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T. V. Koroleva P. P. Krechetov I. N. Semenkov A. V. Sharapova A. D. Kondrat’ev 《Russian Meteorology and Hydrology》2016,41(8):585-591
Snow cover contamination is assessed in the impact areas of the first stage of the expandable launch system Proton in Central Kazakhstan. It was revealed that the chemical effect ofpropellants on the snow cover is local. The increase in the content of the following high-toxic substances in the snow was registered: unsymmetrical dimethylhydrazine, nitrosodimethylamine, and nitrate and nitrite ions. The most part of the pollutants is localized in the upper 5-cm snow layer. Nitrogen tetroxide decreases the value of pH, and unsymmetrical dimethylhydrazine increases it. The inflow of calcareous soil particles to the atmosphere and their subsequent fallout result in the alkalization of snow and in the neutralization of acidification by nitrogen tetroxide accompanied by the formation ofthe salts of nitric acid and nitrous acid. 相似文献
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Surface wave tomography method based on analysis of ambient noise is widely used during the last decade. It is assumed that correlated component of noise is composed of surface waves generated by sources distributed over the Earth’s surface more or less uniformly. In such a case the cross-correlation function (CCF) at two stations may be considered as the Green’s function of surface wave. This function should be symmetric relatively to zero time. However analysis of CCF at the stations located at the East-European Platform shows that as a rule CCF is characterized with a strong asymmetry. Since “purered noise cannot be extracted from seismic records due to superposition of earthquake signals, the method for calculation of CCF includes amplitude normalization for suppression of earthquakes that reduces signals from earthquakes to a noise level. The parts of records containing waves from earthquakes are neglected because of their short duration. Present study shows that this contribution turns out to be dominant at periods larger than 20–40 s. In other words, what is assumed as a “noisered in reality is a superposition of signals from earthquakes. This fact results in distortion of the Green’s function and of surface wave dispersion curve used in surface wave tomography if in the time interval used for calculation of CCF many earthquakes occur within a small area apart of an extension of the interstation path (clustering). Numerical modeling shows how clusters of sources affect CCF and dispersion curve correspondingly. Means for reducing this effect are outlined. 相似文献
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The surface wave tomography from ambient seismic noise recorded at stations in Western Europe (WE) and on the East European Platform (EEP) revealed the structure of the crust and upper mantle in the transitional zone from the Precambrian platform to the younger geological units in Western Europe. The Tornquist-Teisseyre Line separating these structures is clearly traced as a transition zone from the high velocities beneath EEP to the low velocities beneath WE in the crust and upper mantle, which extends to a depth of 150?C170 km. Below 200 km the relationship between the velocities beneath EEP and WE becomes the opposite. A similar relationship between the velocities in the upper mantle down to a depth of 300 km is observed on the southern boundary, where EEP borders on the northern segment of the Alpine-Himalayan seismic belt. 相似文献
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A. V. Zotov B. R. Tagirov L. A. Koroleva V. A. Volchenkova 《Geology of Ore Deposits》2017,59(5):421-429
The coupled solubility of Au(cr) and Pt(cr) has been measured in acidic chloride solutions at 350–450°С and 0.5 and 1 kb using the autoclave technique with determination of dissolved metal contents after quenching. The constants of the reaction combining the dominant species of Au and Pt in high-temperature hydrothermal fluids (K(Au–Pt)) have been determined: 2 Au(cr) + PtCl42- = Pt(cr) + 2AuCl2-; log K(Au–Pt) =–1.02 ± 0.25 (450°С, 1 kb), 0.09 ± 0.15 (450°С, 0.5 kb), and –1.31 ± 0.20 (350°С, 1 kb). It has been established that the factors affecting the Au/Pt concentration ratio in hydrothermal fluids and precipitated ores are temperature, pressure, redox potential, and sulfur fugacity. An increase in temperature results in an increase in the Au/Pt concentration ratio (up to ~550°С at P = 1 kb). A decrease in pressure and redox potential leads to enrichment of fluid in Au. An increase in sulfur fugacity in the stability field of Pt sulfides results in increase in the Au/Pt concentration ratio. Native platinum is replaced by sulfide mineral in low-temperature systems enriched in Pt (relative to Au). 相似文献