GPR and aerial imageries to identify the recent historical course of the Obra River and spatial extent of Obrzańskie Lake, altered by hydro-technical works
Abstract:Ground penetrating radar (GPR) measurements have been conducted to retrace the natural course of the Obra River and changes of spatial extent of Obrzańskie Lake (western Poland). The Obra River valley was subjected to intensive anthropogenic transformation. Three artificial canals were constructed here in the beginning of the nineteenth century. The GPR surveys were done using a georadar MALA ProEx equipped with 250 MHz antenna. The measurement was verified by coring and analyses of historical maps, aerial pho… Show more
“…26% of the total case studies ( Fig. 7b; Table 4) such as (1) water extraction (RI3a) diminishing groundwater transference to natural systems (Endres et al, 2000;Tsoflias et al, 2001;Bevan et al, 2003); (2) point pollution (RI3b) focused mainly on monitoring contamination plumes (Corbeanu et al, 2002;Conant et al, 2004;Talley et al, 2005;Tsoflias and Becker, 2008); (3) civil works (RI3c) modifying groundwater flow of natural courses (Słowik, 2013); (4) agricultural practices (RI3d) altering aquifer recharge rates and mechanisms (Lunt et al, 2005;Lambot et al, 2008); and (5) mining and quarrying practices (RI3e) changing preferential flows (Grandjean and Gourry, 1996) and generating new GDE (Molina-Sánchez et al, 2015). Despite that shallow groundwater propitiated the existence of GDE in most of the case studies, only one study expressly addressed GDE research (Zurek et al, 2015).…”
Section: Hydrogeological Research Interestsmentioning
“…26% of the total case studies ( Fig. 7b; Table 4) such as (1) water extraction (RI3a) diminishing groundwater transference to natural systems (Endres et al, 2000;Tsoflias et al, 2001;Bevan et al, 2003); (2) point pollution (RI3b) focused mainly on monitoring contamination plumes (Corbeanu et al, 2002;Conant et al, 2004;Talley et al, 2005;Tsoflias and Becker, 2008); (3) civil works (RI3c) modifying groundwater flow of natural courses (Słowik, 2013); (4) agricultural practices (RI3d) altering aquifer recharge rates and mechanisms (Lunt et al, 2005;Lambot et al, 2008); and (5) mining and quarrying practices (RI3e) changing preferential flows (Grandjean and Gourry, 1996) and generating new GDE (Molina-Sánchez et al, 2015). Despite that shallow groundwater propitiated the existence of GDE in most of the case studies, only one study expressly addressed GDE research (Zurek et al, 2015).…”
Section: Hydrogeological Research Interestsmentioning
“…1) by means of geophysical (ground-penetrating radar (GPR)) surveys and the analysis of satellite and aerial images. It is a continuation of studies conducted in the Middle Obra valley by Słowik (2011aSłowik ( , 2013. It presents the results of a field research carried out in the area where traces of former river beds were preserved in the modern land surface (Fig.…”
Section: Introductionmentioning
confidence: 82%
“…1). The canals replaced the natural river course characterized by various patterns (meandering, multi-channel and disappearing in wetlands; Słowik 2011a) and influenced changes of spatial extent of lakes situated in the course of the river (Słowik 2013). According to Dynowska (1972), hydrological regime of the Obra River is temperate with spring floods and groundwater-rainfall water supply.…”
At the beginning of the nineteenth century, a significant change in sedimentation took place along the middle course of the Obra River (W Poland): a ''natural'' channel bed was replaced by three artificial canals. Before that time the Obra River bed had been characterized by various river patterns (braided, meandering and disappearing in wetlands). GPR (ground-penetrating radar) surveys and the analysis of satellite and aerial images were carried out to retrace the natural river course near the village of Kopanica. The GPR, ground-truthed with core data, revealed that at least two types of the river pattern had been functioning here before the period of the hydrotechnical works: a large-scale meandering pattern (width-to-depth (w/d) ratio ranging from 15 to 40) and a relatively smallerscale multi-channel pattern (w/d = 11-22). Possibly, the transformation was caused by forming a series of large floods followed by in-channel aggradation and avulsions.
“…c). It represents two wetland depressions (remains of former bays of Obrzańskie Lake; Słowik ) separated by an elevated area composed of fine and medium sands (former lake island).…”
A field experiment aiming to study the influence of measurement conditions on depths of penetration and resolution of GPR surveys was conducted in the middle Obra valley (western Poland). The tests were carried out along five profile lines in three sites representing fluvial, lacustrine and anthropogenic landforms. The GPR surveys were conducted at various hydrogeological conditions: high and low groundwater levels, and in winter conditions when the ground was under snow/ice cover and frozen. The best measurement conditions for imaging the internal structure of fluvial landforms were found during a period of low groundwater levels. At high groundwater levels the bottom parts of radar profiles were obscured by reverberations originating from the differences in the water content between unsaturated and saturated parts of the studied sections. Some sedimentary structures within lacustrine landforms were better seen at high levels when all the deposits were saturated. In winter conditions, high quality radar profiles were obtained only when measurements were conducted on an elevated, anthropogenic landform, unaffected by dispersion and attenuation of the radar signal in the other landforms due to a water layer situated between the ice cover and land surface. It was also shown that it is possible to image sedimentary structures of landforms built of deposits with significant admixtures of silts, although the depths of penetration are reduced in such cases.
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