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32.
总结了上海浦东机场二期飞行区3种不同组合的冲击碾压试验——冲击碾压联合高真空排水、冲击碾压联合塑料排水板、冲击碾压，试验结果表明，冲击碾压联合高真守排水方法压实效果最为显著，并在二期飞行区浅层地基处理实践中得到应用。 相似文献
33.
A thermohaline front is located at the southeastern entrance of the Yellow Sea in winter, and it is generated by the intrusion of warm saline water into the Yellow Sea caused by a strong northerly wind. Recently, a westward transversal current traveling away from the west coast of Korea toward the open sea area along the front was reported. The westward transversal current is dominant in the surface layer during the temperature inversion period. The formation and structure of this current are examined using a numerical vertical ocean-slice model. When two different water masses meet, a front is formed and adjusted geostrophically. In this frontal zone, a horizontal pressure gradient flow by the vertically inclined isopycnal occurs under the thermal wind process in a baroclinic effect, and the cold fresh coastal water moves westward along the front in the upper layer. The barotropic effect across the front and the bottom friction effect strengthen the westward component of the velocity. The velocity of the bottom layer decreases remarkably in the increase of the bottom drag coefficient. This means that the bottom friction with the strong background tidal current causes a reduction in the current in the bottom layer. 相似文献
34.
THEUTILIZATIONOFCHITINANDCHITOSANINDETERMINGTHECONTENTOFTRACECUPRICION测定铜含量的方法有多种,如二乙氨基二硫代甲酸钠,原子吸收分光光度法等。几丁质（缩写为CT）广泛地存在于动植物中,它是一种天然的大分子含氮多糖化合物,是β-1,4连接的乙酰氨基葡聚糖,它具有吸附离子的能力,能富集金属离子,故对水的净化具有应用潜力[1]。近年来国人对CT的研究日渐增多,在食品、医药、环保、农业、造纸、印染、日用化工以及酶制剂等方面,已陆续见诸报道。自然界甲壳质产量达100×108t,但实际用量仅2000t… 相似文献
35.
Comments on ``Direct Radiative Forcing of Anthropogenic
Aerosols over Oceans from Satellite Observation" 总被引：1，自引：0，他引：1
Previous observational studies have estimated anthropogenic aerosol direct radiative forcing over oceans without due consideration of cloudy-sky aerosols.However,when interaction between clouds and aerosols located below or above the cloud level is taken into account,the aerosol direct radiative forcing is larger by as much as 5 W m-2 in most mid-latitude regions in the Northern Hemisphere. 相似文献
36.
在对世界著名的维特瓦特斯兰德矿床成因讨论中，存在着2种主要观点：热液交代说和砂积成因说。后者经过补充、修改演变为改造砂矿成因说。最近，加拿大地质学家Reimer和Mossman代表后一种观点撰文，概括了近年来争论的焦点，回答了热液成因论者的质疑。 相似文献
37.
YU Bingsong DONG Hailiang CHEN Jianqiang LI Xingwu LIN Changsong State Key Laboratory of Geological Processes Mineral Resources China University of Geosciences Beijing Chin Key Laboratory of Lithosphere Tectonics Lithoprobing Technology of Ministry of Education China University of Geosciences Beijing China Department of Geology Miami University Oxfor OH USA 《《地质学报》英文版》2005,79(2):215-224
The sedimentary sequence of the Lower Cambrian is a key interval to reveal the early evolution history of the Earth and there occur widespread cherts worldwide. These cherts possibly carry important information to decipher the breakup process of the Rodinia Continent. Black rock series at the bottom of the Lower Cambrian in the Northern Tarim Basin, China, is composed of black shales interbedded with thin-bedded cherts. Ten chert samples were systematically collected from two outcrops at Xiaoerbulak and Sogatbulak, 8.8 and 7.5 m thick respectively. The cherts were crushed, and were analyzed for trace element and rare earth concentrations. Trace elements such as V, Cu, Zn, U, Pb, Ba, Cd, Ag, Mo,As and Sb are highly enriched, and others such as Rb, Zr, Cs, Hf, Ta, W, T1, Bi and Th are highly depleted in the cherts.These trace element patterns suggest that the cherts may be of deep crustal origin. The low ratios of Th/U and Rb/Sr further suggest that the cherts are of earth interior sources or received hydrothermal input during their deposition. Chondritenormalized Eu/Eu* value markedly decreases upward in the section from 5.54 at the lowermost to 0.73 at the top, and NASC-normalized Eu/Eu* value decreases from 8.05 to 1.03. The relatively high Eu/Eu* ratio for the cherts from the northern Tarim Basin is most likely due to a hydrothermal input (e.g., Eu/Eu*-10). The systematic decrease of Eu/Eu* ratio from the bottom to the top of the section reflects that the hydrothermal input is the largest in the lowermost portion of the section and gradually decreases upward. The chondrite-normalized Ce/Ce* ratio ranges from 0.42 to 0.83, with an average of 0.60. North American Shale Composite (NASC)-normalized Ce/Ce* ratio ranges from 0.42 to 0.79, with an average of 0.57. Negative Ce anomalies are distinct. EREEs in the cherts generally increase from 10.50 ppm at the bottom to 35.97 ppm at the top of the sampled section. NASC-normalized (La/Lu)N ratio decreases from 2.72 at the bottom to 0.67 at the top. NASC-normalized (La/Ce)N ratio increases from 1.36 at the bottom to 3.13 at the top. These REE patterns are very similar to those for the cherts deposited in the pelagic ocean-basin floor in the Franciscan Complex exposed at Marin Headlands, California (F-MH chert) (Murray et al., 1991). These geochemical signatures are inconsistent with our previous sedimentological data, which suggests a continental shelf setting. Based on multiple lines of evidence including high TOC content in the concomitant black shales, phosphorite at the bottom of black rock series, regional rise of sea level,and beginning of the southern Tianshan Ocean geotectonic cycle, the authors infer that the hydrothermal fluid was carried to the continental shelf by upwelling from a divergent pelagic ocean floor setting. 相似文献
38.
以资源——资源生态——资源经济科学的理论为基础,对青海省土地资源人口承载力系统条件的综合分析,针对各类资源之间的平衡关系、农业结构与资源结构的匹配关系、单产潜力的预测与总生产潜力的仿真,进行人口与资源关系的综合研究,建立该地区土地资源人口承载力的动态模型。 相似文献
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