The Authors describes principal soils of the SE-facing slopes of Limbara relief. Lithic Haplumbrepts are the principal soils above 1100 m, Lithic and Tipic Xerochrepts are widely distributed between 1100 and 700 m and Lithic Xerorthents are the principal soil from 700 to 450 m. In this work differences with the soil of NW-facing slopes are described. In the SE-facing slopes the transition to Xerochrepts isn't gradual, cambie horizon is uncommon and the soils between 800 and 500 m have an higher content of clay and higher saturation.
I Suoli su substrati acidi in Sardegna: nota 3: alcune osservazioni sui suoli del versante sud-est del Massiccio del Limbara / Passino, Anna Maria. - In: STUDI SASSARESI. SEZIONE 3: ANNALI DELLA FACOLTÀ DI AGRARIA DELL'UNIVERSITÀ DI SASSARI. - ISSN 0562-2662. - 29:(1982), pp. 367-391.
I Suoli su substrati acidi in Sardegna: nota 3: alcune osservazioni sui suoli del versante sud-est del Massiccio del Limbara
1982-01-01
Abstract
The Authors describes principal soils of the SE-facing slopes of Limbara relief. Lithic Haplumbrepts are the principal soils above 1100 m, Lithic and Tipic Xerochrepts are widely distributed between 1100 and 700 m and Lithic Xerorthents are the principal soil from 700 to 450 m. In this work differences with the soil of NW-facing slopes are described. In the SE-facing slopes the transition to Xerochrepts isn't gradual, cambie horizon is uncommon and the soils between 800 and 500 m have an higher content of clay and higher saturation.| File | Dimensione | Formato | |
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