Hydrology of Dali Lake in central-eastern Inner Mongolia and Holocene East Asian monsoon variability   总被引：12，自引：1，他引：11  

Jule Xiao  Bin Si  Dayou Zhai  Shigeru Itoh  Zaur Lomtatidze 《Journal of Paleolimnology》2008,40(1):519-528

Lacustrine records from the northern margin of the East Asian monsoon generate a conflicting picture of Holocene monsoonal precipitation change. To seek an integrated view of East Asian monsoon variability during the Holocene, an 8.5-m-long sediment core recovered in the depocenter of Dali Lake in central-eastern Inner Mongolia was analyzed at 1-cm intervals for total organic and inorganic carbon concentrations. The data indicate that Dali Lake reached its highest level during the early Holocene (11,500–7,600 cal yr BP). The middle Holocene (7,600–3,450 cal yr BP) was characterized by dramatic fluctuations in the lake level with three intervals of lower lake stands occurring 6,600–5,850, 5,100–4,850 and 4,450–3,750 cal yr BP, respectively. During the late Holocene (3,450 cal yr BP to present), the lake displayed a general shrinking trend with the lowest levels at three episodes of 3,150–2,650, 1,650–1,150 and 550–200 cal yr BP. We infer that the expansion of the lake during the early Holocene would have resulted from the input of the snow/ice melt, rather than the monsoonal precipitation, in response to the increase in summer solar radiation in the Northern Hemisphere. We also interpret the rise in the lake level since ca. 7,600 cal yr BP as closely related to increased monsoonal precipitation over the lake region resulting from increased temperature and size of the Western Pacific Warm Pool and a westward shifted and strengthened Kuroshio Current in the western Pacific. Moreover, high variability of the East Asian monsoon climate since 7,600 cal yr BP, marked by large fluctuations in the lake level, might have been directly associated with variations in the intensity and frequency of the El Niño-Southern Oscillation (ENSO) events.  相似文献   

Period changes and photometric solution of AP Leonis     

Zhang Ji-tong  Zhang Rong-xian  Zhai Di-sheng 《Chinese Astronomy and Astrophysics》1992,16(4):407-415

The results of BV photometry of AP Leonis are presented. Photometric analysis is carried out by using the Wilson-Devinney program. The solution shows that the system is an over-contact binary with an over-contact degree of 23.5% and its mass ratio q equal to 0.301. A starspot group is found in the low latitude region on the secondary component. The average temperature of the spot is about 1220 K lower than that of surrounding photosphere.

The light minimum times observed over ninety years are collected. The O-C curve of minima reveals that the period of AP Leo changes with the time in a pseudo-sinusoidal pattern and there is probably a third body in the system.  相似文献   

深部找矿研究问题   总被引：69，自引：7，他引：62  

翟裕生  邓军  王建平  彭润民  刘家军  杨立强 《矿床地质》2004,23(2):142-149

中国大部分矿产资源供应的紧缺形势,要求加大中东部地区深部找矿(包括矿山和矿集区)的力度。文章在论述深部找矿的重要性、可能性和艰巨性的基础上,阐释了深部找矿的有关概念,对比了深部矿床和浅表矿床的差异,重点论述了深部探矿的4个基本科学问题,包括：①成矿系统发育的完整程度;②成矿系统发育的深度;③成矿系统网络的三维结构与矿床分带;④深部矿床的示踪标志。最后,作者对加强深部找矿提出了意见和建议。  相似文献   

几种亚洲季风指数与中国夏季主要雨型的关联   总被引：5，自引：0，他引：5       下载免费PDF全文

江滢  翟盘茂 《应用气象学报》2005,16(Z1):70-76

首先采用EOF方法分析了中国夏季降水的主要特征 ,其第一 (EOF1 )和第二 (EOF2 )特征向量及其时间序列 (EOF1 - T、EOF2 T)基本上反映了中国夏季 1 (或 3)类和 2类主要雨型的空间和时间分布 ;进一步建立了EOF1、EOF2及其对应的时间序列EOF1 - T、EOF2- T与季风指数的关联 ,以及中国夏季主要雨型与季风指数直接的关联。结果表明 :各季风指数都对中国夏季的 1类雨型有较好的反映能力 ,都对 2类雨型无反映能力 ,仅学者施能定义的指数对 3类雨型有一定的反映能力。  相似文献   

广东三水盆地古近系心组生油层的元素地球化学特征   总被引：5，自引：0，他引：5       下载免费PDF全文

刘春莲  秦红  车平  翟伟  石贵勇  周永章  谢叶彩  董艺辛 《古地理学报》2005,7(1):125-136

沉积物的元素地球化学特征是对沉积盆地水体环境以及古气候条件变化的响应。本文根据元素（Al、Fe、Mg、Ca、K、Na、P、V、Ni、Co、Cr、Cu、Zn、Sr、Ba、Cd、Li、Mn、Pb、Ti）的含量及其比值（Al/Ti、Fe/Mn、Sr/Ba、Mg/Ca、Sr/Ca、Na/Ca、V/Cr、Ni/Co、Ni/V）的变化，对三水盆地古近系心组红岗段生油层的沉积条件进行了系统分析。心组红岗段下部（亚段A）表现为较稳定的地球化学特征。各元素丰度及其比值指示这一时期陆源输入持续较高、且物源组成变化不大。由于海水入侵的影响，湖盆水体盐度相对较高，底部水体以弱氧化条件为主，O₂-H₂S界面位于水/沉积物界面附近。红岗段中上部（亚段B、C）的元素地球化学特征变化较为频繁且幅度很大，反映古气候和湖盆沉积条件的迅速变迁。在潮湿气候条件下，沉积物的地球化学特征表现为以Al、Ti为代表的外源元素含量及其比值较高，而Mg、Ca等盆内化学沉积元素含量较低。古氧气指标指示底部水体为还原环境，有利于有机质保存。因而，相应于较高的有机碳含量。在间歇性干旱时期，陆源输入减少，外源元素含量及其比值显著降低。随着蒸发作用的加强，水体盐度加大，内源元素丰度以及Mg/Ca、Sr/Ba、Sr/Ca和Na/Ca比值大幅度上升。底部水体为氧化环境，O₂-H₂S界面多位于水/沉积物界面或沉积物中。上述两种气候条件在红岗段中上部沉积时期交替出现。红岗段沉积后期由于淡水的长期输入，湖水出现逐渐淡化趋势。  相似文献   

近年秋季南美沿岸海表温度周期性下降对ＥＮＳＯ事件的可能影响     

李威  翟盘茂 《气象》2007,33(2):29-33

文章分析了1950年以来赤道南美沿岸海表温度变化特点，发现1999年以来，Nino1＋2区海表温度的年变化振幅呈增大趋势，使得赤道东太平洋东北地区每年出现周期性降温，这主要是由秋季月平均SST最低值偏低造成，这种长时间持续偏低是1950年以来首次出现。进一步的分析表明，近年来南美沿岸海表温度在秋季的周期性下降可能对ENS0暖事件发生产生了影响，使得2002／2003ENS0暖事件成为20世纪50年代以粜由玲事件向瞎事件转换历时最长的一次．  相似文献   

气候变化国家评估报告(Ⅰ):中国气候变化的历史和未来趋势   总被引：7，自引：0，他引：7  

丁一汇  任国玉  石广玉  Gong Peng  Zheng Xunhua  Zhai Panmao  Zhang De'er  Zhao Zongci  Wang Shaowu  Wang Huijun  Luo Yong  Chen Deliang  Gao Xuejie  Dai Xiaosu 《气候变化研究进展》2007,3(Z1):1-5

The climate change in China shows a considerable similarity to the global change, though there still exist some significant differences between them. In the context of the global warming, the annual mean surface air temperature in the country as a whole has significantly increased for the past 50 years and 100 years, with the range of temperature increase slightly greater than that in the globe. The change in precipitation trends for the last 50 and 100 years was not significant, but since 1956 it has assumed a weak increasing trend. The frequency and intensity of main extreme weather and climate events have also undergone a significant change. The researches show that the atmospheric CO2 concentration in China has continuously increased and the sum of positive radiative forcings produced by greenhouse gases is probably responsible for the country-wide climate warming for the past 100 years, especially for the past 50 years. The projections of climate change for the 21st century using global and regional climate models indicate that, in the future 20-100 years, the surface air temperature will continue to increase and the annual precipitation also has an increasing trend for most parts of the country.  相似文献   

1-D and 2-D analyses of weak motion data in Fraser Delta from 1966 Duvall earthquake     

W. D. Liam Finn  E. Zhai  T. Thavaraj  X. -S. Hao  C. E. Ventura 《Soil Dynamics and Earthquake Engineering》2003,23(4):323-329

The 1996 Duvall earthquake in Washington State triggered ground motion stations in the Fraser Delta, British Columbia, located on varying depths of Holocene and Pleistocene soils to a maximum depth of 800 m and one station on bedrock. Recorded ground motions were used to examine the applicability of 1-D and 2-D site response analyses for amplification studies in the Delta. 1-D response analysis gave a good indication of the period of peak response. Response spectra computed by 1-D analysis did not compare well with recorded spectra except at very deep sites. The use of 2-D analyses to include buried topography generally improved the predictions of site response spectra at the shallow sites. However, for the shallow earth sites, the recorded motions showed a strong spectral response at short periods in the range of 0.1–0.25 s. Neither 1-D nor 2-D analysis predicted this response.  相似文献   

A new type of interaction between generalized Chaplygin gas and dark matter     

Y. D. Xu  Z. G. Huang  X. H. Zhai 《Astrophysics and Space Science》2012,339(1):31-36

In this paper, we investigate the model with a new type of interaction between generalized Chaplygin gas (GCG) and dark matter. It is shown that there exists a stable scaling attractor, which provides the possibility to alleviate the coincidence problem. The equation of state (EoS) of GCG approaches the attractor phase from either w _g >?1 or w _g w _g w _g w _g >?1), and next cross again the phantom divide (the transition from w _g >?1 to w _g Q can change its sign from Q<0 to Q>0 as the universe expands, which is different from the usual interaction. Moreover, we investigate the model from statefinder viewpoint. The statefinder diagnostic can not only discriminate the model with different coupling constant but also distinguish the model from other dark energy models.  相似文献   

Study on Effects of Low Viscosity Fluid Pre-injection on Hydraulic Fracture Complexity in Tight Heterogeneous Glutenite Reservoirs     

Zhang  Liaoyuan  Qu  Zhanqing  Zhai  Mingyang  Li  Aishan  Huang  Bo  Zhang  Zilin 《Geotechnical and Geological Engineering》2021,39(2):839-854

Tight heterogeneous glutenite reservoir is typically not easy to form complex hydraulic fracture (HF) due to its poor physical properties, poor matrix seepage capacity, and small limit discharge radius and undeveloped natural fracture system. To improve the HF complexity and the stimulated reservoir volume (SRV), a novel stimulation technology called CO₂ miscible fracturing has been introduced and its fracturing mechanism has been studied. The CO₂ miscible fracturing modifies the in situ stress field by injecting low viscosity fluid to increase the HF complexity and SRV. Therefore, a series of numerical simulations based on a hydro-mechanical-damage model were carried out to study the effects of low viscosity fluid pre-injection on pore pressure, stress field, and fracturing effect in tight heterogeneous glutenite reservoirs. The results indicate that the low viscosity fluid injection can effectively increase the pore pressure around the wellbore and reduce the effective stress of the glutenite. The FCI and SRV increase with the increase of the pre-injection amount of the low viscosity fluid. The HF complexity and SRV can be improved by pre-injecting low viscosity fluid to transform the in situ stress field. The field application of this technology in a well of Shengli Oilfield showed that low-viscosity fluid pre-injection can effectively increase the width of the fractured zone, improve the SRV, and optimize the fracturing effect.

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