{"title":"Nowe znaleziska polskich tektytów z obszaru niecki żytawskiej","authors":"Karolina Paszcza","doi":"10.7306/2021.114","DOIUrl":"https://doi.org/10.7306/2021.114","url":null,"abstract":"","PeriodicalId":35787,"journal":{"name":"Przeglad Geologiczny","volume":"1 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2021-05-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"71109239","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Temperatura wód podziemnych i jej znaczenie w badaniach hydrogeologicznych","authors":"S. Staśko, S. Buczyński, Marek Błachowicz","doi":"10.7306/2021.12","DOIUrl":"https://doi.org/10.7306/2021.12","url":null,"abstract":"","PeriodicalId":35787,"journal":{"name":"Przeglad Geologiczny","volume":"1 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2021-05-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"71109185","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Variability of physical and chemical properties of spring water in the Zagórzański Stream 69: A b s tr a c t. The aim of the paper is to examine the variability ofphysical and chemical characteristics of two springs located in the Zagórzański Stream catchment (Spisko-Gubalowskie Foothills, Podhale region). Cal careous tufa occurs at one of the investigated springs. Field studies were conducted once a month from 25th March 2017 to 28thFebruary 2018. Water Z Nieckarz o f the studied springs represents the bicarbonate-calcium-magnesium type during almost the whole year. The chemical composition of both springs is characterized by seasonal variability. The highest concentrations o f most ions occurred in the summer, when the rainfall was the lowest and during winter drought; while the lowest concentration - in the period of increased rainfall. The variability ofphysical and chemical parame ters of the spring with tufa is smaller than the other one. The spring with calcareous tufa stands out by the higher concentration ofMg2+ and SO42- and the presence of radon. The unique landscape values of the surroundings and hydrogeochemicalfeatures of the spring with calcareous tufa favour this place as an interesting hydro-tourism attraction in the Bukowina Tatrzańska region.
Zagórzański溪泉水物理和化学性质的变化69：A b s tr A c t。本文的目的是研究Zagór zański溪流域（Spisko-Gubalowskie Foothills，Podhale地区）两个泉水物理和化学品特征的变化。Calcareous tufa出现在其中一个被调查的泉水中。从2017年3月25日至2018年2月28日，每月进行一次实地研究。所研究的泉水Z Nieckarz o几乎全年都代表碳酸氢钙-镁类型。两个泉水的化学成分都具有季节性变化的特点。大多数离子的最高浓度出现在降雨量最低的夏季和冬季干旱期间；而最低浓度-在降雨量增加的时期。含凝灰岩的春季的物理和化学参数变化较小。石灰性凝灰岩的泉水以较高的Mg2+和SO42-浓度以及氡的存在而引人注目。周围环境的独特景观价值和带有钙质凝灰岩的泉水的水文地球化学特征使这里成为布科维纳-塔尔扎恩斯卡地区一个有趣的水文旅游景点。
{"title":"Zmienność cech fizycznych i chemicznych wód źródlanych w zlewni Zagórzańskiego Potoku (Pogórze Spisko-Gubałowskie)","authors":"G. Czarny, Joanna Pociask-Karteczka, Z. Nieckarz","doi":"10.7306/2021.9","DOIUrl":"https://doi.org/10.7306/2021.9","url":null,"abstract":"Variability of physical and chemical properties of spring water in the Zagórzański Stream 69: A b s tr a c t. The aim of the paper is to examine the variability ofphysical and chemical characteristics of two springs located in the Zagórzański Stream catchment (Spisko-Gubalowskie Foothills, Podhale region). Cal careous tufa occurs at one of the investigated springs. Field studies were conducted once a month from 25th March 2017 to 28thFebruary 2018. Water Z Nieckarz o f the studied springs represents the bicarbonate-calcium-magnesium type during almost the whole year. The chemical composition of both springs is characterized by seasonal variability. The highest concentrations o f most ions occurred in the summer, when the rainfall was the lowest and during winter drought; while the lowest concentration - in the period of increased rainfall. The variability ofphysical and chemical parame ters of the spring with tufa is smaller than the other one. The spring with calcareous tufa stands out by the higher concentration ofMg2+ and SO42- and the presence of radon. The unique landscape values of the surroundings and hydrogeochemicalfeatures of the spring with calcareous tufa favour this place as an interesting hydro-tourism attraction in the Bukowina Tatrzańska region.","PeriodicalId":35787,"journal":{"name":"Przeglad Geologiczny","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2021-03-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"49221020","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Dziedzictwo geologiczne","authors":"J. Urban, P. Migoń, B. Radwanek-Bąk","doi":"10.7306/2021.1","DOIUrl":"https://doi.org/10.7306/2021.1","url":null,"abstract":"","PeriodicalId":35787,"journal":{"name":"Przeglad Geologiczny","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2021-02-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"47172033","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Difficulties in determining landslides in historical and urbanized areas – a case study of the Przemyśl Fortress. A b s t r a c t.The Przemyoel Fortress is a huge complex of defensive objects from the turn of the 19 th and 20 th centuries. Various types of objects, ruins and remains of the fortress and signs of fights have been preserved to different extents in the area to this day. They constitute a huge problem when determining landslides. The greatest difficulties are caused by vegetation-covered ruins of forts, trenches, remnants of ramparts and defense ditches, and signs of fights preserved in places. Such residues can be interpreted as a landslide or a part of it, especially if they occur in a neighbourhood or inside a landslide. The problem then arises of clearly identifying the boundaries of the landslide and the correct identification of its internal forms, e.g. a devastated trench around the fort can be marked as a landslide. Similar difficulties are provided by numerous inactive quarries, excavations, clay pits, e.g. a closed limestone open-pit mine from the 19 th century, located in Kruhel Wielki. Elements of the old mine are deceptively reminiscent of intra-field forms and they are difficult to separate from the real colluvial forms of the neighbouring landslide. Difficulties in determining landslides arise not only from the history of this region and its geological structure, but also from the degree of urbanization of the area. Strong anthropopression blurs the natural morphology of the slopes, and the limited availability of the area makes cartographic work difficult. It is difficult to distinguish between natural and artificial forms in such areas. Good examples are landslides on the ski slope, on the municipal cemetery, in the castle park and in the area of military areas, housing estates and allotments.
{"title":"Trudności w wyznaczaniu osuwisk na obszarach historycznych i zurbanizowanych na przykładzie Twierdzy Przemyśl","authors":"Edyta Rycio","doi":"10.7306/2020.39","DOIUrl":"https://doi.org/10.7306/2020.39","url":null,"abstract":"Difficulties in determining landslides in historical and urbanized areas – a case study of the Przemyśl Fortress. A b s t r a c t.The Przemyoel Fortress is a huge complex of defensive objects from the turn of the 19 th and 20 th centuries. Various types of objects, ruins and remains of the fortress and signs of fights have been preserved to different extents in the area to this day. They constitute a huge problem when determining landslides. The greatest difficulties are caused by vegetation-covered ruins of forts, trenches, remnants of ramparts and defense ditches, and signs of fights preserved in places. Such residues can be interpreted as a landslide or a part of it, especially if they occur in a neighbourhood or inside a landslide. The problem then arises of clearly identifying the boundaries of the landslide and the correct identification of its internal forms, e.g. a devastated trench around the fort can be marked as a landslide. Similar difficulties are provided by numerous inactive quarries, excavations, clay pits, e.g. a closed limestone open-pit mine from the 19 th century, located in Kruhel Wielki. Elements of the old mine are deceptively reminiscent of intra-field forms and they are difficult to separate from the real colluvial forms of the neighbouring landslide. Difficulties in determining landslides arise not only from the history of this region and its geological structure, but also from the degree of urbanization of the area. Strong anthropopression blurs the natural morphology of the slopes, and the limited availability of the area makes cartographic work difficult. It is difficult to distinguish between natural and artificial forms in such areas. Good examples are landslides on the ski slope, on the municipal cemetery, in the castle park and in the area of military areas, housing estates and allotments.","PeriodicalId":35787,"journal":{"name":"Przeglad Geologiczny","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2020-12-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"47548282","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Trzeci wymiar geologii złoża rud miedzi","authors":"M. Twardowski, W. Kaczmarek, R. Rożek","doi":"10.7306/2020.37","DOIUrl":"https://doi.org/10.7306/2020.37","url":null,"abstract":"","PeriodicalId":35787,"journal":{"name":"Przeglad Geologiczny","volume":"114 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2020-12-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"71109003","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Własność złóż kopalin a kryterium społeczno-gospodarczego przeznaczenia gruntu w prawie polskim","authors":"D. Kowal","doi":"10.7306/2022.30","DOIUrl":"https://doi.org/10.7306/2022.30","url":null,"abstract":"","PeriodicalId":35787,"journal":{"name":"Przeglad Geologiczny","volume":"18 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2020-11-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"71112039","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
T. Przylibski, P. Maciejewski, K. Zagożdżon, P. Zagożdżon
222 Rn release rate from groundwater to the atmosphere. Prz. Geol., 70: 742–750; doi: 10.7306/2022.27 A b s t r a c t. The authors conducted studies on the re- lease rate of 222 Rn from groundwater flowing out of a spring, from metamorphic reservoir rocks. This source gives rise to a stream about 205 m long. The activity concentration of 222 Rn in the spring was about 700 Bq/dm 3 . We found that the rate of radon release into the atmosphere was best described by a third degree polynomial function. This means that the rate of radon release to the atmosphere decreases with distance from the spring. This process is accelerated by all zones of turbulent water flow in the stream – cascades, waterfalls, rapids, and similar zones. The decrease in the radon concentration to the values characteristic for surface waters in the investigated stream, which was a constant and minimum value, equal to about 1 Bq/dm 3 , took place at a distance of about 170–180 metres from the spring. With regard to the water flow path, flow time and the volume of water flowing through the cross-section of the tested stream, the exhalation coefficient of 222 Rn from water to atmospheric air is 3.80 Bq/dm 3 /m, 1.51 Bq/dm 3 /s and 1.25 Bq/dm 3 /dm 3 , respctively. According to the authors, further research conducted in other springs occurring in other types of rocks and under different flow conditions (at different times of the year) will allow characterizing the dynamics of the process of 222 Rn release from groundwater through surface waters into the atmosphere. Per-haps this process can be described with a universal mathematical function.
222 Rn从地下水向大气的释放速率。Prz。Geol。，70:742–750；doi:10.7306/222.27 A b s t r A c t。作者对从泉水流出的地下水和变质储层岩石中重新释放222 Rn的速率进行了研究。这个源头产生了一条长约205米的溪流。春季222 Rn的活性浓度约为700 Bq/dm3。我们发现，氡释放到大气中的速率最好用三次多项式函数来描述。这意味着氡释放到大气中的速率随着距离泉水的距离而降低。这一过程被溪流中的所有湍流区域加速——瀑布、瀑布、急流和类似区域。氡浓度在距离泉水约170-180米处下降到所调查溪流地表水的特征值，这是一个恒定的最小值，约等于1 Bq/dm3。关于水的流动路径、流动时间和流过测试流的横截面的水的体积，222 Rn从水到大气的呼气系数分别为3.80 Bq/dm3/m、1.51 Bq/dm2/s和1.25 Bq/dm3/dm3。根据作者的说法，在其他类型的岩石中以及在不同的流动条件下（一年中的不同时间）对其他泉水进行的进一步研究，将有助于表征地下水通过地表水向大气释放222 Rn的过程动力学。也许这个过程可以用一个通用的数学函数来描述。
{"title":"Szybkość uwalniania się 222Rn z wód podziemnych do atmosfery","authors":"T. Przylibski, P. Maciejewski, K. Zagożdżon, P. Zagożdżon","doi":"10.7306/2022.27","DOIUrl":"https://doi.org/10.7306/2022.27","url":null,"abstract":"222 Rn release rate from groundwater to the atmosphere. Prz. Geol., 70: 742–750; doi: 10.7306/2022.27 A b s t r a c t. The authors conducted studies on the re- lease rate of 222 Rn from groundwater flowing out of a spring, from metamorphic reservoir rocks. This source gives rise to a stream about 205 m long. The activity concentration of 222 Rn in the spring was about 700 Bq/dm 3 . We found that the rate of radon release into the atmosphere was best described by a third degree polynomial function. This means that the rate of radon release to the atmosphere decreases with distance from the spring. This process is accelerated by all zones of turbulent water flow in the stream – cascades, waterfalls, rapids, and similar zones. The decrease in the radon concentration to the values characteristic for surface waters in the investigated stream, which was a constant and minimum value, equal to about 1 Bq/dm 3 , took place at a distance of about 170–180 metres from the spring. With regard to the water flow path, flow time and the volume of water flowing through the cross-section of the tested stream, the exhalation coefficient of 222 Rn from water to atmospheric air is 3.80 Bq/dm 3 /m, 1.51 Bq/dm 3 /s and 1.25 Bq/dm 3 /dm 3 , respctively. According to the authors, further research conducted in other springs occurring in other types of rocks and under different flow conditions (at different times of the year) will allow characterizing the dynamics of the process of 222 Rn release from groundwater through surface waters into the atmosphere. Per-haps this process can be described with a universal mathematical function.","PeriodicalId":35787,"journal":{"name":"Przeglad Geologiczny","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2020-11-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"48119348","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Application of in situ cosmogenic nuclides in dating glacial till – research potential, limitations and prospects. Prz. Geol., 68: 764–773; doi: 10.7306/2020.32 A b s t r a c t. Determination of numerical age for glacial till is one of the most intriguing issues in glacial geology and geomorphology. Till layers are unequivocal evidence of ice sheets advances and retreats, and therefore they are very important for Quaternary palaeoclimatic reconstructions. Herein, we present a review dedicated to the methodology of glacial till dating with in situ cosmogenic nuclides. This relatively novel approach enables direct dating of depo- sition of till and its exposure after deglaciation. Getting reliable numerical age (in years) of till opens a new prospect for reconstructions of past glaciations and palaeogeographic studies. Despite some limitations of applying in situ cosmogenic exposure and burial dating, we argue that this technique may be successfully employed in studies of glacial deposits in Poland.
{"title":"Zastosowanie ziemskich izotopów kosmogenicznych w datowaniu glin lodowcowych – potencjał, ograniczenia i perspektywy badawcze","authors":"Karol Tylmann, Damian Moskalewicz","doi":"10.7306/2020.32","DOIUrl":"https://doi.org/10.7306/2020.32","url":null,"abstract":"Application of in situ cosmogenic nuclides in dating glacial till – research potential, limitations and prospects. Prz. Geol., 68: 764–773; doi: 10.7306/2020.32 A b s t r a c t. Determination of numerical age for glacial till is one of the most intriguing issues in glacial geology and geomorphology. Till layers are unequivocal evidence of ice sheets advances and retreats, and therefore they are very important for Quaternary palaeoclimatic reconstructions. Herein, we present a review dedicated to the methodology of glacial till dating with in situ cosmogenic nuclides. This relatively novel approach enables direct dating of depo- sition of till and its exposure after deglaciation. Getting reliable numerical age (in years) of till opens a new prospect for reconstructions of past glaciations and palaeogeographic studies. Despite some limitations of applying in situ cosmogenic exposure and burial dating, we argue that this technique may be successfully employed in studies of glacial deposits in Poland.","PeriodicalId":35787,"journal":{"name":"Przeglad Geologiczny","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2020-10-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"48764127","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
京公网安备 11010802042870号
京ICP备2023020795号-1
扫码关注我们
求助内容：
应助结果提醒方式：