Factors of soils formation of the NW-facing slopes of Limbara relief are described. The climatic factor is considered to be the most important factor in determining the properties of soils in upslope positions (1300-1100 m). The principal soils are Lithie Haplumbrepts. The morphology and vegetation help the development of the soils between 1100 and 800 m. They are Typic Xerumbrepts. Between 800 and 500 m the principal soils are Lithic Xerorthents. Steepness of the slope controls their development.
I Suoli su substrati acidi in Sardegna: nota 2.: i suoli del versante nord-ovest del Massiccio del Limbara / Delogu, G.; Passino, Anna Maria; Pulina, Maria Antonia. - In: STUDI SASSARESI. SEZIONE 3: ANNALI DELLA FACOLTÀ DI AGRARIA DELL'UNIVERSITÀ DI SASSARI. - ISSN 0562-2662. - 28 (1980-1981):(1981), pp. 295-311.
I Suoli su substrati acidi in Sardegna: nota 2.: i suoli del versante nord-ovest del Massiccio del Limbara
Delogu, G.;Pulina, Maria Antonia
1981-01-01
Abstract
Factors of soils formation of the NW-facing slopes of Limbara relief are described. The climatic factor is considered to be the most important factor in determining the properties of soils in upslope positions (1300-1100 m). The principal soils are Lithie Haplumbrepts. The morphology and vegetation help the development of the soils between 1100 and 800 m. They are Typic Xerumbrepts. Between 800 and 500 m the principal soils are Lithic Xerorthents. Steepness of the slope controls their development.| File | Dimensione | Formato | |
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