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排序方式: 共有6774条查询结果,搜索用时 15 毫秒
891.
CAO Hong MA Enbao WANG Xuehua CHEN Jiazang BIN Xiaobei 《《地质学报》英文版》2006,80(2):285-289
By loading nanometer anatase onto exfoliated graphite with the sol-gel method, exfoliated graphite-TiO2 composite (EG-TiO2) can be prepared, which can adsorb oil and can also degrade oil. In a technologic condition for preparing EG-TiO2, the impregnated number of times is the most important factor to influence oil-adsorbing capability, that is, when the impregnated number of times increases, the amount of saturation-adsorbed oil decreases. The study of EG-TiO2 photocatalytic degradation of machine oil based on the weight-loss method and infrared spectrum method indicates that EG-TiO2 has obvious effect of photocatalytic degradation for machine oil. Its performance is superior to pure nanometer TiO2 powder because nanometer TiO2 in EG-TiO2 has three-dimension laminar structure and comparatively high adsorption capability. 相似文献
892.
This study deals with the toxic effects of Zn2+, Cu2+, Cd2+ and NH3 on Chinese prawn (Penaeus orientalis). The median lethal concentrations of the toxic matters on Chinese prawn were determined. Cd2+>Cu2+>Zn2+>NH3-Nm is the toxic order of these chemicals to Chinese prawn. The toxic order of concentrated Zn2+ and Cd2+ in tissues and organs of Chinese prawn is in the order. gill>shell+appendage>viscera>muscle. 相似文献
893.
894.
利用光腔衰荡光谱(CRDS)技术在线观测了广州番禺大气成分站(GPACS)的大气CO2浓度特征,分析了地面风对CO2的作用。结果表明:(1)大气CO2在珠江三角洲地区存在明显的地域不均匀特征,2014—2016年期间GPACS的年均本底浓度比全球背景地区平均增加了22.5×10-6(22.5 ppm);(2)大气CO2浓度在春季最高,冬、秋季次之,夏季最低,年均值为426.64±15.76 ppm;(3) CO2的日变化为双峰结构,峰值分别在05:00—07:00和21:00—22:00,谷值在13:00—15:00,表明受到了自然过程以及人为排放源的复合影响;(4)风场显著影响CO2的浓度分布,春、夏季CO2浓度距平日变化与地面风速为显著负相关,秋、冬季则为显著正相关。在春、夏季,S-WSW和NNE-N风向上CO2浓度较低,在秋、冬季,SSE-S和N方向均导致CO2浓... 相似文献
895.
Thermodynamic conditions of framework grain dissolution of clastic rocks and its application in Kela 2 gas field 总被引:3,自引:2,他引:3
LAI Xingyun YU Bingsong CHEN Junyuan CHEN Xiaolin LIU Jianqing MEI Mingxiang JING Weiguang & CHENG Suhua School of Earth Sciences Mineral Resources China University of Geosciences Beijing China Key Laboratory of Lithospheric Tectonics Deep-level Process Exploration of Ministry of Education Beijing China 《中国科学D辑(英文版)》2005,48(1):21-31
Feldspar and clastic debris are the most important constituent framework grains of sedimentary clastic rocks and their chemical dissolution plays an essential role in the formation and evolution of the secondary pore in the reservoir rocks. On the basis of thermodynamic phase equilibrium, this study investigates the chemical equilibrium relationships between fluid and various plagioclase and K-feldspar in diagenesis of the sediments, particularly, the impact of temperature and fluid compositions (pH, activity of K+, Na+, Ca2+ and so on) on precipitation and dissolution equilibria of feldspars. Feldspar is extremely easily dissolved in the acid pore water with a low salinity when temperature decreases. The dissolution of anorthite end-member of plagioclase is related to the Ca content of the mineral and the fluid, higher Ca either in the mineral or in the fluid, easier dissolution of the feldspar. Moreover, the dissolution of albite end-member of plagioclase is related to Na of both the mineral and fluid, 相似文献
896.
隧道衬砌空洞探地雷达图谱正演模拟研究 总被引:4,自引:0,他引:4
探地雷达作为一种高效、先进的无损检测设备,能够对隧道衬砌实施连续扫描,实时获得雷达图谱。然而,由于探地雷达在我国的应用时间还非常短暂以及雷达图谱的复杂性,隧道衬砌空洞探地雷达图谱的辨识还存在一定的问题。据此,通过不同环境的试验得到空洞雷达图谱特征,并利用二维时域有限差分法对衬砌空洞雷达图谱进行正演模拟。采用VC++语言编写探地雷达正演模拟程序,对隧道衬砌检测中常见的几种空洞模型进行正演模拟,得出模拟波形和图谱,并与实测隧道衬砌空洞的探地雷达波形和图谱进行对比。结果表明,模拟图谱与实测结果相似,具有较明显的空洞特征。良好的结果也验证了二维时域有限差分法(2D-FDTD)正演模拟的可行性。 相似文献
897.
不纯碳酸盐岩的变质作用 总被引:1,自引:0,他引:1
不纯碳酸盐岩中的矿物共生组合与变质时的总压和二氧化碳分压密切相关。总压增高促使透闪石、透辉石和橄榄石等矿物生成温度增高。变质过程中岩石中流体成分的变化有两种极端情况,即渗滤作用和缓冲作用。渗滤作用下变质反应,变质矿物界线和变质矿物特征等均与缓冲作用下有所差异,以此可以区别它们。湖北宿松群和河北红旗营子群不纯大理岩是在渗滤作用下变质的。山西五台群板峪口组不纯大理岩是在缓冲加渗滤作用下变质的。 相似文献
898.
899.
Rivers in the Liaohe River Estuary area have been seriously polluted by discharges of wastewater containing petroleum pollutants and nutrients. In this paper, The Enhanced Stream Water Quality Model (QUAL2K) and its revised model as well as One-dimensional Tide Mean Model (1D model) were applied to predict and assess the water quality of the tidal river reach of the Liaohe River Estuary. Dissolved oxygen (DO), biochemical oxygen demand (BOD5), ammonia nitrogen (NH3-N) and total phosphorus (TP) were chosen as water quality indices in the two model simulations. The modelled results show that the major reasons for degraded rivers remain petroleum and non-point source pollution. Tidal water also has a critical effect on the variation of water quality. The sensitivity analysis identifies that flow rate, point load and diffuse load are the most sensitive parameters for the four water quality indices in the revised QUAL2K simulation. Uncertainty analysis based on a Monte Carlo simulation gives the probability distribution of the four water quality indices at two locations (6.50 km and 44.84 km from the river mouth). The statistical outcomes indicate that the observed data fall within the 90% confidence intervals at all sites measured, and show that the revised QUAL2K gives better results in simulating the water quality of a tidal river. 相似文献
900.
Hans-Joachim Massonne 《Earth and Planetary Science Letters》2003,216(3):347-364
The petrography and chemical composition of minerals of quartz-rich diamondiferous rocks from the Kokchetav Massif, especially the zonation of garnet, were studied and compared with diamondiferous quartzofeldspathic rocks from the Saxonian Erzgebirge. Many compositional and textural features were found to be similar. For instance, microdiamonds are enclosed systematically in a specific intermediate growth zone of garnet in these rocks. On the basis of experimental data, a magmatic scenario was constructed to check if the quartz-rich diamondiferous rocks are of magmatic origin. By this, the P-T paths, derived here for the Kokchetav rocks, and the textural observations it is concluded that the minerals of the diamondiferous rocks have crystallized from silicate melts. These melts originated by anatexis of deeply submerged metasediments (Erzgebirge: at T as high as 1200°C, Kokchetav Massif: at 50-100°C lower T) and ascended from at least 200 km depth. Relics of the pre-anatectic evolution are still present, for instance, as garnet cores. After ascent and emplacement of the magma in deep portions of thickened continental crust (Kokchetav Massif: 45-50 km close to 800°C, Erzgebirge: 55-60 km at 30-50°C lower T) considerable quantities of (white and/or dark) micas formed by peritectic reactions from melt. For instance, garnets could be resorbed at this stage and biotite grew instead. After the magmatic stage, retrogression took place much stronger in the Kokchetav Massif. This was accompanied by deformation transforming broadly the magmatic texture of quartz-rich diamondiferous rocks from the Kokchetav Massif to a gneissic texture. 相似文献