Zobrazeno 1 - 10
of 1 937
pro vyhledávání: '"clay mineralogy"'
Publikováno v:
Geoenvironmental Disasters, Vol 11, Iss 1, Pp 1-30 (2024)
Abstract Background The weathering intensity and geochemical properties of a rock contribute to shallow landslide occurrences. This study aims to establish the role of rock weathering in shallow slope instability in low-grade metamorphic rocks of the
Externí odkaz:
https://doaj.org/article/494157d538194128a39c5e6a75a4930b
Autor:
Edward L. Lo, Michael M. McGlue, Christopher J. Matocha, Aguinaldo Silva, Giliane G. Rasbold, Sidney Kuerten, Rômullo O. Louzada, Kevin C. Haller
Publikováno v:
Sedimentologika, Vol 2, Iss 1 (2024)
The Pantanal Basin is a low-gradient back-bulge analog for distal depozones associated with retroarc foreland basin systems in the geological record. Extensive lowland environments including fluvial megafans, floodplains, wetlands, and lakes make up
Externí odkaz:
https://doaj.org/article/39d93cbb8c554237bb9d268f8673f3e2
Autor:
Xianming Zhang, Yuntao Jing, Wanfu Zhao, Yongjun Jiang, Dong-Xing Guan, Hongxia Du, Ying Qian, Fei Ye, Wancang Zhao
Publikováno v:
Geoderma, Vol 445, Iss , Pp 116879- (2024)
Rare earth elements (REEs) have gained attention as tracers of pedogenic processes over the last few decades. Clay-sized fractions (CSFs, < 2 μm) may play a crucial role in hosting REEs. To better understand the pedochemical signals of REEs in clay-
Externí odkaz:
https://doaj.org/article/8482e4b3ff5b40c1af079ebe455cd694
Autor:
H.R. Owliaie
Publikováno v:
مجله آب و خاک, Vol 37, Iss 4, Pp 603-620 (2023)
Introduction Soil classification is the systematic categorization of soils based on distinguishing soil characteristics, aiding in the comprehension of soil properties through soil surveys, and establishing suitable strategies for effective soil uti
Externí odkaz:
https://doaj.org/article/ab1b5decb221401e9ff15c2b489e59bf
Publikováno v:
Land, Vol 13, Iss 9, p 1415 (2024)
This article examines the clay mineralogy of twelve representative soils developed from gypsum-rich parent materials on several geomorphic positions. These soils were classified as Haploxerept, plus one profile as Humixerept and another as Xerorthent
Externí odkaz:
https://doaj.org/article/b508056de6dc4dadb99b47251257a420
Autor:
J. W. Marschalek, P.‐H. Blard, E. Sarigulyan, W. Ehrmann, S. R. Hemming, S. N. Thomson, C.‐D. Hillenbrand, K. Licht, J.‐L. Tison, L. Ardoin, F. Fripiat, C. S. Allen, Y. Marrocchi, M. J. Siegert, T. van deFlierdt
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 5, Pp n/a-n/a (2024)
Abstract Provenance records from sediments deposited offshore of the West Antarctic Ice Sheet (WAIS) can help identify past major ice retreat, thus constraining ice‐sheet models projecting future sea‐level rise. Interpretations from such records
Externí odkaz:
https://doaj.org/article/4338bfdfd9d54bd3a524e0528fddaf44