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71.
陆彦邦 《安徽理工大学学报(自然科学版)》1992,(2)
本文讨论了中国南方二叠纪含煤岩系沉积特征、沉积类型、含煤性及聚煤规律。着重探讨了古构造及岩相古地理与聚煤作用的关系。三角洲平原及潮坪——泻湖是中国南方二叠纪最重要的聚煤环境。富煤带往往分布于次级坳陷或隆起与坳陷的斜坡部位,同时也受同沉积断裂的制约。 相似文献
72.
本文在统计华南登陆台风暴雨的基础上,着重对8107号台风登陆后的强度变化及其暴雨过程进行了诊断研究.结果表明,华南登陆台风及其降水的强度变化主要取决于水汽输送条件的变化,Q_1、Q_2的变化则表明,积云对流及其潜热加热的反馈作用是登陆台风及其暴雨维持和加强的主要机制. 相似文献
73.
略论美国历史上的牛仔与牛仔文化 总被引:3,自引:0,他引:3
李青 《杭州师范学院学报(社会科学版)》2004,(1):89-92,98
19世纪后期在美国中西部大草原上营造"牧牛王国"的牛仔们,其劳动生活之艰苦卓绝令人叹为奇观.至于好莱坞西部片中的浪漫放荡、好勇斗狠的牛仔形象,虽为世人津津乐道,其实不过是牛仔文化的误读而已.持续仅1/4月世纪的牛仔时代,何以生发具有恒久魅力的牛仔文化,确是美国文化史上一个值得探究的课题. 相似文献
74.
对中美两国社会力量设奖的历史与现状进行了系统考察,通过对比分析,认为二者在4个方面有相似之处,包括设奖者以专业学会为主、奖励范围以单个学科为主、奖励对象以个人为主、物质奖励和精神奖励相结合等;同时也存在5个方面的主要区别,包括社会力量设奖的影响力、国际奖的数量、对社会力量设奖的管理、资金来源、评审机制等。在此基础上,对如何推动中国社会力量设奖的健康发展提出了看法。 相似文献
75.
南海北部大陆架海洋生态系统Ecopath模型的应用与分析 总被引:8,自引:1,他引:8
过度捕捞和环境恶化导致渔业资源和海洋生态系统逆向发展。采用EwE5.1软件,对南海北部大陆架建立Ecopath(生态通道模型)模型。通过各级流量、生物量、生产量、捕捞量、系统总流量以及生态位和混和营养效应等方面的分析,得出营养流通主要有2种途径,肉食鱼类间饵料竞争非常激烈,低值鱼类间具相似的捕食压力,顶级捕食者对大部分鱼类负效应不明显。系统受过度捕捞渔业影响很大,并存在营养级I利用效率低和渔业资源小型化、低值化等不稳定的幼态特征。 相似文献
76.
HUANG BaoQi JIAN ZhiMin WANG PinXian 《科学通报(英文版)》2007,52(6):839-843
Quantitative analysis of benthic foraminifera from ODP Site 1146 in the northern South China Sea (SCS) shows that abundance of Bulimina alazanensis, sometimes up to about 90%, decreased gradually since 3.2 Ma, especially at 2.1 Ma. Abundance of other benthic foraminiferal species, Globobulimina sub-globosa and Cibicidoides wuellerstorfi, increased after 2.1 Ma. Comparison with changes in oxygen and carbon isotopes of planktonic and benthic foraminifera shows that high abundance values of B. alazanensis corresponded with lower values of oxygen isotope, but for carbon isotope, high values of the species were consistent with heavier carbon isotope of benthic foraminifera and lighter carbon isotope of planktonic foraminifera, respectively, and vice versa. Considering factors such as uplift of Bashi Strait, expansion of the North Hemisphere Glaciation, strengthening of East Asian winter mon-soon and variations in oxygen and carbon isotope of foraminifera, changes of B. alazanensis in ODP Site 1146 suggest that the source of deep water masses of the northern South China Sea changed from the warm Pacific deep water with high oxygen content to Pacific Intermediate water with low oxygen content at 2.1 Ma. In addition, the strengthened East Asian winter monsoon resulted in increased pri-mary productivity, high nutrient and suboxic bottom water. Variations in species of B. alazanensis seemed to be unable to tolerate environmental stress induced by deep water masses and productivity changes. 相似文献
77.
Coupling and propagating of mesoscale sea level variability between the western Pacific and the South China Sea 总被引:4,自引:0,他引:4
LI Li JING ChunSheng ZHU DaYong 《科学通报(英文版)》2007,52(12):1699-1707
The coupling and propagating features of mesoscale sea level variability between the western Pacific (WP) and the South China Sea (SCS) were studied based on time series analyses of satellite altimeter measured, along-track sea surface height anomalies (SSHA) along 21°N and the slope of the northern SCS. The analyses show that mesoscale sea level fluctuations in the WP have rather limited coherent effects on the SCS, and no statistically significant propagation of mesoscale variability through the Luzon Strait was observed except in the 45-day band. Evidence suggests that the 45-day fluctuation is very much likely a character of the Kuroshio originating from its low-latitude beginning. It is also sug- gested that the westward propagating Rossby waves will deform when they encounter the dynamical barrier of the Kuroshio. The Kuroshio will then acts on the SCS in its own way. The SCS is a relatively isolated system in the sense of coupling and propagating of oceanic mesoscale waves. 相似文献
78.
PU XiaoQiang ZHONG ShaoJun YU WenQuan TAO XiaoWan 《科学通报(英文版)》2007,52(3):401-407
This is a report of the study of the authigenic sulfide minerals and their sulfur isotopes in a sediment core (NH-1) collected on the northern continental slope of the South China Sea, where other geo-physical and geochemical evidence seems to suggest gas hydrate formation in the sediments. The study has led to the findings: (1) the pyrite content in sediments was relatively high and its grain size relatively large compared with that in normal pelagic or hemipelagic sediments; (2) the shallowest depth of the acid volatile sulfide (AVS) content maximum was at 437.5 cm (>2 μmol/g), which was deeper than that of the authigenic pyrite content maximum (at 141.5-380.5 cm); (3) δ 34S of authigenic pyrite was positive (maximum: 15‰) at depth interval of 250-380 cm; (4) the positive δ 34S coincided with pyrite enrichment. Compared with the results obtained from the Black Sea sediments by Jorgen-sen and coworkers, these observations indicated that at the NH-1 site, the depth of the sulfate-methane interface (SMI) would be or once was at about 437.5-547.5 cm and the relatively shallow SMI depth suggested high upward methane fluxes. This was in good agreement with the results obtained from pore water sulfate gradients and core head-space methane concentrations in sediment cores collected in the area. All available evidence suggested that methane gas hydrate formation may exist or may have existed in the underlying sediments. 相似文献
79.
阐述基于CPS标准的南方电网联络线功率与频率偏差的控制模式和考核办法,分析目前南方电网CPS考核情况和存在的问题,并从AGC的管理、控制策略、运用方法以及调度员调节等方面提出一系列有利于提高南方电网的CPS考核水平和频率质量的建议. 相似文献
80.