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Wiek wałów morenowych we wschodniej części przedpola lodowca Fláa (SE Islandia) w oparciu o wyniki datowania lichenometrycznego 基于地衣测年的Fláa冰川（冰岛东南部）东部前院冰碛波年龄
Landform Analysis Pub Date : 2014-09-16 DOI: 10.12657/LANDFANA.024.005
Katarzyna Łuszczak, Aneta Modzelewska, D. Sawicka, Dominika Niezabitowska, M. Dąbski
{"title":"Wiek wałów morenowych we wschodniej części przedpola lodowca Fláa (SE Islandia) w oparciu o wyniki datowania lichenometrycznego","authors":"Katarzyna Łuszczak, Aneta Modzelewska, D. Sawicka, Dominika Niezabitowska, M. Dąbski","doi":"10.12657/LANDFANA.024.005","DOIUrl":"https://doi.org/10.12657/LANDFANA.024.005","url":null,"abstract":"","PeriodicalId":30719,"journal":{"name":"Landform Analysis","volume":"24 1","pages":"45-54"},"PeriodicalIF":0.0,"publicationDate":"2014-09-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"66210347","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
Wpływ spękań ciosowych na kształtowanie przebiegu dolin rzecznych zachodniego Podhala 冲击裂缝对波德黑尔西部河谷形成的影响
Landform Analysis Pub Date : 2014-09-16 DOI: 10.12657/LANDFANA.024.006
K. Majewski
{"title":"Wpływ spękań ciosowych na kształtowanie przebiegu dolin rzecznych zachodniego Podhala","authors":"K. Majewski","doi":"10.12657/LANDFANA.024.006","DOIUrl":"https://doi.org/10.12657/LANDFANA.024.006","url":null,"abstract":"The directions of joints, measured in bedrock outcrops in stream channels, have been compared with the directions of the low-order valleys The results indicate that upper courses of all studied valleys are consistent with the orientation of dominant joint system This correlation can be an evi- dence of valley-forming process along joints of diagonal system In contrast to the upper courses, lower courses of most of the valleys are inconsistent with diagonal joint system According to the research results, the valley directions changed in the course of their development, especially during the Tatra glaciations, when lower courses of the valleys were filled with fluvio-glacial material","PeriodicalId":30719,"journal":{"name":"Landform Analysis","volume":"24 1","pages":"55-64"},"PeriodicalIF":0.0,"publicationDate":"2014-09-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"66210696","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: 2
Wskaźnik średniej rocznej erozyjności deszczu i spływu powierzchniowego (R) na przykładzie stacji meteorologicznej w Łazach k. Bochni (region klimatu Pogórza Karpackiego) Bochnia附近的Łazy气象站（喀尔巴阡山脉气候区）的降雨和地表径流的年均侵蚀率指数（R）
Landform Analysis Pub Date : 2014-09-16 DOI: 10.12657/LANDFANA.024.009
J. Święchowicz
{"title":"Wskaźnik średniej rocznej erozyjności deszczu i spływu powierzchniowego (R) na przykładzie stacji meteorologicznej w Łazach k. Bochni (region klimatu Pogórza Karpackiego)","authors":"J. Święchowicz","doi":"10.12657/LANDFANA.024.009","DOIUrl":"https://doi.org/10.12657/LANDFANA.024.009","url":null,"abstract":": Rainfall and runoff erosivity factor (R) is a key input parameter to the USLE (Universal Soil Loss Equation) and many other models (RUSLE – Revised Universal Soil Loss Equation, USPED – Unit Stream Power based Erosion/Deposition) There is still no precise characteristic of rainfall erosivity in Poland Local R factor values, according to Wischmeier and Smith procedure (1965, 1978) were calculated only for 13 meteorological stations The main aim of the paper is to estimate rainfall and runoff erosivity factor (R) for the Carpathian Foothills climatic region on the basis of 1987–2008 rainfall data for Łazy near Bochnia meteorological station (Wiśnicz Foothills) The average rainfall and runoff factor (R) for Łazy calculated for the years 1987–2008 equalled 106 6 MJ cm ha –1 h –1 This value was bigger in comparison with the values for other locations in western (Wrocław-Swojec), northern (Elbląg) northeastern (Suwałki) or central Poland (Otwock, Sandomierz, Puczniew) and similar to the values for the Carpathians (Lesko, Lima- nowa, Szymbark) The annual values of R factor for Łazy ranged between 27 7 in 1993 and 455 9 MJ cm ha –1 h –1 in 2006 Maximum monthly values of rainfall factor R r in a year varied from 6 1 in July (1993) to 428 7 MJ cm ha –1 h –1 in June (2006) The most intensive potential soil erosion by water due to erosivity of rains is likely to happen in June, July, May and August","PeriodicalId":30719,"journal":{"name":"Landform Analysis","volume":"24 1","pages":"85-95"},"PeriodicalIF":0.0,"publicationDate":"2014-09-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"66210750","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
Możliwości wykorzystania bezzałogowej fotogrametrii lotniczej do identyfikacji przekształceń antropogenicznych w korytach rzecznych 利用无人航空摄影测量识别河床人为变化的可能性
Landform Analysis Pub Date : 2014-09-16 DOI: 10.12657/LANDFANA.024.012
M. Witek, Justyna Jeziorska, Tomasz Niedzielski
{"title":"Możliwości wykorzystania bezzałogowej fotogrametrii lotniczej do identyfikacji przekształceń antropogenicznych w korytach rzecznych","authors":"M. Witek, Justyna Jeziorska, Tomasz Niedzielski","doi":"10.12657/LANDFANA.024.012","DOIUrl":"https://doi.org/10.12657/LANDFANA.024.012","url":null,"abstract":"","PeriodicalId":30719,"journal":{"name":"Landform Analysis","volume":"24 1","pages":"115-126"},"PeriodicalIF":0.0,"publicationDate":"2014-09-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"66210355","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: 7
Próba oceny zróżnicowania nasilenia antropopresji w zlewniach 2. rzędu w Górach Świętokrzyskich 试图评估集水区人类压力强度的多样性2。在西维托克日斯基山脉
Landform Analysis Pub Date : 2014-09-16 DOI: 10.12657/LANDFANA.024.004
K. Koper
{"title":"Próba oceny zróżnicowania nasilenia antropopresji w zlewniach 2. rzędu w Górach Świętokrzyskich","authors":"K. Koper","doi":"10.12657/LANDFANA.024.004","DOIUrl":"https://doi.org/10.12657/LANDFANA.024.004","url":null,"abstract":"","PeriodicalId":30719,"journal":{"name":"Landform Analysis","volume":"24 1","pages":"35-43"},"PeriodicalIF":0.0,"publicationDate":"2014-09-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"66210307","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
Formy biodostępne Cd, Cu, Pb, Zn w osadach den dolin zachodniej części Wyżyny Lubelskiej 卢布林高原西部山谷沉积物中的生物有效态Cd、Cu、Pb、Zn
Landform Analysis Pub Date : 2014-09-16 DOI: 10.12657/LANDFANA.024.007
A. Plak, W. Zgłobicki, L. Lata, M. Telecka
{"title":"Formy biodostępne Cd, Cu, Pb, Zn w osadach den dolin zachodniej części Wyżyny Lubelskiej","authors":"A. Plak, W. Zgłobicki, L. Lata, M. Telecka","doi":"10.12657/LANDFANA.024.007","DOIUrl":"https://doi.org/10.12657/LANDFANA.024.007","url":null,"abstract":"This study was concerned with the content of bio-available forms of Cd, Cu, Pb and Zn in samples collected from the valley bottoms in the western part of the Lublin Upland Analysis was carried out for 55 samples of sediments located at sites with various degrees of anthropogenic pressure The highest percentage of bio-available forms was found in flood plains located in urban and industrial areas This pattern was mostly pronounced in the case of bio-available zinc: its content in the sediments in industrial areas was 5 to 6 times higher than in the other types of profiles For copper, this indicator reached a maximum of 45%, for cadmium 30% The absolute bio-available form content showed a high correlation with the total content, particularly for copper There was also a significant correlation with organic matter content, sand fraction content (Zn) and clay fraction content (Pb and Zn) The accumulation of the bio-available forms of heavy metals (Cd, Cu, Pb and Zn) in the sediments under study is a result of many factors The study findings indicate, however, a correlation between the content of bioavailable forms and the intensity of geochemical pressure - the highest percentage of these forms was found in urban and industrial areas Geomorphic location of the profile was also an important factor","PeriodicalId":30719,"journal":{"name":"Landform Analysis","volume":"24 1","pages":"65-71"},"PeriodicalIF":0.0,"publicationDate":"2014-09-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"66210731","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: 2
Problematyka przywrócenia migracji ryb przez obiekty hydrotechniczne w korytach rzecznych 利用河床水利设施恢复鱼类洄游的问题
Landform Analysis Pub Date : 2014-09-16 DOI: 10.12657/LANDFANA.024.011
M. Wierzbicki
{"title":"Problematyka przywrócenia migracji ryb przez obiekty hydrotechniczne w korytach rzecznych","authors":"M. Wierzbicki","doi":"10.12657/LANDFANA.024.011","DOIUrl":"https://doi.org/10.12657/LANDFANA.024.011","url":null,"abstract":"","PeriodicalId":30719,"journal":{"name":"Landform Analysis","volume":"24 1","pages":"107-113"},"PeriodicalIF":0.0,"publicationDate":"2014-09-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"66210813","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: 2
Przekształcenia powierzchni brzegów rzecznych przez procesy mrozowe 冻结过程对河岸的改造
Landform Analysis Pub Date : 2014-09-16 DOI: 10.12657/LANDFANA.024.001
K. Augustowski, J. Kukulak
{"title":"Przekształcenia powierzchni brzegów rzecznych przez procesy mrozowe","authors":"K. Augustowski, J. Kukulak","doi":"10.12657/LANDFANA.024.001","DOIUrl":"https://doi.org/10.12657/LANDFANA.024.001","url":null,"abstract":"The effects of frost processes on undercut riverbanks in the period November-April, at the turn of 2011/2012 were examined Erosion of the riverbanks in the Czarny Dunajec basin (Orava Basin, Gubalowka Hills) and in the Ropa basin (Low Beskid) was studied by erosion pins and catchers of bank sediments There were 4-5 multigelation periods It has been shown that the frost processes caused the largest erosion in area of rocky banks; erosion was smaller on banks built with medium and coarse gravels, and the smallest on banks built with sands and clays The size of this erosion was influenced not only by lithology and the degree of cohesion, but also the presence and density of cracks","PeriodicalId":30719,"journal":{"name":"Landform Analysis","volume":"24 1","pages":"3-10"},"PeriodicalIF":0.0,"publicationDate":"2014-09-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"66210206","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: 2
Wpływ antropopresji na przemiany środowiskowe w dolinie Warty w Poznaniu 人类压迫对波兹南瓦尔塔山谷环境变化的影响
Landform Analysis Pub Date : 2014-09-16 DOI: 10.12657/LANDFANA.024.003
A. Kaniecki
{"title":"Wpływ antropopresji na przemiany środowiskowe w dolinie Warty w Poznaniu","authors":"A. Kaniecki","doi":"10.12657/LANDFANA.024.003","DOIUrl":"https://doi.org/10.12657/LANDFANA.024.003","url":null,"abstract":"","PeriodicalId":30719,"journal":{"name":"Landform Analysis","volume":"24 1","pages":"23-34"},"PeriodicalIF":0.0,"publicationDate":"2014-09-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"66210292","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: 12
Wybrane analizy geoinformacyjne w badaniach związków budowy geologicznej z rzeźbą terenu Obniżenia Chabówki-Jordanowa Chabówka-Jordanowa凹陷地质构造与雕塑关系研究中的选定地理信息分析
Landform Analysis Pub Date : 2014-09-16 DOI: 10.12657/LANDFANA.024.008
M. Szczęch
{"title":"Wybrane analizy geoinformacyjne w badaniach związków budowy geologicznej z rzeźbą terenu Obniżenia Chabówki-Jordanowa","authors":"M. Szczęch","doi":"10.12657/LANDFANA.024.008","DOIUrl":"https://doi.org/10.12657/LANDFANA.024.008","url":null,"abstract":"This study presents the results of researches on correlation between geological structure and terrain morphology of the Orawa-Jordanów Depression GIS tools and software, as well as remote sensing methods were used in the investigations Lineaments method basing on DEM data was applied too The research area bearing foothill morphology is distinctly depressed from the surrounding it Beskidy ranges The foothills are characterized by lower high peek and relative highs than the Beskids Morphology of the Chabówka-Jordanów Depression is associated with tectonic structure The tectonics determines that Chabówka-Jordanów Depression is intermountain tectonic trough Completed analysis allowed to conclude, that ridges on this terrain are mainly formed of the thick-bedded sandstones of the Magura Formation, and depressions and valleys are dissected in older rocks represented by shale and sandstone-shale complexes Directions of the main ridges and valleys are parallel to extensions of the main fold structures Lineaments marked in studied terrain correlate mainly with faults The lineaments method allowed to conclude that some of valleys exploit the transverse faults","PeriodicalId":30719,"journal":{"name":"Landform Analysis","volume":"24 1","pages":"73-84"},"PeriodicalIF":0.0,"publicationDate":"2014-09-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"66210739","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
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