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Cold dew and thick grass cover everything.
Grass cover provided both a later winter freezing and delay of spring thawing of soils.
Differences in grass cover existed between low and high density management units, yet no difference in grass cover was evident between low and medium density management units.
Excessive grazing and other practices that destroy the grass cover have also produced soil loss.
The planar collector collected about 90% of the dew at the grass cover while the pyramid collector collected about 1.20% of the grass cover.
The soil groups of the Great Plains are correlated with rainfall and natural grass cover.
Areas with high shrub and grass cover are scarce and important for arid-land ungulates.
Species richness of the pollinators was negatively correlated with grass cover.
Increasing biosolids rates resulted in increased native perennial grass cover in 2005.
Most participants favored grass cover over shrubs or saplings on ROW for aesthetic or utilitarian reasons.
Possible reasons for the decline in surface soil carbon include a decline in grass cover and reduced soil water content.
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CEO of Professional Science Editing for Scientists @ prosciediting.com