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Soil carbonates are key features in soils of arid and semiarid environment, playing an important role from pedogenetic, landscape history, paleoclimatic and environmental points of view.
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Calcite depletion pedofeatures were the most striking features in these soils.
However, similar features in lunar soils attributed to micrometeorite impact events are typically amorphous because the vapor-deposited material is quenched at low temperatures, preventing the development of crystalline domains.
At the time of relay sowing, excess soil moisture and puddles are common features in puddled soil and such crops face transient soil waterlogging from an early developmental stage.
The physical understanding of these spectral parameters was also sought and the results show a close relationship between the clay mineralogy related bound water and hydroxyl spectral features in the soil spectra and the swelling index.
The burrows of M. terricolor I, II and III showed more or less similar measurements and other features in different soil-types from northern and southern India.
Freeze-back also causes coarse fragments to be heaved and sorted, resulting in oriented features in the soil and a micro-topography of 'patterned', sorted and non-sorted, areas at the surface.
Arctic tundra landscapes are composed of a complex mosaic of patterned ground features, varying in soil moisture, vegetation composition, and surface hydrology over small spatial scales (10 100 m).
Soil hydrology can, in turn, be used to explain soil features (soil morphology), distributions (soil geography) and ecosystem functions (dynamics).
The relationship between number of saturation events and percentage of redoximorphic features showed that some features were forming in soil horizons that saturated only four times within a 10-year period.
The model described here does not preclude possible biological contributions to ooid genesis, nor refute the role of other processes in producing similar features in the same soil.
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CEO of Professional Science Editing for Scientists @ prosciediting.com