Zobrazeno 1 - 10
of 21
pro vyhledávání: '"Artur Kuligiewicz"'
Autor:
Artur Kuligiewicz, Wojciech Szymański, Ilya Bindeman, Mariola Kowalik-Hyla, Zuzanna Ciesielska, Paweł P. Ziemiański, Kazimierz Różański
Publikováno v:
Geoderma, Vol 449, Iss , Pp 116981- (2024)
Pedogenic minerals reflect the environmental conditions that prevailed during soil formation. The present study investigates the clay mineral composition of the fine clay fraction separated from four soil profiles in the Tatra Mountains, Poland. All
Externí odkaz:
https://doaj.org/article/663ddc89217c453a81698456a95c6d6d
Publikováno v:
Geoderma, Vol 449, Iss , Pp 116985- (2024)
Stable isotope compositions of pedogenic clay minerals can be used as a paleoclimatic proxy. The underlying fundamental assumption is that pedogenic clays are formed in isotope equilibrium with the environment, which is well-documented for hot and hu
Externí odkaz:
https://doaj.org/article/391502ba2a95417ebab668e95f5c370f
Autor:
Jan Środoń, Lynda Williams, Marek Szczerba, Tatiana Zaitseva, Maciej J. Bojanowski, Beata Marciniak-Maliszewska, Artur Kuligiewicz, Krzysztof Starzec, Zuzanna Ciesielska, Mariusz Paszkowski
Publikováno v:
Geochimica et Cosmochimica Acta. 352:157-174
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6327562a9ad3c379ed86ce99f9a38d5a
https://doi.org/10.1016/j.gca.2023.05.010
https://doi.org/10.1016/j.gca.2023.05.010
Autor:
Arkadiusz Derkowski, Artur Kuligiewicz
Publikováno v:
Clays and Clay Minerals. 70:946-972
Smectites are a group of minerals traditionally analyzed by thermal methods due to their exceptionally large adsorbed-water contents and the presence of OH groups, which makes them unique among all common soil- and rock-forming minerals. The dehydrat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::997b52c0edf5becdf49a25b6e44dcf89
https://doi.org/10.1007/s42860-023-00222-y
https://doi.org/10.1007/s42860-023-00222-y
Publikováno v:
Geochimica et Cosmochimica Acta. 322:1-23
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e2d87db666e1820388806c7b5ca55dfb
https://doi.org/10.1016/j.gca.2022.01.027
https://doi.org/10.1016/j.gca.2022.01.027
Publikováno v:
Clays and Clay Minerals. 70:1-19
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3e7e91b01c088cebdaaf1617ee7962a2
https://doi.org/10.1007/s42860-022-00176-7
https://doi.org/10.1007/s42860-022-00176-7
Autor:
Murray Moinester, Christian Chmelik, Marija Avramovska, Arkadiusz Derkowski, Vincent J. Hare, Artur Kuligiewicz, Dieter Freude, Jörg Kärger, Jürgen Haase, Alexander Fantalkin
Publikováno v:
Journal of the American Ceramic Society. 104:5328-5340
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::631efb7bd95329169e8cb519a0569b68
https://doi.org/10.1111/jace.17753
https://doi.org/10.1111/jace.17753
Publikováno v:
Clays and Clay Minerals. 70:305-305
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::50c9426b0117c60e34a8214faee7f6cf
https://doi.org/10.1007/s42860-022-00182-9
https://doi.org/10.1007/s42860-022-00182-9
Publikováno v:
Applied Clay Science. 216:106338
Atmospheric water adsorbed onto clay mineral surfaces, of smectite group minerals in particular, can contaminate hydrogen released from structural hydroxyl groups during hydrogen-isotope analysis. Interlayer cation composition and cation hydration en
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::751f2df6b910881899e824f9f5a09cae
https://doi.org/10.1016/j.clay.2021.106338
https://doi.org/10.1016/j.clay.2021.106338
Publikováno v:
Applied Clay Science. 161:354-363
The aim of the present study was to test the applicability of the O-D method, a newly developed spectroscopic layer charge measurement technique, to measure the charge present on wettable surfaces of mixed-layer illite-smectite (I-S). The O-D method
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::14cbc8fd7cd66638ffb49e1f381c0ce4
https://doi.org/10.1016/j.clay.2018.05.003
https://doi.org/10.1016/j.clay.2018.05.003