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Table 3 Soil texture in the 0 15 cm soil layer across different land use/land cover systems and altitudes Soil property Altitude Land use types Virgin forest Virgin savana Farming Park afforestation Grazing land Eucalyptus forest Texture High (> 1500 m) Silt loam Loam Silt loam – Loam Loam Mid (900 1500 m) Loam Silt loam Loam Loam Silt loam Loam Low (< 900 m) Loam Loam Loam – Silt loam Silt loam.
Soil types include loamy and sandy loam, clay loam, loam, loamy sand, and silt loam.
Textural classes found on the study sites were clay, clay loam, loam, loamy sand, sand, sandy clay loam, and sandy loam.
Additionally, the sites were grouped according to the topsoil soil texture (depth to 0.3 m) into sand, sandy loam, loam, and clay.
One-dimensional water flow was simulated with the HYDRUS code for bare and grassed sandy loam, loam and clay soils at different levels of variability in the saturated hydraulic conductivity Ksat.
Basic soils can be sand, sandy loam, loam, loamy clay, and clay.
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The fine texture of basaltic rocks, on the other hand, yields soils with a loam or clay-loam texture and hinders the development of E horizons.
Because of the preponderance of mountainous and forested areas, the remainder of German soil types range from sand to loam, from loam to clay, and from clay to rocky outcrops.
Open image in new window Fig. 4 a Soil map acquired from global public domain (Case 1) and (b) Local detailed soil map (Case 2) Table 2 Variation of percentage area covered by different soil textures between Case 1 and Case 2 Case 1 (% area) Sandy Clay Loam Loam Total Case 2 (% area) Sandy clay loam 83.32 3.63 86.94 Clay loam 7.88 0 7.88 Clay 4.25 0.93 5.18 Total 95.44 4.56 .
The soil textures were loam and sandy loam.
Nitrogen leaching from loam and sandy loam soils was negligible.
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