(Table 4) Forms of iron, aluminum, and silicon in mountainous tundra soils from the Rai-Iz Massif
Cobertura |
MEDIAN LATITUDE: 66.858860 * MEDIAN LONGITUDE: 65.504085 * SOUTH-BOUND LATITUDE: 66.850140 * WEST-BOUND LONGITUDE: 65.326000 * NORTH-BOUND LATITUDE: 66.867580 * EAST-BOUND LONGITUDE: 65.682170 * DATE/TIME START: 2007-07-01T00:00:00 * DATE/TIME END: 2007-07-01T00:00:00 * MINIMUM DEPTH, sediment/rock: 0.02 m * MAXIMUM DEPTH, sediment/rock: 0.61 m |
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Data(s) |
13/06/2012
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Formato |
text/tab-separated-values, 108 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.815782 doi:10.1594/PANGAEA.815782 |
Idioma(s) |
en |
Publicador |
PANGAEA |
Relação |
doi:10.1594/PANGAEA.815783 Lesovaya, SN; Goryachkin, Sergey V; Polekhovskii, Yu S (2012): Soil formation and weathering on ultramafic rocks in the mountainous tundra of the Rai-Iz massif, Polar Urals. Eurasian Soil Science, 45(1), 33-44, doi:10.1134/S1064229312010097 Vorob'eva, LA (1998): Chemical analysis of soils. Izd. Mosk. Gos. Univ., Moscow, 272 pp (See for Bascomb's, Tamm's and Mehra-Jackson's method) |
Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
Palavras-Chave | #Aluminium oxide; DATE/TIME; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Event label; Iron oxide, Fe2O3; Percentage; Pit_Y-01-07; Pit_Y-02_03-07; Rai-Iz Massif, Polar Ural; Silicon dioxide; Site; SOIL; Soil horizon; Soil profile; Soil type |
Tipo |
Dataset |