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81.
A. Szczucińska 《Geochemistry International》2017,55(12):1164-1170
Hydrogeochemical background determined for an investigated environment, defines characteristic range of its hydrochemical characteristics. This allows to observe the temporal changes of the chemical water properties taking place in the studied environments, such as due to human impact. The paper presents the results of study on the present-day hydrogeochemical background in the Lubuskie Lakeland, the region repeatedly covered by the ice sheets during the Pleistocene and little affected by anthropogenic impact. The hydrogeochemical background was established on a basis of physicochemical analyses of spring waters sampled every 3 months between November 2011 and October 2013 from 20 springs. Present-day hydrogeochemical background was assumed to be represented by values ranging between 16 and 84 percentiles. The ranges of hydrogeochemical background for the studied ions on the Lubuskie Lakeland, were in the lower range of the background considered for useful waters in Poland. The obtained results indicated that the studied spring waters were poorly diversified in terms of composition of main cations and anions, as well as electrical conductivity and total water hardness. However, large variability was observed for Fetot, Mn2+ and NO3?. Moreover, NO3? and SO42? were noted in some cases to be in excess of national hydrogeochemical background values. 相似文献
82.
New marine ΔR values for Arctic Canada 总被引:1,自引:0,他引:1
Roy D. Coulthard Mark F.A. Furze Anna J. Pieńkowski F. Chantel Nixon John H. England 《Quaternary Geochronology》2010,5(4):419-434
For more than four decades, the reporting of 14C dates on marine molluscs from Arctic Canada has been notable for the lack of consistently applied marine reservoir corrections. We propose that the common approach of reporting Canadian Arctic marine 14C dates using presumed time-invariant reservoir corrections be abandoned in favour of calibration of 14C dates, using the current standard protocol. This approach best facilitates inter- and intra-regional correlation, and correlation with other geochronometers. In order to enable the consistent calibration of marine 14C dates from Arctic Canada, we analysed a 14C database of 108 marine mollusc samples collected live between 1894 and 1956, and determined regional reservoir offset values (ΔR) for eight oceanographically distinct regions. The following new ΔR values should be used for 14C calibration: NW Canadian Arctic Archipelago, 335 ± 85 yrs; Foxe Basin, 310 ± 90 yrs; NE Baffin Island, 220 ± 20 yrs; SE Baffin Island, 150 ± 60 yrs; Hudson Strait, 65 ± 60 yrs; Ungava Bay, 145 ± 95 yrs; Hudson Bay, 110 ± 65 yrs; and James Bay, 365 ± 115 yrs. 相似文献
83.
Beata Dziak-Jankowska 《Acta Geophysica》2010,58(2):392-416
This article is a continuation of the previous one considering the evolution of a long-period comet. The changes of the local
radius and the moment of inertia as well as the orientation of the rotation axis are calculated. With reference to the previous
model, the time-dependent orbital parameters are introduced. The procedure of sublimation-driven evolution is implemented
to the comets 67P/Churyumov-Gerasimenko, 9P/Tempel 1, and 81P/Wild. The inclination of the rotation axis of Comet Ch-G is
calculated. The position of the rotation axis is a result of the best fit of the water production rate curve received from
modelling to the observational water production rate curve. The method is verified through application to Comets 9P/Tempel
1 and 81P/Wild with well-known positions of the rotation axes. The best fit is for inclination of the rotation axis which
is close to the position of the rotation axis with minimum energy (maximum of the moment of inertia). For the best fitted
position of the rotation axis I = 90° and Φ = 60°, the largest decrease of radius was about 5.6 m in the northern polar region. The smallest decrease of radius, of about
0.3 m, was noticed on cometographic latitudes between 39° and 46°. 相似文献
84.
85.
In 2011, a geophysical survey was carried out in the surroundings of the Jagiellonian University in Cracow, using a Very Low Frequency method. The measurements were designed to determine the reason of frequent flooding of the lowest level of the building. The main objective of the study was to find out from where and in which way the rainwater seeps into the building and how this problem can be solved in the least invasive manner. The aim of geophysical methods was also to provide necessary information that will enable the construction of a hydro-geological model of the local environment. The interpretation revealed the presence of a sandy gutter surrounded by impermeable clay. There is a big resistivity contrast between those layers. Their location and approximate dimensions were determined. 相似文献
86.
An analysis of linear relationships between the ground-level components of the Earth’s magnetic field measured at different sites is a relatively new topic compared to the analysis of data at a single location. The data collected by the INTERMAGNET observation network provide perfect set of data to which this analysis can be used. An important tool in this analysis may be developing a method of determination of the impulse response for linear systems in the time domain. An advantage of calculations in the time domain over the generally known and applied methods in the frequency domain is the possibility of determining prediction of output signals. By that, simultaneously with the analysis of linear relationships, a tool for recovering missing records in incomplete observation data is obtained. Filling-in the missing data may increase interest and possibility of using the observational data by researchers experimenting with the analysis in the frequency domain where gaps in data records are a significant limitation. 相似文献
87.
88.
Lech Krysiński 《Pure and Applied Geophysics》2009,166(3):375-408
The paper describes a new method of gravity modelling of the density cross section along a DSS profile. We propose a systematic
procedure of gravity interpretation using structural information contained both in the velocity distribution of the seismic
model and the geometry of its layers. The procedure is based on the optimisation of the density parameters of the model. The
values of the parameters are limited by relationships between the seismic velocity and the density (optimisation with inequalities).
The formulation of the method allows for discussion of the presence of isostasy and the distribution of compensating masses.
The discussion is very important for the considered crust-lithosphere system. The presented calculations are done for one
Carpathian profile (CEL01). The analysis of the properties of the fitting procedure provides the characteristic depth of subcrustal
compensating density structures, the position of crucial tectonic boundaries along the profiles, locations of the crustal
areas having exceptional lithology, the regional density differences of subcrustal matter and the estimation of regional deviations
from the isostatic equilibrium. 相似文献
89.
Comparison of source parameters estimated in the frequency and time domains for seismic events at the Rudna copper mine,Poland 总被引:3,自引:0,他引:3
Source parameters estimated in the frequency domain for 100 selected seismic events from the Rudna copper mine, with moment
magnitude ranging from 1.4 to 3.6, were collected to study their scaling relations and to compare them with the parameters
estimated in the time domain. The apparent stress and static stress drop, corrected for the limited bandwidth recording, increase
slightly in a similar manner with increasing seismic moment. The ratio of apparent stress to static stress drop, a measure
of radiation efficiency, is practically constant and its mean value is close to 0.1.
For 37 seismic events, with moment magnitude between 1.9 and 3.4, source parameters were estimated in the time domain from
relative source time functions, that displayed unilateral rupture propagation, and their rupture velocity could be estimated.
It ranges from 0.23 to 0.80 of shear wave velocity and is almost independent of seismic moment. The fault length, estimated
from the average source pulse width and rupture velocity, is clearly dependent on seismic moment and is smaller than the source
radius estimated from the corner frequency on the average by about 25 percent. There is no correlation between the values
of static stress drop estimated in the frequency and time domains, but the time domain stress drop is in general similar to
that estimated in the frequency domain. The apparent stress increases with increasing rupture velocity, and the ratio of apparent
stress to static stress drop seems also to depend on rupture velocity. 相似文献
90.