Zobrazeno 1 - 10
of 18
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
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. 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
Autor:
Arkadiusz Derkowski, Artur Kuligiewicz
Publikováno v:
American Mineralogist. 102:1073-1090
Smectites are able to retain molecular tightly bound water (TBW) at temperatures above 100 °C, even after prolonged drying. The presence of TBW affects the stable isotope ratios, the dehydroxylation behavior of smectites and smectite-rich samples an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2334d2447d456971c4c2adae0a6063df
https://doi.org/10.2138/am-2017-5918
https://doi.org/10.2138/am-2017-5918
Autor:
Artur Kuligiewicz, Arkadiusz Derkowski
Publikováno v:
Applied Clay Science. 136:219-229
Dehydroxylation-rehydroxylation experiments were performed on various dioctahedral aluminous 2:1 layer clay minerals using the precise thermogravimetry (TG) system equipped with a continuous N2 gas flow enriched with H2O vapor of controlled concentra
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::694fe52575182ce5bc456ac1219054f6
https://doi.org/10.1016/j.clay.2016.11.030
https://doi.org/10.1016/j.clay.2016.11.030