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1.
Chemical characteristics of the surface water and algae in lakes in the Seduiyakha River basin are presented. Specific features of components of limnetic ecosystems under the influence of anthropogenic factors in the territory of an oil–gas condensate field are shown. Ambiguous response of algal communities to changes in the aquatic environment is revealed. 相似文献
2.
V. L. Khokhlova D. V. Vasilchenko V. V. Stepanov I. I. Romanyuk 《Astronomy Letters》2000,26(3):177-191
We present the results of our analysis of magnetic-field configuration and abundance anomalies on the surface of the rapidly rotating, chemically peculiar helium-strong variable B2 V star HD 37776 with unresolved Zeeman components of spectral lines. Simultaneous inversion of the observed Stokes I and V profiles, which realizes the method of Doppler-Zeeman mapping [1], has been applied for the first time. Spectroscopic observations were carried out with the Main stellar spectrograph of the 6-m Special Astrophysical Observatory telescope equipped with a Zeeman analyzer and a CCD array, which allowed spectra in right-and left-hand circularly polarized light to be taken simultaneously at a signal-to-noise ratio S/N≥200 [2]. The profile width of winged spectral lines (reaching 5 Å) is determined by Zeeman line splitting; however, the observed Zeeman components are blurred and unresolved because of the rapid stellar rotation. When solving the inverse problem, we sought for the magnetic-field configuration in the form of a combination of arbitrarily oriented dipole, quadrupole, and octupole placed at the stellar center. The observed Stokes I and V profiles for eight spectral lines of He, O II, Al III, Si III, and Fe III averaged over the visible stellar surface were used as input data. We constructed a model of the magnetic field from the condition of coincidence of magnetic maps obtained from different lines of different chemical elements and from the condition of a minimum profile residual. This model is a combination of centered coaxial dipole and quadrupole with the dominant quadrupole component at 30°<i<50°, β=40°, and a maximum surface field strength H s=60 kG. A comparison of our abundance maps with the field configuration shows that the He concentration is at a maximum in the regions of maximum radial field, while the maximum concentrations of O, Al, Si, and Fe coincide with the regions of maximum tangential field. 相似文献
3.
I. A. Aslanov G. Heildebrandt V. L. Khokhlova W. Shöneich 《Astrophysics and Space Science》1973,21(2):477-485
The period of light variationP=1
.
d
13316 has been found for the silicon B9 IVp star HD 193722. Spectroscopic study of this star was based on 35 spectrograms with dispersion 4 Å mm–1 well distributed in phase. The measurements of radial velocities of spectral line components for SiII, HeI, EuII, FeII and SrII allowed us to localize several regions on the surface of the star with enhanced abundance of these elements. The phase of maximum light inU, B andV was found to be the same as the phase of maximum Eu abundance. The coincidence of the regions with larger abundance of Si and He in HD 193 722 disagree with the hypothesis of diffusion in the presence of a magnetic field developed by Michaud (1971), to explain the peculiar chemical composition of Ap-stars.HD 193722 is a silicon B9 IVp star for which the magnetic field has not been measured. In the list by Palmeret al. (1962) its rotational velocityV sini is given as 250 kms–1. As will be seen below, this value is too high. Megessier (1971) determined from hydrogen line profiles and continuous spectrumT
eff=13 000° and lgg=3.5.The results of photometric and spectroscopic study of HD193722 are given below. 相似文献
4.
Data on water chemistry in water bodies and streams in Pechora basin in the territory of several gas-condensate deposits are
presented. Diatom algae of periphyton and macrophytes are used to assess the effect of production facilities on aquatic ecosystems.
The specific features of the structure of diatom complexes in streams subject to the effect of pollutants and accumulation
of heavy metals in individual plant species in water bodies accumulating production wastes are shown. 相似文献
5.
The results are presented of the analysis of mean values and trends in precipitable water in the Arctic atmosphere determined from the data of 55 aerological stations located northwards of 60° N for 1972-2011. The regions with maximum and minimum mean values and trends are identified. It is demonstrated that the humidity increase took place almost over the whole latitudinal zone in summer. The comparison with similar characteristics obtained by other researchers from the reanalysis data demonstrates good agreement. 相似文献
6.
Carbonate pedofeatures （CPs） in a chronosequence of paleosols buried under kurgans in the Northern Caucasus region of Russia in a period from the end of the 4th to the middle of the 5th centuries AD （It seams that there is no time left） were studied by using a set of morphological and isotopic methods. The CPs in chernozem-type soils of Russia are usually represented by crystallomorphic calcite whereas the non-segregated carbonates occurred at the same horizons - by collomorphic one. Those two morphotypes of calcite have the differences in elemental composition and isotopic composition of carbon and, hence, should have different origins - from true and colloidal solutions, respectively. The same differences including radiocarbon age have been revealed for pseudomycelium of the ABca horizon of the youngest paleosols as compared with the same CPs of other paleosols in the chronosequence studied. Our assumption is that it was succeeded in finding that the pseudomycelium right away after its precipitation from a colloidal solution migrated from the lower soil horizons to the surface horizons during the periods of climatic aridization. After a short time interval （not more than 25-50 years） collomorphic calcite in the pseudomicelium of the yongest paleosols mentioned above will likely become by ＂usual＂ acicular calcite. 相似文献
7.
O. Popovicheva E. Kireeva N. Persiantseva T. Khokhlova N. Shonija V. Tishkova B. Demirdjian 《Atmospheric Research》2008,90(2-4):326-ICNAA07
More than 3000 water droplets with soot particles immersed were monitored individually to identify the effect of heterogeneous freezing and establish the link between soot properties and freezing efficiency. A set of soot samples from many combustion sources, including an aircraft engine combustor were examined. The list of key soot properties affecting freezing were determined. It appears that soot effectiveness in causing the droplets to freeze mainly depends on the soot behaviour in water defined by the mass density of soot agglomerates, size and wetting. When large mass particles were homogeneously distributed through droplets and were stable to sedimentation effects median freezing temperatures of such droplets were significantly warmer than pure water droplets. The long-term presence of large soot agglomerates in water leads to an increase in the freezing efficiency over time because of the slow kinetics of wetting. Small sizes of soot agglomerates stimulate aggregative instability in droplets with large soot mass which decreases the total soot surface area and the freezing temperature. The highest freezing efficiency is found for homogeneously distributed soot agglomerates of high porosity. A gradual increase of the freezing temperature in correspondence with number density of active oxygen-containing sites is observed for soots having surfaces of low or intermediate polarity. However, highly soluble surface compounds, such as sulfates, may be easily dissolved in water leading to a decrease in the potential freezing efficiency. This was the case found for aircraft engine combustor generated soot. Therefore relatively hydrophobic soot with a significant number of oxygen-containing functional groups but not covered totally by hydrophilic sites and soluble compounds is proposed to act as the most efficient immersion freezing nuclei in the atmospheric cloud droplets. 相似文献
8.
Methodological problems of climatic reconstruction for different periods of Holocene are discussed on the basis of a multiple group biological analysis on peat-sapropel sediments.The possibility of biological analysis is exemplified by the paleoclimatic reconstruction for Carpathian and Altai Mountain ranges.For the "Skolevsky Beskidy" national park of Carpaty the paleoclimatic scenarios have been drown up aiming at the more precise definition of climatic conditions for the period of mass mountain slope terracing.The stability of terrace systems of various designs in the current climatic conditions has been assessed.It is shown that during periods of humid climate the terraces,whose designs have been focused on drainage,were built.In periods of dry and warm climate the terrace systems capable of accumulating water were built.Both these types of terrace systems are destroyed in nowadays.Only those terrace systems are stable which were adjusted by their builders to contrast variations of precipitation.For Western Altais the paleoclimatic scenario has been done to forecast the safety of the Bronze Age kurgans(burial earth mounds) with permafrost inside the construction.In the Altay region during the Holocene it has revealed two periods of sharp cooling,the peaks of which occurred in the intervals 4500-4300 and 2500-2300 years ago,and two periods of pronounced climatic drying 4900-4700 and 130-70 years ago.Depletion of the algae composition in the layer corresponding to the last period of drying climate indicates a very sharp change in the parameters of moisture and turning the lake into a dry swamp.Periods of cold weather may have contributed to the formation of special ritual traditions of the Sakan tribes that require the frozen ground to bury the dead.The later climate fluctuations identified have not affected the safety of permafrost in burial mounds constructed in the V-III cc BC. 相似文献
9.
The time series of seasonal average values and standard deviations of wind speed components at the isobaric surfaces of 850 and 200 hPa are analyzed on the basis of the data of upper-air observations carried out in 1961–2003 at 18 stations of the Russian Federation territory. The energy spectra of wind speed components in the first and in the second halves of the whole period under study are compared. On the whole, an increase in average values of U-component and decrease in average values of V-component took place both in upper and lower troposphere, and the largest variations occurred in winter season in the upper troposphere. Average coefficients of linear trends of average winter values for the whole region amount to 0.57 and ?0.62 m/s per 10 years for the wind components U and V at the isobaric surface of 200 hPa, respectively. The increase in the standard deviations of both components was registered in the upper troposphere in winter period almost on the whole territory. The average coefficients of linear trends of standard deviations at the isobaric surface of 200 hPa in winter for the whole region amount to 0.53 and 0.61 m/s per 10 years for U- and V-components, respectively. The intensity of the annual cycle and processes of intraseasonal scale both in the lower and upper troposphere increased in the second half of the whole interval under study. 相似文献
10.
The surface inhomogeneities of the chemical composition of HD 140160 (χ Ser) were studied from the spectral line profiles. The method of quantitative analysis of local abundance proposed by Khokhlova (1974) was used. The overabundance of Sr up to 103 was found in three ‘spots’ on the surface of the star and normal abundance outside the spots. Iron was found to be overabundant up to 10 times in four spots and deficient by 10 times outside the spots. Some arguments in favour of a supernova hypothesis are mentioned to explain the deficiency of iron. 相似文献