GENUS
发表于 2025-3-23 11:00:16
A Critique on Degradation of HT and SAT Soils in View of Their Pedology and Mineralogy,y two extreme climatic conditions i.e. semi-arid (SAT) and humid tropical (HT) climates. Past research reports indicated that the red ferruginous (RF) of both HT and SAT climates are physically and chemically degraded to a considerable extent. However, newly acquired research data on the rate of top
Phonophobia
发表于 2025-3-23 16:11:04
Anomalous Potassium Release and Adsorption Reactions: Evidence of Polygenesis of Tropical Indian Sohumid to semi-arid in the geological past. Dominant low charge di-octahedral smectite in shrink-swell soils (Vertisols and Vertic intergrades) formed at the expense of plagioclase feldspar in previous humid tropical (HT) climate is being preserved in the present day semi-arid (SA) climate, which fav
Estimable
发表于 2025-3-23 21:04:31
Concluding Remarks,ficult to manage tropical soils to sustain their productivity because comprehensive knowledge on their formation remained elusive for a long time. Soil care has become a national agenda in the Indian context to meet the food demand for ever increasing human population. This task demands the basic pe
intellect
发表于 2025-3-23 23:51:02
Unique Depth Distribution of Clays in SAT Alfisols: Evidence of Landscape Modifications,long with the geomorphic and climatic history of such Alfisols indicate that these Alfisols are developed on the old rock system of the earth and represent relict paleosols. The unique depth distribution of clays bears the testimony of the landscape modification affected through the truncation of Alfisols developed in the preceding humid climate.
慷慨援助
发表于 2025-3-24 06:13:23
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absorbed
发表于 2025-3-24 09:22:16
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名次后缀
发表于 2025-3-24 12:09:42
Simple Methods to Study Pedology and Edaphology of Indian Tropical Soils
jagged
发表于 2025-3-24 14:53:13
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充气女
发表于 2025-3-24 20:38:25
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Prophylaxis
发表于 2025-3-25 00:21:16
Evidence of Clay Illuviation in Soils of the Indo-Gangetic Alluvial Plains (IGP) and Red Ferruginou) and some of them considered the clay enrichment due to the sedimentation processes, geogenic origins and in situ weathering of biotite particles..Loamy to clayey Mollisols, Alfisols and Ultisols of HT climate, which are in general mild to strongly acidic, have clay enriched B horizons and maintain