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A Probe into the City Combination of Shanghai,Hangzhou & Ningbo
构建沪-杭-甬组合城市的新探索

HU Gang,ZHOU Fu duo,
胡刚
,周复多

浙江大学学报(人文社会科学版) , 2002,
Abstract: The six cities - including Shanghai, Hangzhou and Ningbo - around the Hangzhou Bay have maintained close social and economic relationships with each other. With transportation and other infrastructure facilities improving day by day and especially the Hangzhou Bay Bridge under construction, two hours' car drive will be made possible between Shanghai, Hangzhou and Ningbo. As groups of cities, belts of cities and rings of cities are being formed in many parts of the world today, Shanghai, Hangzhou and Ningbo in the Bay area are likely to form a city combination. Based on the analysis of the present conditions of the Bay cities' development and the important function of the city combination, a tentative plan is advanced for the space planning of the combination.
杭州地区34种观果植物的综合评价与分析
Comprehensive Evaluation and Analysis on 34 Ornamental-Fruit Plants in Hangzhou
 [PDF]

徐明,蔡建国,臧毅,王丽英
- , 2016, DOI: 10.3969/j.issn.1001-7461.2016.03.49
Abstract: 对杭州地区34种观果植物采用层次分析法(AHP)进行评价与分析。评价的约束层权重值分别为果(C1)0.715 3,花(C2)0.187 0以及其他影响因子(C3)0.097 8,说明观果植物的观赏性状是以果实观赏为基础,在人们的视觉观赏中占有较大分量。34种观果植物可分为5个等级,等级Ⅰ共4种植物,占总数的11.8%,等级Ⅱ共12种植物,占总数的35.3%,等级Ⅲ共10种植物,占总数的29.4%,等级Ⅳ共4种植物,占总数的11.8%,等级Ⅴ共4种植物,占总数的11.8%。
Analytic hierarchy process (AHP) was adopted to evaluate 34 ornamental-fruit plants occurring in Hangzhou area.Constrained layer weights of evaluation values were fruit (C1) 0.715 3,flower (C2) 0.187 0 and other factors (C3) 0.097 8,indicating that the ornamental characters of fruit plants is based on their fruit,which accounted for a large component in people’s visual enjoyment.Based on the final scores of the evaluation,34 plant species were divided into 5 levels,in which 4 species were in level,accounting for 11.8% of the total,12 species in level II,35.3%,10 species in level Ⅲ,29.4%,4 species in level IV,11.8%,and 4 species in level V,11.8%
A Reseau-Dividing Algorithm for Distributing Products of Hangzhou Tobacco Company
杭烟物流送货线路的划分模式与算法研究

CHEN Zi-xia,JIANG Chang-bing,
陈子侠
,蒋长兵

系统工程理论与实践 , 2004,
Abstract: A reseau-dividing algorithm was presented in this paper for determining more than 110 distribution lines in routing the products of Hangzhou Tobacco Company. There are more than 6400 cigarette shopkeepers selling products for this company. The method aims to reach the equilibrium of generalized workload between different distribution lines. Simulation results show that the algorithm is both effective and applicable,and it may extend to other cases.
Analysis of peroxidase isozymes and HPLC chromatographic study of paeoniflorin in Hangzhou white peony
杭白芍过氧化物酶同工酶及芍药苷HPLC图谱分析

Song QIN,HU Jia-shu,TONG Fu-dan,HU Qiao-ping,
宋勤
,胡家恕,童富淡,胡巧平

浙江大学学报(农业与生命科学版) , 2005,
Abstract: The peroxidase isozymes of Hangzhou white peony were isolated by polyacrylamide gel electrophoresis.Up to 2-5 active bands of peroxidase isozyme were observed in 13 lines after active dyeing, and the rate of relative migration was located in the range from 0.567 to 0.685. Based on the differences in number and location of bands the individuals were divided into 3 groups. The results of HPLC showed that paeoniflorin was the primary component in Hangzhou white peony, and only a little albiflorin with no oxypaeoniflorin was observed. The paeoniflorin content of Hangzhou white peony as detected after different processing was different, although the HPLC chromatograms of paeoniflorin were similar.
Geological characteristics and genesis of porphyry copper deposits in Qinzhou-Hangzhou suture zone, South China
钦-杭结合带斑岩型铜矿的基本地质特征及成因分析

LIANG Jin,ZHOU YongZhang,LI HongZhong,YIN ZhuiZhui,ZHOU LiuYu,ZENG ChangYu,YU PengPeng,
梁锦
,周永章,李红中,尹缀缀,周留煜,曾长育,虞鹏鹏

岩石学报 , 2012,
Abstract: The Qinzhou Bay-Hangzhou Bay suture zone (QHSZ) is an important porphyry copper deposits (PCD) belt. PCDs are well distributed in the northern, the middle and the south sections of the QHSZ. They are mainly formed in the Yanshanian Period. Porphyries related to copper mineralization are mainly granodiorite porphyry, granite porphyry and sub-dacite porphyry, which belong to the calc-alkaline magma series of acidic rock. The porphyries above have similar trace element geochemical characteristics of the Neoproterozoic island arc igneous rock. They are derived from the partial melting of a mixture of magma in asthenosphere and the lower crustal material, and are related to the lithospheric mantle affected by earlier plate subduction, with evident crust-mantle contamination. The geodynamic setting of the Yanshanian petrogenesis and metallogenesis of the QHSZ is characterized by subduction of the Pacific plate, while the Yanshanian porphyries and copper ore bodies have the trait of island arc magma system, which is related to the geological evolution before the Mesozoic tectonic transition event in South China. It is concluded that such acidic porphyries of the QHSZ resulted from the partial melting of the Proterozoic island arc basaltic rocks during the Mesozoic, and the associated PCDs have the gene of island arc subduction environment.
THE WILD ORNAMENTAL XYLOPHYTA RESOURCE IN THE SHERGYLA MOUNTAIN REGION IN TIBET AND ITS EXPLOITATION AND UTILIZATION
西藏色季拉山野生观赏树木资源及其开发利用

Zheng Weilie,
郑维列

自然资源学报 , 1996,
Abstract: The wild ornamental xylophyta resource in the Shergyla Mountain region is abundant. There are 40 families, 75 genuses and more than 190 spieces. The main families are Rose Family, Heath Family, Honeysuckle Family, Saxifrage Family and Pea Family. The main genuses are Rhododendron, Honeysuckle, Plum, Spiraea and Contoneaster. Of them 47.6% are Flower trees, 24.6% are Flower-fruit trees, and 11.0% are Fruit trees. Of the Flower trees, 46.4% are white flower spices, 19.6% yellow, 18. 1 % red and pink, type makes up 75.3%, the Sun-shrubs type 16.8% and the Alpine-shrubs type 7.9%. The spieces of the Sun-shrubs type are introduced and used most easily. Yellow Peony, Hookers St. John'swort, Rockspray Cotoneaster, Largeflower Jasmine, Big Cupress and so on must be exploited first, as they are introduced easily and their ornamental value is very high.
钦杭成矿带南段云浮硫铁矿黄铁矿微组构特征及其对矿床成因的启示
Micro-fabric characteristics of pyrite generations and their implications for genesis of Yunfu pyrite deposit, Qinzhou-Hangzhou metallogenetic belt,South China
 [PDF]

郭晓昱,郑义,周永章,牛佳,虞鹏鹏
GUO Xiaoyu
,ZHENG Yi,ZHOU Yongzhang,NIU Jia,YU Pengpeng

- , 2017,
Abstract: 云浮硫铁矿是位于钦杭结合带南段的超大型硫铁矿床,长期以来对其成因类型及成矿构造背景存在争议。基于矿床地质和岩相矿相学观察,应用最新的扫描电镜能谱技术(SEM-EDS)对其进行了细致研究。研究表明,云浮硫铁矿床黄铁矿矿石结构可分为条带状、浸染状、块状和脉状4种类型。手标本及镜下观察发现,条带状矿石存在揉皱构造,块状矿石中存在两种不同粒度的黄铁矿,黄铁矿细脉普遍存在于各种矿石中。扫描电镜观察和能谱分析显示,条带状矿石中黄铁矿主要呈立方体自形晶,立方体表面生长层发育平整,边缘平直,晶体按照多个层位同时堆积的方式生长,方铅矿等伴生矿物晶形也较好;浸染状矿石中黄铁矿粒度要大于条带状矿石中黄铁矿,但生长层不如后者平整;块状矿石中黄铁矿紧密接触,黄铁矿表面呈贝壳状断口,晶体边缘较难分辨,但样品表面也常见到近八面体晶形的晶体;脉状矿石中黄铁矿粒度较大,伴生有方铅矿等金属矿物,但由于生长空间的限制,晶形为半自形-他形。认为云浮硫铁矿具有2期叠加成矿的特点,为改造加富的热水喷流沉积矿床。喷流沉积阶段形成条带状和浸染状黄铁矿,其成矿温度较低,成矿环境相对平静。后期热液叠加富集阶段形成块状和脉状黄铁矿,其成矿温度较高
英雄一世,学者一生--纪念吴杭生院士  [PDF]
沈电洪
物理 , 2004,
Abstract: ?纪念吴杭生院士
Threatened and Rare Ornamental Plants  [PDF]
Korous Khoshbakht,Karl Hammer
Journal of Agriculture and Rural Development in the Tropics and Subtropics , 2007,
Abstract: The application of IUCN criteria and Red List Categories was done for ornamental plants. Main sources of the study were Glen’s book, Cultivated Plants of Southern Africa (Glen, 2002) and the Red List of Threatened Plants, IUCN (2001). About 500 threatened ornamental plants could be found and presented in respective lists. Rare ornamental plants with 209 species is the largest group followed by Vulnerable (147), Endangered (92), Indeterminate (37), Extinct (6) and finally Extinct/Endangered groups with 2 species. A weak positive correlation (r = +0.36 ) was found between the number of threatened species and the number of threatened ornamental species within the families.
Geochronology and geochemistry of Early Mesozoic acid volcanic rocks from Southwest Guangxi: Constraints on tectonic evolution of the southwestern segment of Qinzhou-Hangzhou joint belt.
桂西南早中生代酸性火山岩年代学和地球化学:对钦-杭结合带西南段构造演化的约束

QIN XiaoFeng,WANG ZongQi,ZHANG YingLi,PAN LuoZhong,HU GuiAng,ZHOU FuSheng,
覃小锋
,王宗起,张英利,潘罗忠,胡贵昂,周府生

岩石学报 , 2011,
Abstract: Early Mesozoic acid volcanic rocks are exposed dominantly in the southwestern segment of Qinzhou-Hangzhou joint belt, and are mainly distributed in both sides of the Shiwandashan Mesozoic-Cenozoic basin. The volcanic rocks of Lower and Middle Triassic Beisi Formation are exposed in northwest side of the basin, which consists of alternating volcanic succession of felsic lavas (basaltic andesite-dacite-rhyolite) interlayered with pyroclastic rocks (dominantly agglomerate lava, breccia lava, tuffolava, breccia...
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