Pedological characteristics of soils in the watersheds of Oueds Nekôr and Ghiss (Central Rif; Morocco)

• Main Authors: Ed Dakiri, Soukaina, Faiz, Hatim, Ouldchaib, Jaouad, El Moussaoui, Said, El Talibi, Hajar, Cherkaoui Dekkaki, Hinde, Mourabit, Taoufik, Bouzid, Saida, Damnati, Brahim, Etebaai, Issam
• Format: Conference Proceeding
• Language: English
• Subjects: Alkaline soils; Aridity; Carbonates; Concretions; Gravel; Horizon; Limestone; Lithology; Magnetic permeability; Magnetic susceptibility; Marl; Moisture content; Organic matter; pH effects; Sandstone; Schist; Soil chemistry; Soil erosion; Soil pH; Soil profiles; Soil properties; Vegetation cover; Water content; Watersheds
• ISSN: 2267-1242; 2555-0403; 2267-1242
• DOI: 10.1051/e3sconf/202129804002

The objective of this work is the pedological characterization of soils in the watersheds of Oueds Nekôr and Ghiss. Several profiles were identified and sampled for Physico-chemical and sedimentological analyses (color index, magnetic susceptibility, pH, granulometry, water content, organic matter, and carbonates). The watersheds in question are roughly characterized by a soft and diversified lithology, a sparse vegetation cover, and a semi-arid Mediterranean climate. The soils in the Oued Nekôr watershed are of the silty type (> 50%), not very developed and relatively well-drained, and become well-drained stony in the steep and eroded areas. Soil pH varies between 7 and 8, reflecting low alkaline to alkaline soils. In the Oued Ghiss watershed, the sandstone-limestone or marl-schist soils are poorly differentiated in the steep slopes. The well-drained soils are gravelly, relatively alkaline, and show the beginning of rubefaction. Very locally on wooded flats, the soil profiles can become deep and well-differentiated due to colluvial accumulation. The dark brown eluvial A horizon is relatively rich in organic matter (3.6%). The well individualized illuvial B horizon has strongly rubbed concretions and is richer in organic matter (4.6%). The light beige C horizon corresponds to the strongly altered marl and limestone parent rock with low organic matter content (1.3%) and very low magnetic susceptibility values.