mollisol|mollisols in English

noun

mineral-rich surface layer soil

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Below are sample sentences containing the word "mollisol|mollisols" from the English Dictionary. We can refer to these sentence patterns for sentences in case of finding sample sentences with the word "mollisol|mollisols", or refer to the context using the word "mollisol|mollisols" in the English Dictionary.

1. Aridisols Entisols Gelisols Histosols Inceptisols Mollisols Oxisols Spodosols Ultisols Vertisols Contact

2. Mollisol, Aridisol, entisol and inceptisol, alfisol, ultisol, andisol, oxisol, spodosol, gelisol, histosol, and vertisol

3. Question 22 Options: Mollisol Oxisol Ultisol Alfisol Question 23 Match The Soil Order To Its Definition

4. Question 23 Options: 123456 Inceptisol 123456 Andisol 123456 Alfisol 123456 Mollisol 123456 Histosol 123456 Aridisol 1

5. Currently there are 12 soil orders in the USDA classification system: Alfisols, Andisols, Aridisols, Entisols, Gelisols, Histosols, Inceptisols, Mollisols, Oxisols, Spodosols, Ultisols, and Vertisols.

6. As nouns the difference between mollisol and Alfisol is that mollisol is (us soil taxonomy) a type of soil that forms in semiarid to semihumid areas, typically under a grassland cover, with deep, high organic matter and a nutrient-enriched surface soil (or horizon) while Alfisol is an abundant soil order in the usda soil taxonomy, with a clay-enriched subsoil and relatively high native

7. The major soil groups in South America according to the US soil taxonomy classification system are Oxisols, Ultisols, Alfisols, Mollisols, Entisols, Inceptisols, Vertisols, Aridisols, Andisols, Histosols, Gelisols, and Spodosols (Sanchez and Logan, 1992).

8. Soil orders are frequently defined by a single dominant characteristic affecting soils in that location, e.g., the prevalent vegetation (Alfisols, Mollisols), the type of parent material (Andisols, Vertisols), or the climate variables such as lack of precipitation (Aridisols) or the presence of permafrost (Gelisols).

9. ‘The series consists of very deep, well drained, fine silty Alfisol formed in loess.’ ‘In order to study the origins of Alfisols and mollisols, Mella examined the mineralogical and chemical properties of the soils, as well as those of the insoluble residue of the coral rocks.’

10. It occurs worldwide, in Aridisol and mollisol soil orders—generally in arid or semiarid regions, including in central and western Australia, in the Kalahari Desert, in the High Plains of the western USA, in the Sonoran Desert and Mojave Desert, and in Eastern Saudi Arabia at Al-Hasa