Przeglad Geologiczny最新文献_第9页

Od geologicznego parku krajobrazowego do geoparku globalnego (1991-2021) 从地质景观公园到世界地质公园（1991-2021）

Przeglad Geologiczny Pub Date : 2021-06-21 DOI: 10.7306/2021.15

Tymoteusz Wróblewski

引用次数: 4

Nowe znaleziska polskich tektytów z obszaru niecki żytawskiej Zittau盆地波兰闪长岩的新发现

Przeglad Geologiczny Pub Date : 2021-05-11 DOI: 10.7306/2021.114

Karolina Paszcza

引用次数: 1

Temperatura wód podziemnych i jej znaczenie w badaniach hydrogeologicznych 地下水温度及其在水文地质研究中的重要性

Przeglad Geologiczny Pub Date : 2021-05-11 DOI: 10.7306/2021.12

S. Staśko, S. Buczyński, Marek Błachowicz

引用次数: 1

Zmienność cech fizycznych i chemicznych wód źródlanych w zlewni Zagórzańskiego Potoku (Pogórze Spisko-Gubałowskie) Zagórzańskie Potok流域（Spisko Gubałowskie Pogór ze）泉水物理和化学特征的可变性

Przeglad Geologiczny Pub Date : 2021-03-30 DOI: 10.7306/2021.9

G. Czarny, Joanna Pociask-Karteczka, Z. Nieckarz

{"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":null,"pages":null},"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}

引用次数: 0

Dziedzictwo geologiczne 地质遗迹

Przeglad Geologiczny Pub Date : 2021-02-03 DOI: 10.7306/2021.1

J. Urban, P. Migoń, B. Radwanek-Bąk

引用次数: 2

Trudności w wyznaczaniu osuwisk na obszarach historycznych i zurbanizowanych na przykładzie Twierdzy Przemyśl 确定历史和城市化地区山体滑坡的困难——以Przemyśl要塞为例

Przeglad Geologiczny Pub Date : 2020-12-21 DOI: 10.7306/2020.39

Edyta Rycio

{"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":null,"pages":null},"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}

引用次数: 0

Trzeci wymiar geologii złoża rud miedzi 铜矿地质的第三维度

Przeglad Geologiczny Pub Date : 2020-12-21 DOI: 10.7306/2020.37

M. Twardowski, W. Kaczmarek, R. Rożek

引用次数: 0

Własność złóż kopalin a kryterium społeczno-gospodarczego przeznaczenia gruntu w prawie polskim 矿床性质与波兰法律中的社会经济用地标准

Przeglad Geologiczny Pub Date : 2020-11-23 DOI: 10.7306/2022.30

D. Kowal

引用次数: 0

Szybkość uwalniania się 222Rn z wód podziemnych do atmosfery 地下水向大气中222Rn的释放速率

Przeglad Geologiczny Pub Date : 2020-11-23 DOI: 10.7306/2022.27

T. Przylibski, P. Maciejewski, K. Zagożdżon, P. Zagożdżon

{"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":null,"pages":null},"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}

引用次数: 1

Zastosowanie ziemskich izotopów kosmogenicznych w datowaniu glin lodowcowych – potencjał, ograniczenia i perspektywy badawcze 陆地宇宙成因同位素在冰川粘土年代测定中的应用——潜力、局限性和研究前景

Przeglad Geologiczny Pub Date : 2020-10-21 DOI: 10.7306/2020.32

Karol Tylmann, Damian Moskalewicz

引用次数: 0