The Soils of Nepal - Soil Properties

AuthorShree Prasad Vista
AuthorKrishna Bahadur Karki
AuthorYam Kanta Gaihre
AuthorSonisa Sharma
AuthorBandhu Raj Baral
Jurisdiction:Nepal
Date of acession2023-05-03T13:35:35Z
Date of availability2023-05-03T13:35:35Z
Date of issue2021
AbstractNepalese soils are developed dominantly from micaceous parent materials such as phyllites, schists, gneisses, and granites; thus, most of the soil contains a higher proportion of mica. Nepalese soils are mostly friable in hills and mountains because of the continuous use of organic inputs such as farmyard manure and compost, while soils are hard and compacted in the Terai region because of the continuous use of machinery and less use of organic inputs. Soils in hills exhibit higher soil plasticity but the intensity of soil plasticity decreases in lower belts where erosion deposits prevail and most of the soils are sandy in nature. The soils of Nepal also show wide variability in chemical properties, and thereby respond differently to the same crop across ecological zones and soil types. In general, the soils of Nepal are acidic in nature. About 53% of soils are in the acidic range, while 33% are neutral, and 13% are in the alkaline range. In general, soils in hills and mountains are richer in major plant nutrients and organic matter than soils in the Terai region. However, the content of micronutrients such as zinc, boron, and molybdenum are low. Overall, soil nutrients are being mined throughout the nation, with the fastest decline in eastern areas and in the Terai region. Soil erosion, imbalanced use of fertilizers, low or no use of organic inputs, and adoption of intensive cropping systems are some of the major causes for the decline in soil nutrients.
URLhttps://hub.ifdc.org/handle/20.500.14297/2122
Languageen_US
SubjectSoil fertility
SubjectOrganic matter
SubjectBiofertilizers
SubjectSoil acidity
TitleThe Soils of Nepal - Soil Properties
TypeBook chapter
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