کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
8893761 | 1629192 | 2018 | 12 صفحه PDF | دانلود رایگان |
عنوان انگلیسی مقاله ISI
Genesis of a Holocene soil chronosequence from the southernmost Andes Mountains, Tierra del Fuego
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کلمات کلیدی
موضوعات مرتبط
مهندسی و علوم پایه
علوم زمین و سیارات
فرآیندهای سطح زمین
پیش نمایش صفحه اول مقاله
![عکس صفحه اول مقاله: Genesis of a Holocene soil chronosequence from the southernmost Andes Mountains, Tierra del Fuego Genesis of a Holocene soil chronosequence from the southernmost Andes Mountains, Tierra del Fuego](/preview/png/8893761.png)
چکیده انگلیسی
At the southernmost Andes Mountains, the Martial cirque glacier has retreated 2 km in distance and 500 m in elevation since the mid-Holocene. This study examines soil properties, processes, and classification in relation to soil age and elevation. Soils were sampled at elevations from 430 to 925 m a.s.l. on drifts periodically influenced by volcanic ash that represent five age classes: 5.0 to 6.0 kyr BP under deciduous Nothofagus pumilio forest; 1.3 to 3.2 kyr BP under N. pumilio and N. antarctica forest and tundra; 0.3 to 1.4 kyr BP under tundra; 0.3 Kyr BP CE under tundra; and 0.007 Kyr BP CE under scattered lichens and mosses. The soils represent a developmental sequence on metapellitic rocks ranging from: Cryorthents, Dystrocryepts, Humicryepts, and Humicryods. In general the soils contain abundant coarse fragments, sandy loam textures, and high levels of organic C. Clays have been altered in the soils from chlorite to a hydroxyl-interlayered vermiculite and ferrihydrite. The most developed soils are very strongly acid, Al saturated, and have illuvial horizons enriched in fulvic-acid C and organic-bound forms of free Fe and Al. The following properties are highly correlated with soil age: pyrophosphate soluble iron (Fep) in the B horizon (R2 = 0.97), color-development equivalence in the B horizon (R2 = 0.87), clay content of the B horizon (R2 = 0.68), and fulvic-acid C in the B horizon (R2 = 0.65). The results of this study imply that soil formation in magellanic subantarctic forests and tundra is rapid and involves podsolization, andisolization, and humification as primary soil-forming processes.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: CATENA - Volume 162, March 2018, Pages 291-302
Journal: CATENA - Volume 162, March 2018, Pages 291-302
نویسندگان
Mariana M.F. Sá, Carlos E.G.R. Schaefer, James G. Bockheim, Diego C. Loureiro, Roberto F.M. Michel, Felipe N.B. Simas,