetics was assumed. Calculated recrystallization rates in the salt solutions ranged from 2.8 × 10⁻¹¹ to 1.9 × 10⁻¹⁰ mol m⁻² s⁻¹ (2.4-16 μmol m⁻² d⁻¹), with no specific trend related to solution composition. For the suspensions prepared in pure water, significantly higher rates (∼5.7 × 10⁻¹⁰ mol m⁻² s⁻¹ or ∼49 μmol m⁻² d⁻¹) were determined.Radium uptake by barite was determined by monitoring the decrease of ²²⁶Ra activity in the aqueous solution with alpha spectrometry, after filtration of the suspensions and sintering. The evaluation of the Ra uptake experiments, in conjunction with the recrystallization data, consistently indicated formation of non-ideal solid solutions, with moderately high Margules parameters (W_AB = 3720-6200 J/mol, a₀ = 1.5-2.5). These parameters are significantly larger than an estimated value from the literature (W_AB = 1240 J/mol, a₀ = 0.5).In conclusion, our results confirm that radium forms solid solutions with barite at fast kinetic rates and in complete thermodynamic equilibrium with the aqueous solutions. Moreover, this study provides quantitative thermodynamic data that can be used for the calculation of radium concentration limits in environmentally relevant systems, such as radioactive waste repositories and uranium mill tailings.  相似文献   

海洋牧场背景下的休闲渔业旅游发展模式研究   总被引：1，自引：0，他引：1       下载免费PDF全文

宋昱瑾  田涛  杨军  刘敏  吴忠鑫  高东奎  尹增强  李晓钰 《海洋开发与管理》2022,39(1):110-116

近年来随着产业融合的发展趋势显著,第一产业和第二产业开始向第三产业转型,海洋牧场建设发展过程中渔业与旅游业逐渐融合发展形成休闲渔业等渔业旅游形式。许多地区因地制宜形成了不同的休闲渔业发展模式,休闲渔业旅游发展多元化的趋势也在逐渐形成。文章对休闲渔业的概念进行了阐述,介绍了休闲渔业的产生与发展,并对我国休闲渔业的旅游模式进行归纳,提出当前休闲渔业发展存在的问题。如:发展观念滞后,缺乏长远规划;海洋休闲渔业产业结构单一;缺乏高素质的从业人员;科技、资金投入不足等。最后总结了海洋牧场背景下休闲渔业的未来发展趋势并对发展方向提出建议。  相似文献   

基于企业大数据的京津冀制造业集聚的影响因素     

黄宇金  盛科荣  孙威 《地理学报》2022,77(8):1953-1970

产业集聚是经济活动最突出的地理特征之一,也是经济地理学重要的研究对象,然而对产业集聚的机制解释往往由于没有很好的区分产业空间分布形态和产业集聚阶段而出现偏差。本文基于3次全国经济普查企业微观数据,利用DO指数方法计算了2004—2013年京津冀地区三位数制造业行业的空间分布形态,利用Hurdle模型定量解释了集聚形成和集聚提升两个阶段的影响因素及其差异性。结果表明：① 2004年、2008年和2013年京津冀地区分别有124个、127个、129个三位数行业集聚,技术密集型和劳动密集型制造业集聚强度较高,但整体集聚强度出现下降,从0.332下降至0.261。② 制造业集聚存在两阶段且主导因素存在差异。在集聚形成阶段,企业主要考虑基础条件,农业资源和交通运输有负向作用,劳动力池和外商投资有正向作用;在集聚提升阶段,企业更侧重于集聚经济和政策等因素,产业内部关联和产业外部关联有正向作用且前者作用更强,开发区主导产业政策和电力燃气水资源起负向作用。③ 影响因素对产业集聚的作用具有尺度效应,均随距离扩大呈现减弱趋势,但不同因素对距离的反应存在差异。  相似文献   

Long-term variations of North Pacific Tropical Water along the 137°E repeat hydrographic section     

Toshiya Nakano  Tomoyuki Kitamura  Shusaku Sugimoto  Toshio Suga  Masafumi Kamachi 《Journal of Oceanography》2015,71(3):229-238

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Reminiscences of a Japanese Contemporary     

Masatoshi Kitamura 《Astrophysics and Space Science》2005,296(1-4):33-41

It was in 1936 when a young Czech student of age 22 came to Japan through Siberia for participating in the solar eclipse expedition. Since then, he had visited us 13 times until 1993 (when he passed away). At each visit his lectures were vivid for us and had strong impact on the audience. Needless to say, it was the late Professor Zdeněk Kopal. In this brief presentation first I reveal my reminiscences of our common time in Manchester and Japan as a contemporary, and second I make some remarks on my activities for the Japanese Official Development Assistance (ODA) for astronomy in developing countries, in a similar way like Professor Kopal contributed in later years to the development of astronomy mainly in middle-east countries.  相似文献