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Wyświetlanie 1-15 z 19
Tytuł:
Effects of swelly pressure on changes in pore space morphology in Miocene clays from Warsaw: preliminary results and open questions
Autorzy:
Gawriuczenkow, I.
Powiązania:
https://bibliotekanauki.pl/articles/2059190.pdf
Data publikacji:
2003
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
swelly pressure
microstructure
porosity
hydraulic conductivity
Opis:
Miocene clays of the Poznań series from Warsaw were analysed by scanning electron microscope. The influence of swelly pressure causes soil porosity to decrease slightly together with a reorientation of pores. They become more anisometric, while their original matrix microstructure acquires properties of matrix-turbulent microstructure.
Źródło:
Geological Quarterly; 2003, 47, 2; 215-220
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Rozpoznanie stref dopływu wody podziemnej do wykopu pod fundamenty nowego budynku ACK CYFRONET AGH w Krakowie z wykorzystaniem metody konduktometrycznej
Application of the ground conductivity meters to finding groundwater leak zones in the foundations of the new-built AKC CYFRONET building, AGH UST, Cracow
Autorzy:
Klityński, W.
Stefaniuk, M.
Cygal, A.
Powiązania:
https://bibliotekanauki.pl/articles/2075384.pdf
Data publikacji:
2015
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
przewodność
woda zmineralizowana
wyciek wody
strefy dopływu wody
conductivity
mineralized water
water leakage
ground conductivity meters
Opis:
Electrical conductivity is used in the study of fresh-water and/or mineralized water outflow zones. Conductivity of water is relatively low. It strongly depends on its salinity and mineralization. Increased salinity and mineralization of water give rise to conductivity growth of hydrogeological medium. Finding water leak zones is an important problem during planning any building works. The influence of water on the building can be disadvantageous (elution, destruction of the foundations and sulfate aggressiveness). Because of high conductivity of water, watered zones can be recognized with the use of electromagnetic methods. The paper presents results of examination of mineralized water leak zones on the building site of the new CYFRONET building in the Ruczaj quarter, Cracow, Poland. The examinations were conducted with the use of ground conductivity meters. The main goal of the research was to find mineralized water leakage under the foundations of the new-built building.
Źródło:
Przegląd Geologiczny; 2015, 63, 10/1; 814--819
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Variability of horizontal hydraulic conductivity of fen peats from Eastern Poland in relation to function of peatlands as a natural geological barriers
Autorzy:
Rydelek, P.
Bąkowska, A.
Zawrzykraj, P.
Powiązania:
https://bibliotekanauki.pl/articles/2060274.pdf
Data publikacji:
2015
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
hydraulic conductivity
natural geological barriers
peat
valley bog
Opis:
This paper presents the test results of horizontal hydraulic conductivity (k) of fen peats from eastern Poland. Three fen peatlands in the Lubartów Plateau (3 objects marked as LP1, LP2 and LP3) and two in the Siedlce Plateau (2 objects marked as SP1 and SP2) have been selected. Studied objects represent valley bogs type and are similar in peat thickness, but different in the occupied area. They are also vary in terms of botanic compositions and basic physical and chemical parameters of peats. The BAT permeameter was used to in-situ measurements of horizontal hydraulic conductivity. Horizontal hydraulic conductivity of studied peats varies from 1.3×10-8 m/s to 1.1×10-6 m/s. The lowest values of horizontal hydraulic conductivity were observed for silted (high-ash) carbonate peats and amorphous or pseudo-fibrous peats, while the highest values were observed for unsilted (low-ash) non-carbonate peats of fibrous structure. The analysis of variability of horizontal hydraulic conductivity showed that in each case the lowest values were observed for the bottom of the studied profile. The study allowed to indicate the specific areas within the peatlands differing in permeability and identify the role of individual objects as natural geological barriers.
Źródło:
Geological Quarterly; 2015, 59, 2; 426--432
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
New magnetic anomalies of the Outer Carpathians in NE Slovakia and their relationship to the Carpathian Conductivity Zone
Autorzy:
Kucharič, L.
Bezák, V.
Kubeš, P.
Konečný, V.
Vozár, J.
Powiązania:
https://bibliotekanauki.pl/articles/2060028.pdf
Data publikacji:
2013
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Western Carpathians
Flysch belt
Magnetic anomalies
Subvolcanic bodies
Carpathian Conductivity Anomaly
Opis:
A hitherto unknown magnetic anomaly has been detected in the framework of assembling magnetic picture of the Slovakian territory. The impressive magnetic object was recognized in the northeasternmost part of Slovakia within the area which is created by sediments of the Flysch belt. This is certain rarity because the Flysch sequence is practically without magnetic rocks. Due to this was obvious that anomaly is caused by an exotic rocks complex, intruded into Flysch sediments. The shape and the character of anomalous body indicated that source of anomaly is located in the shallow depth under surface relatively. The anomaly has been modelled in the 2D. Source of magnetic anomaly was interpreted as the product of Neogene volcanism – neck of intermediate rocks. Besides of this there were found out other minor anomalies within this area which might be caused also by smaller subvolcanic bodies. The Carpathian Conductivity Anomaly is located in the proximity of new observed magnetic anomalies. Due to this fact it is possible to open new view on the importance of this zone. In the case of justification of such interpretation the area might be interesting for its potential prognosis of hydrocarbons occurrence, metallogenetic prominence, as well as possibilities for underground storage of carbon dioxide.
Źródło:
Geological Quarterly; 2013, 57, 1; 123--134
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Nowa metoda pomiaru współczynnika filtracji osadów dennych
A new method of measuring the hydraulic conductivity of the bottom sediment
Autorzy:
Marciniak, M.
Chudziak, Ł.
Powiązania:
https://bibliotekanauki.pl/articles/2075434.pdf
Data publikacji:
2015
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
filtrometr
gradientomierz
drenaż
infiltracja
współczynnik filtracji
filtrometer
gradientmeter
drainage
infiltration
hydraulic conductivity
Opis:
Interaction of surface water and groundwater is an important element of issue in hydrogeological measurements. Surface water may infiltrate into the subsurface through the bed sediments of rivers and water reservoirs. An opposite direction of reverse water flow through these sediments is also possible with groundwater seeping into surface water. The paper presents two new measuring apparatus: a so-called “filtrometer” and a “gradientmeter”. The filtrometer enables measuring the intensity of water filtration through bed sediments, both during drainage and infiltration. The gradientmeter is designed to measure the hydraulic gradient in the bed sediments. After measuring both of these parameters, it is possible to determine the in situ hydraulic conductivity of these sediments. Usability testing of the new devices was performed under field conditions. The filtrometer and the gradientmeter were used to determine the drainage conditions of a tested section of the Parsêta river. The drainage volume measured with the instruments was in good agreement accordance with the value obtained using the differential water flow method. The proposed new method way of determining the hydraulic parameters of the bed sediments extends the present scope of hydrogeological research.
Źródło:
Przegląd Geologiczny; 2015, 63, 10/2; 919--925
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zmienność współczynnika filtracji w strefie hyporeicznej w świetle badań laboratoryjnych
Variability of the hydraulic conductivity in the hyporheic zone in the light of laboratory research
Autorzy:
Marciniak, M.
Szczucińska, A.
Kaczmarek, M.
Powiązania:
https://bibliotekanauki.pl/articles/2075584.pdf
Data publikacji:
2017
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
strefa hyporeiczna
współczynnik filtracji
badania laboratoryjne
hyporheic zone
hydraulic conductivity
laboratory research
Opis:
The interaction between surface water and groundwater throughout the hyporheic zone determines the diurnal water level fluctuations in springs, streams and lakes. The previous studies have listed evapotranspiration, variability of hydraulic conductivity in the hyporheic zone, melting andfreeze-thawing processes, thermal expansion and water viscosity among the factors responsible for the water level diurnal fluctuations. The aim of the research was to investigate the variability of hydraulic conductivity in the hyporheic zone and its impact on the diurnal fluctuations of the water level. Experimental series were performed in laboratory conditions using seepage columns. Four types of sand sediments, with a hydraulic conductivity ranging from 6x10-6 to 5x10-4 m/s, were tested. The obtained values of hydraulic conductivity appeared to depend on the sand grain size, temperature, the direction of the hydraulic gradient, and the fluidization of the sediment (flowing sand). In all tests, higher hydraulic conductivity values were observed when water was set to flow in the direction opposite to gravity (flow up) rather than downward (flow down). In the sediments, which have not reached the state of fluidization, with an increase of the hydraulic gradient, values of hydraulic conductivity were two times higher during flow up than in the case of flow down. In the case of sediments being fluidized, the obtained values of hydraulic conductivity were roughly 3 times higher. The initiation of the fluidization process has been observed at the hydraulic gradient close to one. The results of laboratory experiments allow for a better understanding of the factors that have impact on diurnal fluctuations of the water level, especially when seepage of groundwater is present. Fluidization of the hyporheic zone after precipitation or thawing events may inhibit diurnal fluctuations.
Źródło:
Przegląd Geologiczny; 2017, 65, 11/1; 1115--1120
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Terrestrial heat flow density in Poland - a new approach
Autorzy:
Szewczyk, J.
Gientka, D.
Powiązania:
https://bibliotekanauki.pl/articles/2059118.pdf
Data publikacji:
2009
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
alaeoclimate
Weichselian glaciation
well logging
geothermics
thermal conductivity
terrestrial heat flow density
Opis:
The Earth’s thermal field, particularly the heat flow density (HFD), is a valuable source of information on geodynamic processes within the Earth’s crust, conditions for hydrocarbon generation and on ar eas and formations promising for geothermal energy. Lithospheric thermal and rheological modelling is critically dependent on high-quality surface heat flow values. The available maps of heat flow density, not only for the area of Poland, are not reliable from the point of view of the current state of knowledge. The main critical factorin determining heat flow density is the knowledge of depth distribution of thermal conductivity. We used a new method of estimating the thermal conductivity from well logging data interpretation with control calibration based on laboratory determined thermal parameters. We con sider that the observed vertical variations of HFD in the shallow part of profiles (<2000 m) are mainly due to a Holocene warming. We have proposed a new original method of determination of HFD based on modelling of palaeoclimatic ef fect. Using this method, we have calculated new HFD values for 308 deep boreholes and completed a new map of this parameter for Poland, which is the first of this type. We propose to undertake a critical analysis of all the existing heat flow data not only for Europe that may change the present understanding of global heat flow.
Źródło:
Geological Quarterly; 2009, 53, 1; 125-140
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Problematyka badań współczynnika filtracji w aparacie trójosiowego ściskania
On the issue of hydraulic conductivity tests using a triaxial compressi apparatus
Autorzy:
Kaczmarek, Łukasz
Dąbska, Agnieszka
Popielski, Paweł
Powiązania:
https://bibliotekanauki.pl/articles/2087059.pdf
Data publikacji:
2022
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
przewodność hydrauliczna
przepływ wody
gradient hydrauliczny
stan naprężenia
hydraulic conductivity
water flow
hydraulic gradient
stress state
Opis:
Laboratory tests, which enable determination of the permeability properties of soil, are distinguished by the accuracy and relatively shorttesttime. Moreover, laboratory methods using a triaxial compression apparatus expand capability for tests with a different filtration regime and a spatial stress state applied on the analysed material. Such flexibility of research procedures allows for a number of scientific and engineering applications. The article outlines the construction of the triaxial apparatus system dedicated to filtration tests, their procedure, and important interpretation aspects.
Źródło:
Przegląd Geologiczny; 2022, 70, 5; 417--423
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zastosowanie metody konduktometrycznej do typowania stref o zmiennych parametrach filtracyjnych w obrębie podstawy wału przeciwpowodziowego
Application of the conductivity methods to select zones with variable filtration parameters around the base of river levee
Autorzy:
Cygal, A.
Stefaniuk, M.
Kret, A.
Klityński, W.
Powiązania:
https://bibliotekanauki.pl/articles/2075405.pdf
Data publikacji:
2015
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
metody konduktometryczne
wał przeciwpowodziowy
przebicie hydrauliczne
geofizyka niesejsmiczna
conductivity methods
river levee
subsurface erosion
non-seismic geophysics
Opis:
The need to continuously monitor the flood embankment is necessary to introduce the measurement methods which give quick results in crisis situations. The protection of embankments as well as the prevention from floods are not only associated with the examination of the body river levee. Experience suggests that one of the problems involves the unknown geotechnical conditions of the levee base. Unfortunately, point geotechnical surveys carried out with a big measurement step were not able to fully identify the lithology variation over larger areas. This is caused by the high cost of drilling shallow wells. The application of non-invasive geophysical methods allows the completion of geotechnical research, and supplies additional information about the variability of geological medium. The structure in the area of the former river beds creates favorable conditions for carrying out geophysical surveys dependent on the variability of geoelectrical properties of rocks. This problem is solved by the use of conductivity method on the 100 m long part of the flood bank. This is recommended for quick and non-invasive measurements. A complex interpretation of geotechnical, hydrogeological and geophysical data provided information about the variability of geoelectrical parameters over this area and therefore made it possible to identify areas prone for greater filtration during high water levels.
Źródło:
Przegląd Geologiczny; 2015, 63, 10/1; 652--656
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Iły poznańskie jako izolacyjne bariery geologiczne składowisk odpadów komunalnych
Poznań Clays as a geological barriers for the disposal sites of municipal wastes
Autorzy:
Gawriuczenkow, I.
Powiązania:
https://bibliotekanauki.pl/articles/2074354.pdf
Data publikacji:
2005
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
bariera geologiczna
iły poznańskie
odpady komunalne
składowisko odpadów komunalnych
mineral barriers
hydraulic conductivity
void ratio
Poznań clays
Opis:
Projects for the storage of municipal waste involve systems of successive safety barriers consisting at least of a geomembrane and a natural mineral layer. “Poznań Clay” are among materials which can be used as a mineral layer. In this paper mineral layers standards from different countries are described. Studies of the important properties of “Poznań Clay” such as hydraulic conductivity, mineral composition, and void ratio are presented. Samples with undisturbed and disturbed structure were examined. Differences between properties of these samples are negligible.
Źródło:
Przegląd Geologiczny; 2005, 53, 8; 691--694
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Krótki przegląd badań współczynnika filtracji gruntów
Brief overview of soil hydraulic conductivity testing methods
Autorzy:
Popielski, Paweł
Dąbska, Agnieszka
Kaczmarek, Łukasz
Powiązania:
https://bibliotekanauki.pl/articles/2087057.pdf
Data publikacji:
2022
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
przewodność hydrauliczna
klasyfikacja metod badawczych
gradient hydrauliczny
typ gleby
hydraulic conductivity
classification of test methods
hydraulic gradient
soil type
Opis:
Many research methods enable the determination of the permeability properties of the soil. These methods differ, inter alia, in accuracy, complexity, application ranges, and technical conditions. The choice of a particular method is often dictated by the purpose of determining the hydraulic conductivity. The review of the most popular methods facilitates the optimization of the selection, as well as the application of mutually verifying methods or using them at different stages of the research. The article summarizes selected methods of determining the soil hydraulic conductivity from common research groups, including correlation, laboratory, and field methods, as well as less frequently used geophysical methods.
Źródło:
Przegląd Geologiczny; 2022, 70, 5; 410--416
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zagadnienie parametryzacji hydrogeologicznej regionalnych modeli ustalonego przepływu wód podziemnych
A problem of the hydrogeological parametrization of the regional steady-state groundwater flow models
Autorzy:
Śmietański, L.
Filar, S.
Olesiuk, G.
Piasecka, A.
Tokarska, A.
Powiązania:
https://bibliotekanauki.pl/articles/2075249.pdf
Data publikacji:
2015
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
parametryzacja hydrogeologiczna
przewodność hydrauliczna
współczynnik filtracji
model przepływu wód podziemnych
hydrogeological parametrization
hydraulic transmissivity
hydraulic conductivity
groundwater flow model
Opis:
The paper presents two already used in practice ways of the hydrogeological parametrization of the regional groundwater flow models. One way is the use of the hydraulic transmissivity resulting in the construction of the authors called “T” models for use in the groundwater resources quantitative assessments. The second way is the use of the hydraulic conductivity k to construct what the authors call the “k” models used for the evaluation of the Main Groundwater Reservoirs protection zones. The authors also present their attitude to the randomization of the hydrogeological parameters.
Źródło:
Przegląd Geologiczny; 2015, 63, 10/2; 1105--1110
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Oznaczanie współczynnika filtracji ośrodków anizotropowych o strukturze warstwowej
Determining the hydraulic conductivity of layered anisotropic media
Autorzy:
Żak, S.
Powiązania:
https://bibliotekanauki.pl/articles/2063184.pdf
Data publikacji:
2008
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
współczynnik filtracji
anizotropia
ośrodek o strukturze warstwowej
permeametr
metoda różnic skończonych
hydraulic conductivity
anisotropy
layered medium
permeameter
finite difference method
Opis:
W artykule przedstawiono formułę wyrażającą wartość zastępczego współczynnika filtracji dla dowolnego kierunku przepływu w ośrodku o strukturze warstwowej. Przedstawiono również wyrażenie na obliczanie kąta między kierunkiem gradientu hydraulicznego (gradH) a kierunkiem prędkości filtracji v. Ta różnica kierunków powinna być uwzględniana przy badaniu współczynnika filtracji w permeametrach. Jest to jednak praktycznie niemożliwe do spełnienia. W permeametrach kierunek gradH jest zwykle zbliżony do kierunku prędkości filtracji v. W przypadku przepływu w kierunku ukośnym do ułożenia warstw (innym niż kierunki główne tensora wodoprzepuszczalności) powoduje to powstanie błędów w oznaczaniu zastępczego współczynnika filtracji. W artykule oszacowano wielkość tych błędów. W tym celu porównano obliczenia teoretyczne, uwzględniające zróżnicowanie kierunków gradH i v, z numerycznymi obliczeniami przepływu odpowiadającymi warunkom wykonywania badania w permeametrze. Wynikają stąd praktyczne wnioski związane z oznaczaniem elipsy współczynnika filtracji ośrodków anizotropowych.
The article presents a formula expressing the value of equivalent hydraulic conductivity for any possible flow direction in a layered medium. It also presents an expression for calculating the angle between the direction of hydraulic gradient (gradH) and the direction of filtration velocity v. This difference in directions should be also taken into account when investigating hydraulic conductivity in permeameters. However, it is often practically impossible as the gradHdirection in permeameters is usually close to the direction of filtration velocity v. When the flow direction is oblique to layering (it is different from the main directions of permeability tensor), it causes errors in determining equivalent hydraulic conductivity. The article estimates the size of these errors. With this aim, theoretical calculations, allowing for the difference in gradH and v directions, were compared with numerical flow calculations appropriate for permeameter test conditions. They lead to practical conclusions concerning the determination of the hydraulic conductivity ellipse for anisotropic media.
Źródło:
Biuletyn Państwowego Instytutu Geologicznego; 2008, 431, Hydrogeologia; 297--304
0867-6143
Pojawia się w:
Biuletyn Państwowego Instytutu Geologicznego
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Ocena parametrów filtracyjnych iłów warwowych ze stanowiska Plecewice k. Sochaczewa w warunkach in situ
Assessment of permeability parameters of in situ tested varved clays from Plecewice near Sochaczew
Autorzy:
Zawrzykraj, P.
Powiązania:
https://bibliotekanauki.pl/articles/2075674.pdf
Data publikacji:
2017
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
piezometr BAT
dylatometr Marchetti
przewodnictwo hydrauliczne
ciśnienie porowe
dyssypacja
BAT piezometer
Marchetti dilatometer
hydraulic conductivity
pore pressure dissipation
varved clays
Opis:
Vistulian Glaciation ice-dammed lake clays with a varved texture were investigated. The study was focused on numerical determination of horizontal permeability depending on the depth and clay content. Direct assessment of these parameters is a rather complex and time-consuming issue. Therefore, a shortened methodology is offered based on the obtained relationships and the analysis of the dissipation process of excess pore pressure. The studies included mainly in situ tests: Marchetti dilatometer test (DMT) and BAT piezometer test. These methods allowed obtaining the values of the coefficient ofpermeability kh and changeability ofpore pressure u0 in a vertical profile. Investigations included 17 permeability tests using a BAT piezometer and 6 measurements of the coefficient of permeability kh, based on dissipation DMT tests. Results of in situ tests were compared with laboratory test results of the clay content. Values of the horizontal coefficient ofpermeability kh were correlated with the clay content f of varved clays. This relationship shows a high coefficient of correlation. A new formula was also proposed for the prediction of the coefficient of permeability kh in varved clays based on the pore pressure u0 stabilization curve, and thus shortening significantly the process of the coefficient kh determination.
Źródło:
Przegląd Geologiczny; 2017, 65, 9; 587--596
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zastosowanie badań konduktometrycznych z użyciem inwersji 1D, jako narzędzia do kartowania przestrzennego przypowierzchniowych warstw geologicznych
Application of ground conductivity meter data for mapping of geological subsurface layers with the use of 1D inversion
Autorzy:
Czarniak, P.
Pacanowski, G.
Sobótka, P.
Powiązania:
https://bibliotekanauki.pl/articles/2075715.pdf
Data publikacji:
2017
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
mierniki przewodności elektrycznej
GCM
tomografia elektrooporowa
ERT
rozwój innowacji drogowych
RID
inwersja 1D
Ground Conductivity Meters
electrical resistivity tomography
1D inversion
Opis:
This article presents the results obtained from geophysical measurements as a supplement to and refinement of geological information obtained from engineering geological studies for the newly constructed highways. The research was conducted using two geophysical methods: Ground Conductivity Meters (GCM) and Electrical Resistivity Tomography (ERT). The above measurements were made on three research fields located along the planned express road S-19 (Kraśnik-Janów Lubelski section). These areas were selected due to the large amount of available archival data and varied geological conditions. The publication focuses primarily on the presentation of the results obtained using the very fast and extremely efficient GCM method. By processing GCM data, using Laterally Constrained Inversion (LCI) and Spatially Constrained Inversion (SCI) algorithms, the values ofelectrical resistivity of the surveyed centers were derived. The results are presented in the form of cross-sections and maps of electrical resistivity from different depths, which were collated and compared with the results from another geophysical method, ERT. These examples show that the use of inversion has a significant impact on the refinement of geological boundaries between layers of different electrical resistivities. Thanks to the correlation of geophysical data with boreholes and engineering geological probes, detailed models of the geological structure of the analyzed areas were elaborated, which are necessary for the selection of appropriate solutions for the construction and modernization of road infrastructure.
Źródło:
Przegląd Geologiczny; 2017, 65, 10/2; 803--810
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Wyświetlanie 1-15 z 19

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