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61.
马家塬战国墓地是研究西戎文化以及秦戎文化交流的重要考古遗址。在M21墓葬发现了一些附着于铁器表面的矿化纺织品残片。这些矿物外壳保留了比较完整的纺织品形态,是研究早期纺织技术的宝贵资料。为此,本研究采用扫描电子显微镜(SEM)和高效液相色谱-质谱联用技术(HPLC-MS)对矿物纺织品残片的纤维原料进行了鉴定与分析:1)矿物外壳内部的纤维空洞结构形态与桑蚕丝的纤维形态特征相同;2)样品中检出了3组蚕丝蛋白的特征多肽片段。研究结果表明,M21墓葬中的纺织品残片的原料为蚕丝纤维(Bombyx mori)。丝绸的发现表明中原的丝绸成品或者纤维原料已经进入西戎地区,西戎与中原文明的交流更加密切。使用丝绸包裹铁器则表明西戎文化已经受到了一些中原风俗的影响。这一发现填补了马家塬遗址中纺织品研究的空白,不仅为研究秦戎地区的织造工艺和文化交流提供了重要资料,也为矿化纺织遗存中的桑蚕丝残留的鉴定提供了技术支持。  相似文献   
62.
长江三角洲技术扩散规律及其对策初探   总被引:12,自引:1,他引:12  
技术扩散已经成为决定区域高新技术产业乃至区域经济可持续发展的重要因素,从时间尺度上看,区域技术扩散速度呈现\"S\"型分布。本文论述了我国经济技术较为发达的长江三角洲地区的技术扩散历程、态势、不同等级的技术扩散中心,在此基础上,提出了提高认识、建立区域技术扩散体系,发挥企业主体作用等促进技术扩散的对策建议。  相似文献   
63.
汉阳陵帝陵从葬坑遗址保护展示厅常年的高湿度环境(空气相对湿度为95%±5%)容易使遗址文物发生霉变等病害。为此本研究以从葬坑遗址保护展示厅15号坑为研究对象,根据基本假设,建立了从葬坑文物保存区域空气流动的二维数学模型,并采用标准k-ε两方程湍流模型和SIMPLE算法进行了数值计算。研究了风幕送风速度和送风仰角对风幕隔离性能的影响,并确定了15号坑适宜的送风速度为1.5m/s、送风仰角为10°。研究结果对高湿环境下如何营造风幕隔离及富氮低氧环境提供了依据,对坑式遗址文物保护具有重要意义。  相似文献   
64.
    
The high speed railway (HSR) has played a crucial role in the regional integration of urban networks in China. This paper analyses HSR passenger flows instead of commonly‐used time schedules for measuring different polycentricity in urban networks. Using 2013 origin/destination (O/D) passenger flow data, we analyse the spatial configurations of 99 HSR cities at the national scale in China. In addition, we compare the spatial configurations of three regional urban networks: the Pearl River Delta, the Yangzi River Delta and the Bohai Rim. The outcomes show that the three functional regions connected by HSR are the most dominant polycentric regions in China and that the Bohai Rim is less hierarchical than the other two. We conclude that the comprehensive Chinese HSR networks are largely polycentric, especially in the central and eastern regions.  相似文献   
65.
    
High-Impact Educational Practices (HEPs) are a set of specific teaching and learning approaches proven effective in university education. This paper focuses on the benefits derived from utilizing three particular HEPs (inquiry-based collaborative activities, undergraduate research, and experiential learning) while teaching a snow and ice field course titled “Silverton Field Experience.” Student evaluations and instructor feedback reinforce the notion that HEPs encourage deep learning. Deep learning is manifest through increased enthusiasm and participation as well as learning in ways that are meaningful, creative, and stimulating. In terms of pedagogy in geography, these HEPs also create an expanded sense of place and a new way to encourage spatial thinking. The HEPs outlined here are replicable in different geography sub-disciplines and among different settings in higher education and prove exciting to an audience of pedagogic researchers and teacher-practitioners in geographical education.  相似文献   
66.
To assess the analytical accuracies and precisions of archaeometric elemental analyses by different techniques, a relatively homogeneous material such as obsidian must be studied. An assessment of published elemental concentration data from two Anatolian obsidian sources shows that while in most cases analytical accuracy is as high as is commonly expected, in some cases it is not. It also shows that the dispersions of elemental concentration data (indicators of analytical precisions) coming from modern analytical procedures are akin to the estimated homogeneity of the obsidian. Based on this latter observation, if one has element dispersion data from a single analytical technique, with a single source of obsidian as a control, data sets that contain multiple, but similar sources of obsidian may be differentiated.  相似文献   
67.
宋代熙宁年间,着力通过市易法、募役法等解决国家的财政收入问题,进而在国家行政体系的改革中推行增加吏禄、以重法治赃的"重禄法"(亦称"仓法",因首先推行自仓吏)。而市易法的收入是"重禄"的直接经济来源。实行"重禄法"以治吏惩贪,一定程度上遏制了吏的卖法弄权。由于熙宁改革的破产,重禄法难以广泛推行,并在元祐初年被名义上废止,但其以"重禄人"的形式至少推延至南宋绍兴年间;吏之有禄成为行政惯例,延续到南宋。重典治吏的思想则贯穿于宋王朝的始终。  相似文献   
68.
韩岩 《攀登》2011,30(2):130-132
开架借阅是图书馆工作的发展方向,它使图书馆在服务社会方面发挥了积极的作用,但是开架借阅所带来的诸多问题是图书馆管理工作的一大难题。本文通过对存在问题的分析,提出了一些具体的对策。  相似文献   
69.
It is widely recognized that new technologies can play an important role in the interpretation of our cultural heritage legacy. This has become a powerful tool providing a better understanding of our past, and thereby, allowing us to attain a glimpse of the environments in which our ancestors lived. In this domain, the way we see such reconstructed environments is particularly important in order to establish an accurate interpretation of that historical setting. However, the desired visual accuracy in the representation of any archaeological scenario is strictly related to the technology used to visualize it. High Dynamic Range (HDR) technology encompasses the capacity to produce visual results similar to the visual acuity of the human eye, particularly in extreme lighting conditions, such as bright light or dim environments.  相似文献   
70.
    
J. X. LI  G. M. LI  K. Z. QIN  B. XIAO 《Geofluids》2011,11(2):134-143
The Duobuza porphyry copper–gold deposit (proven Cu resources of 2.7 Mt, 0.94% Cu and 13 t gold, 0.21 g t?1 Au) is located at the northern margin of the Bangong‐Nujiang suture zone separating the Qiangtang and Lhasa Terranes. The major ore‐bearing porphyry consists of granodiorite. The alteration zone extends from silicification and potassic alteration close to the porphyry stock to moderate argillic alteration and propylitization further out. Phyllic alteration is not well developed. Sericite‐quartz veins only occur locally. High‐temperature, high‐salinity fluid inclusions were observed in quartz phenocrysts and various quartz veins. These fluid inclusions are characterized by sylvite dissolution between 180 and 360°C and halite dissolution between 240 and 540°C, followed by homogenization through vapor disappearance between 620 and 960°C. Daughter minerals were identified by SEM as chalcopyrite, halite, sylvite, rutile, K–feldspar, and Fe–Mn‐chloride. They indicate that the fluid is rich in ore‐forming elements and of high oxidation state. The fluid belongs to a complex hydrothermal system containing H2O – NaCl – KCl ± FeCl2 ± CaCl2 ± MnCl2. With decreasing homogenization temperature, the fluid salinity tends to increase from 34 to 82 wt% NaCl equiv., possibly suggesting a pressure or Cl/H2O increase in the original magma. No coexisting vapor‐rich fluid inclusions with similar homogenization temperatures were found, so the brines are interpreted to have formed by direct exsolution from magma rather than trough boiling off of a low‐salinity vapor. Estimated minimum pressure of 160 MPa imply approximately 7‐km depth. This indicates that the deposit represents an orthomagmatic end member of the porphyry copper deposit continuum. Two key factors are proposed for the fluid evolution responsible for the large size of the gold‐rich porphyry copper deposit of Duobuza: (i) ore‐forming fluids separated early from the magma, and (ii) the hydrothermal fluid system was of magmatic origin and highly oxidized.  相似文献   
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