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81.
The aerosol number spectrum and gas pollutants were measured and the new particle formation (NPF) events were discussed in Nanjing. The results showed that the size distributions of aerosol number concen- trations exhibited distinct seasonal variations, implying the relations of particle sizes and their sources and sinks. The number concentrations of particles in the nuclei mode (10-30 nm), Aitken mode (30-100 nm), accumulation mode (100 -1000 nm) and coarse mode (〉1μm) varied in the order of summer 〉 spring 〉 autumn, summer 〉 autumn 〉 spring, autumn 〉 summer 〉 spring, and spring 〉 autumn 〉summer, re- spectively. The diurnal variation of total aerosol number concentrations showed three peaks in all observed periods, which corresponded to two rush hours and the photochemistry period at noon. In general, the NPF in summer occurred under the conditions of east winds and dominant air masses originating from marine areas with high relative humidity (50%-70%) and strong solar radiations (400 -700 W m-2). In spring, the NPF were generally accompanied by low relative humidity (14%-30%) and strong solar radiations (400-600 W m-2). The new particle growth rates (GR) were higher in the summertime in the range of 10- 16 nm h-1. In spring, the GR were 6.8-8.3 nm h-1. Under polluted air conditions, NPF events were seldom captured in autumn in Nanjing. During NPF periods, positive correlations between 10- 30 nm particles and 03 were detected, particularly in spring, indicating that NPF can be attributed to photochemical reactions. 相似文献
82.
利用黑龙江省1981-2010年的土壤湿度数据,以富锦县、龙江县、双城县、黑河市、海伦县为代表点,分析了黑龙江省东、西、南、北、中各区域封冻前(11月8日)0~30 cm土层土壤湿度的趋势变化和干湿变化,采用线性趋势、5年滑动平均和Mann-Kendall法检验变化趋势,利用Mann-Kendall和Yamamoto法对土壤湿度变化趋势进行突变点检验.结果表明:封冻前0~30 cm土层各地土壤湿度在30年间均有不同程度下降,西部龙江县下降剧烈,中部海伦县较剧烈,北部黑河市和南部双城县次之,上述代表点20 cm土层土壤湿度下降均达到了P<0.05以内的显著水平,东部富锦县下降趋势最弱;经Mann-Kendall法检验,0~30 cm土层龙江县、海伦县土壤湿度出现了下降的突变区域,其余代表点的土壤湿度变化趋势在近几年中逐渐接近或已经超越了显著线;1994年是龙江县10 cm、20 cm土壤湿度下降的突变时期;黑龙江省各地土壤湿度的下降与封冻前一段时期内气温和降水变化密切相关,还与土壤物理性质的恶化等因素有关. 相似文献
83.
LI Xianguo FENG Lijuan QI Jianhua CHEN Xingmao ZHANG ManpingCollege of Chemistry & Chemical Engineering Ocean University of China Qingdao P.R.China 《中国海洋大学学报(英文版)》2003,2(2)
Aerosol samples of PM10 (particulate matter with aerodynamic diameters less than 10μm) and TSP (total suspended particles) were simultaneously collected from April 2001 to March 2002 at the top of Mount Baguan on the downtown campus of Ocean University of China, Qingdao, China. The concentrations of Al, Fe, Mn, Cu, Pb and Zn were determined by means of inductively coupled plasma atomic emission spectrometry (ICP-AES). The monthly variability of the mass concentrations of aerosol particles and the concentrations of trace metals are presented and discussed. The distribution pattern of these metals in PM10 and TSP is also discussed. During the observation period, the mass concentration of PM10 at this site ranged from 13.80 to 306.42μgm-3 , while that of TSP ranged from 31.02 to 568.82μgm-3. Both PM10 and TSP reached their highest concentrations in springtime, while the lowest values occurred in summertime. The concentrations of crustal metals followed the same variation pattern, while those of anthropo 相似文献
84.
Regular distribution patterns of elements Ca, Sr, K, Na, Mg, Fe, Mn, Ti, Cu, Co, Ni, Zn, Pb, Cr, Rb, Ba, Cd, and U in Late
Quaternary strata have been studied in detail. The regional variation patterns of elements in these strata are similar to
those in recent surface sediments, showing that the sedimentary environment has been relatively stable since Late Quaternary.
Element distribution changes with the variations of lithological characters. Contents of Ca and Sr increase in coarse sediments,
while those of other elements decrease. Na content increases in the pumice layer. Mn, content tends to increase sharply towards
the surface layer. Ca content decreases sharply in strata where water depth is more than 2,000 m. The strata can be divided
based on the distribution curves of element assemblages. The variations in contents of most elements in Holocene Series are
smaller than those in Late Pleistocene Series, which might be related to the factors of glacial and interglacial changes,
sea level fluctuations and material source differences.
Contribution No. 1488 from Institute of Oceanology, Academia Sinica 相似文献
85.
North China, whose total area is 420,000 km2, covers 2 provinces and 2 cities (Shanxi and Hebei provinces, Beijing and Tianjin) and the territories of Henan and Shandong provinces to the north of the Huanghe (Yellow) River, and part of the Inner Mongolia Autonomous Region and Liaoning Province. Most of this region, which is situated in the semi-humid, semi-arid continental climate temperate zone, gets an annual precipitation of 500-600 mm, whereas, the perennial average amount of total water resource is 50.99 billion m3, including 33.82 billion m3 of surface water, 32.94 billion m3 of ground water and 15.77 billion m3 of their duplication. Due to the intensive exploitation of water resource caused by the deficiency of water resource in North China, key elements of water balance was changed, runoff volume reduced, evaporation increased, vertical movement of moisture strengthened, water circulation pattern transformed from open system into regionally closed system; meanwhile, due to the incompetent water 相似文献
86.
Ore-forming fluid and mineralization of Caijiaying and Dajing polymetallic ore deposits 总被引:3,自引:0,他引:3
WANG Lijuan WANG Jingbin WANG Yuwang & ZHU Heping. Key Laboratory of Mineral Resources Institute of Geology Geophysics Chinese Academy of Sciences Beijing China . Beijing Institute of Geology for Mineral Resources Beijing China Correspondence should be addressed to Wang Lijuan 《中国科学D辑(英文版)》2004,47(2):97-107
Fluid inclusions from the Dajing and Caijiaying deposits have nearly the same ho-mogenization temperature. Correlation between temperature and salinity shows that both Sn-and Cu-bearing fluids Sn and Cu were present in the Dajing deposit but only one kind of fluids continuously evolved in the Caijiaying deposit. Study on rare earth elements (REE) in ancient fluid from the inclusions indicates that the fluid of Sn mineralizing stage in Dajing was derived from remelting magma of the continental crust, and the fluid of Cu-Pb-Zn mineralizing stage in the Dajing deposit and the fluid of Cu-Pb-Zn mineralization in the Caijiaying deposit were derived from the mantle. It is concluded that the Cu-Pb-Zn mineralizations in the Dajing and Caijiaying deposits resulted from the identical tectono-thermal event of magma-fluids induced by Mesozoic tectonic transition and extension in the eastern part of North China Craton. 相似文献
87.
WANG Yuwang WANG Jingbin WANG Lijuan WANG Yong TU Caineng Beijing Institute of Geology for Mineral Resources Beijing Key Laboratory of Mineral Resources Research Institute of Geology Geophysics Chinese Academy of Sciences Beijing Xinjiang Kalatongke Cu-Ni Mine Fuyun Xinjiang 《《地质学报》英文版》2004,78(2):396-403
On the basis of the study on the REE geochemistry of the ore minerals and host rocks of the Kalatongke Cu-Ni deposit, Xinjiang, it is indicated that the major ore minerals, sulfides, were sourced from the host mafic-ultramafic magma. Characterized by low REE content of sulfide, such a Cu-Ni sulfide deposit occurring in the orogen is obviously different from that on the margin of the craton. Because the mafic-ultramafic rocks from the Cu-Ni sulfide deposit occurring in the orogen is water-rich and the REEs of some sulfides show a particular "multiple-bending" pattern, which suggests coexistence of multiple liquid phases (fluid and melt), the sulfide melt possibly contains a great deal of hydrothermal fluids and increasingly developed gases and liquid-rich ore-forming fluids after the main metallogenic epoch (magmatic segregation stage). 相似文献
88.
CHARACTERISTICS OF CONVECTIVE ACTIVITIES OVER ASIAN-AUSTRALIAN “LAND BRIDGE” REAS AND ITS POSSIBLE FACTORS* 下载免费PDF全文
Based on TBB data from GMS of Japan,NCEP/NCAR reanalysis data and precipitation data from CMAP(CPC Merged Analysis of Precipitation),an investigation is carried out of seasonal changes of precipitation and convection over Asian-Australian "land bridge" areas and its possible factors.The results show that the precipitation and convection over Sumatra take on clearly seasonal changes with abundant (less) rainfall in winter (summer).The convection over Sumatra moves northwestward rapidly along "land bridge" in the late-April and the early-May (the 25th pentad) and the rainfall shows similar variations.It is the accelerating of the convection moving that affects directly the subsequent enhancement of the convection over Indo-China Peninsula (ICP) area followed by the rupture of the subtropical high (SH) bands in this region leading to South China Sea (SCS) summer monsoon establishment.The zonal wind at lower troposphere in the equatorial Indian Ocean and the cross-equatorial flow in 105°E are the main factors associated with the accelerating of the convection moving northwestward along "land bridge".The further study suggests that the intensity of Sumatra convection has a close relation to the SST:when the central-east equatorial Pacific SST is warmer (colder),i.e.E1 Nino (La Nina) events,the SST in West Pacific warm pool is colder (warmer),Sumatra convection is weaker (stronger). 相似文献
89.
2011年初夏我国长江中下游降水的气候特征及成因 总被引:6,自引:3,他引:3
文章主要分析了2011年初夏长江中下游降水的气候特征及其成因。结果表明:2011年5月长江中下游降水异常偏少,6月转为异常偏多,出现了明显的旱涝转换。长江中下游地区的旱涝转换主要受南海季风、东亚季风强度以及西太平洋副热带高压(副高)的异常快速北跳的影响。研究还发现,6月亚洲中高纬长期维持两槽一脊的环流形势,东北冷涡活动频繁,多次引导冷空气南下。同时,副高异常偏北、偏西,并出现多次西伸过程。由于冷涡的加强南压与西伸的副高相互作用,促使长江以南地区西南气流明显增强,使得冷暖空气在长江中下游地区交汇,最终导致该地降水偏多。 相似文献
90.