新安江流域上空云内外巨盐核的分布   总被引：2，自引：0，他引：2  

黄美元  何珍珍  沈志来 《大气科学》1982,6(3):301-307

1979—1980年6—7月份在新安江流域上空进行了云内外巨盐核的观测,得到:(1)大气中云内外的巨盐核浓度分布都与天气背景有关;(2)云内巨盐核浓度大于同高度上的云外巨盐核浓度,不同云内巨盐核浓度和谱型不一样;(3)云内巨盐核浓度要比小云滴少两个量级,因此巨盐核作为凝结核,对形成小云滴的贡献是很小的。  相似文献   

Mineralogical study of spinel-lherzolite inclusions from basalts in southern and eastern China     

Wankang Huang  Jianguo Xu  Zhenmin Gao  Junya Nan 《中国地球化学学报》1983,2(4):361-376

Ten spinel-lherzolite inclusions and one olivine-websterite inclusion, which were collected from Fujian, Jiangsu, Hebei and Yunnan Provinces, consist of olivine (FΦ_87.7–91.2), enstatite (En_87.3–89.7), Cr-diopside and spinel. According to the Mg/(Mg+Fe²⁺) ratios in the rocks and their mineralogies, they are designated to the Cr-diopside type. The websterite is composed of bronzite (En_71.9) and augite, while the gabbro-norite consists of hypersthene (En_68.9) and augite, belonging to the Al-augite type. The geothermos of spinel-lherzolites were calculated with four geothermometric methods, giving a temperature range of 925°–1,072°C. However, according to P. R. A. Wells' method, temperatures range from 845δ to 1,014°C, and by D. H. Lindsly's approach, from 716°–974°C. Pressures range from 15.1 to 19.8 kb. Genetically, Spinel-lherzolites and olivine-websterite are thought to have been derived from residual mantle material by partial melting at approximately 1,000°C and at a depth of about 50–70 km. Websterite and gabbro-norite may be products of the crystallization-differentiation of alkali basaltic magma.  相似文献   

1901-1995年气候变化导致陆地生态系统净吸收碳   总被引：2，自引：0，他引：2  

Yang Xin  Wang Mingxing  Huang Yao 《大气科学进展》2001,18(6):1192-1206

The spatial and temporal variability of land carbon flux over the past one hundred years was investigated based on an empirical model directly calculating soil respiration rate. Our model shows that during 1901-1995, about 44-89 PgC (equals to 0.5, 0.9 PgC/yr respectively) were absorbed by terrestrial biosphere. The simulated net ecosystem productivity (NEP) after the 1930s was close to the estimated value of" missing C sink” from deconvolution analysis. Most of the total carbon sink happened during 1951-1985 with the estimated value of 33-50 PgC. Three major sinks were located in the tropics (10°S-10°N), Northern mid-latitudes (30°-60°N) and Southern subtropics (10°-40°S). During 1940s-mid-1970s, carbon sinks by terrestrial ecosystem increased with time, and decreased after the mid-1970s. These may be due to the ch anging of climate condition, as during the 1940s-1970s, temperature decreased and precipitation increased, while after the mid-1970s, an opposite climate situation occurred with evident increasing in temperature and decreasing in precipitation. Usually, warmer and dryer climate condition is not favor for carbon absorption by biosphere and even induces net carbon release from soil, while cooler and wetter condition may induce more carbon sink. Our model results show that the net carbon flux is particularly dependent on moisture / precipitation effect despite of temperature effect. The changing of climate in the past century may be a possible factor inducing increases in carbon sink in addition to CO2 and N fertilizer.  相似文献   

Carbon Storage in Terrestrial Ecosystems of China: Estimates at Different Spatial Resolutions and Their Responses to Climate Change   总被引：20，自引：1，他引：19  

Jian Ni 《Climatic change》2001,49(3):339-358

The carbon storage of terrestrial ecosystems in China was estimated using acommon carbon density method for vegetation and soils relating to thevegetation types. Usingmedian density estimates, carbon storage of 35.23 Gt (1 Gt = 10¹⁵g) in biomass and119.76 Gt in soils with total of 154.99 Gt were calculated based on thebaseline distribution of37 vegetation types. Total carbon storage of the median estimates at differentspatial resolutionswas 153.43, 158.08 and 158.54 Gt, respectively, for the fine (10),median (20) and coarse (30)latitude × longitude grids. There were differences of –1.56, +3.09and +3.55 Gt carbon storagebetween baseline vegetation and those at different spatial resolutions. Changein mappingresolution would change area estimates and hence carbon storage estimates. Thefiner the spatialresolution in mapping vegetation, the closer the carbon storage to thebaseline estimation. Carbonstorage in vegetation and soils for baseline vegetation is quite similar tothat of biomes predictedby BIOME3 for the present climate and CO₂ concentration of 340ppmv. Climate changealone as well as climate change with elevated CO₂ concentrationwill produce an increasein carbon stored by vegetation and soils, especially a larger increase in thesoils. Total mediancarbon storage of terrestrial ecosystems in China will increase by 5.09 Gt and15.91 Gt for theclimate scenario at CO₂ concentration of 340 ppmv and 500 ppmv,respectively. This ismainly due to changes in vegetation areas and the effects of changes inclimate and CO₂concentration.  相似文献   

中国遥感卫星辐射校正场气溶胶光学特性观测研究   总被引：19，自引：3，他引：16       下载免费PDF全文

胡秀清  张玉香等 《应用气象学报》2001,12(3):257-266

1999年6月28日~7月19日在敦煌场, 7月25日~7月31日在青海湖水面场进行了一次大规模综合野外测量试验, 其中采用3台先进的法国CIMEL太阳辐射计对两个场地大气光学特性进行了系统全面测量, 获得大量晴空天气条件下的大气光学数据。利用Langley法处理气溶胶通道数据得到气溶胶光学厚度及其光谱变化。测量结果显示550 nm波长平均气溶胶光学厚度分别为0.12、0.18, 由气溶胶光学厚度的波长变化得到气溶胶Junge参数分别为2.6、3.0, 并与几种典型气溶胶类型比较。结果表明两地在晴空天气里, 气溶胶含量较小, 符合遥感卫星传感器辐射定标的大气条件。  相似文献   

山东山旺盆地中新世两个蚂蚁新属（Heteromyrmex Zhang,1989和Tolylasius Zhang,1989）的修正     

洪友崇  吴坚等 《地质论评》2001,47(4):345-349

1989年,张俊峰发表了山东山旺盆地中新世（N2）2个蚂蚁新属新种：Heteromyrmex atopogaster Zhang,1989和Tolylasius inflatus Zhang,1989。经检验,前一个属是基于不实的观察结果,新属、种应予废除,作为未定属种归人蚁亚科（Formicinae);后一个属的建属根据都非建属的根据,其他的特征系毛蚁属（Lasius)的属征范围,没有建属条件,属应予废,保留其种,转移到毛蚁属。  相似文献   

璜山金矿找矿模式及应用     

黄仁荣  何长友 《浙江国土资源》2001,17(2):27-32

诸暨璜山金矿是除治岭头以外浙江省第二金矿,它的找矿模式为"三高两低一复合"的找矿模式,即高金晕、高极化率、高磁场跳跃、低电阻率、低电位和北东断裂与北东东断裂复合处是成矿最有利部位.在其附近仍有类似成矿部位,有望扩大远景.  相似文献   

Adsorption and Desorption of Phosphate on Calcite and Aragonite in Seawater   总被引：3，自引：0，他引：3  

Frank Millero  Fen Huang  Xiaorong Zhu  Xuewu Liu  Jia-Zhong Zhang 《Aquatic Geochemistry》2001,7(1):33-56

The adsorption and desorption of phosphate on calcite and aragonite were investigated as a function of temperature (5–45 °C)and salinity (0–40) in seawater pre-equilibrated with CaCO₃. An increase in temperature increased the equilibrium adsorption; whereas an increase in salinity decreased the adsorption. Adsorption measurements made in NaCl were lower than the results in seawater. The higher values in seawater were due to the presence of Mg²⁺ and Ca²⁺ ions. The increase was 5 times greater for Ca²⁺ than Mg²⁺. The effects ofCa²⁺ and Mg²⁺ are diminished with the addition of SO₄ ^2- apparently due to the formation of MgSO₄ and CaSO₄ complexes in solution and/or SO₄ ^2- adsorption on the surface of CaCO₃. The adsorbed Ca²⁺ and Mg²⁺ on CaCO₃ (at carbonate sites) may act as bridges to PO₄ ^3- ions. The bridging effect of Ca²⁺is greater than Mg²⁺ apparently due to the stronger interactions of Ca²⁺ with PO₄ ^3-.The apparent effect of salinity on the adsorption of PO₄ was largely due to changes in the concentration of HCO₃ ^- in the solutions. An increase in the concentration of HCO₃ ^- caused the adsorption of phosphate to decrease, especially at low salinities. The adsorption at the same level of HCO₃ ^- (2 mM) was nearly independent of salinity. All of the adsorption measurements were modeled empirically using a Langmuir-type adsorption isotherm[ [PO₄]_ad = K_mC_m[PO₄]_T/(1 +K_m [PO₄]_T) , ]where [PO₄]_ad and [PO₄]_T are the adsorbed and total dissolved phosphate concentrations, respectively. The values of C_m (the maximum monolayer adsorption capacity, (mol/g) and K_m (the adsorption equilibrium constant, g/(mol) over the entire temperature (t, °C) and salinity (S) range were fitted to[ C_m = 17.067 + 0.1707t - 0.4693S + 0.0082S² ( = 0.7) ][ ln K_m = - 2.412 + 0.0165t - 0.0004St - 0.0008S² ( = 0.1) ]These empirical equations reproduce all of our measurements of[PO₄]_ad up to 14 mol/g and within ±0.7 mol/g.The kinetic data showed that the phosphate uptake on carbonate minerals appears to be a multi-step process. Both the adsorption and desorption were quite fast in the first stage (less than 30 min) followed by a much slower process (lasting more than 1 week). Our results indicate that within 24 hours aragonite has a higher sorption capacity than calcite. The differences between calcite and aragonite become smaller with time. Consequently, the mineral composition of the sediments may affect the short-term phosphate adsorption and desorption on calcium carbonate. Up to 80 % of the adsorbed phosphate is released from calcium carbonate over one day. The amount of PO₄ left on the CaCO₃ is close to the equilibrium adsorption. The release of PO₄ from calcite is faster than from aragonite. Measurements with Florida Bay sediments produced results between those for calcite and aragonite. Our results indicate that the calcium carbonate can be both a sink and source of phosphate in natural waters.  相似文献   

多维地震动各方向相关性对拱坝动应力的影响     

吴健  金峰  徐艳杰 《地震工程与工程振动》2005,25(2):50-54

本文将随机振动的虚拟激励法与拱坝-地基动力相互作用FE-BE-IBE时域模型结合，发展了一个可以考虑多维随机地震动作用下的拱坝动力响应计算模型，并用Monte Garlo方法对模型进行了验证，计算结果表明，地震动分量的相关性对结构的动力响应存在一定影响，合理考虑地震动各方向分量的相关性可以更好地计算实际地震作用下的拱坝动力响应。  相似文献   

填充墙与钢框架协同工作性能非线性分析   总被引：5，自引：2，他引：5  

戴绍斌  余欢  黄俊 《地震工程与工程振动》2005,25(3):24-28

在试验研究的基础上，运用ANSYS有限元中的接触单元建模，对加气混凝土填充墙钢框架的结构性能进行了研究，同时与纯钢框架结构在强度、刚度、以及延性等方面进行了对比分析，结果表明：填充墙与钢框架协同工作能够改善钢框架结构的受力性能和抗震能力，这为钢结构及其围护体系的研究与推广应用提供了一定的理论依据。  相似文献