Noun:

ಗ್ರೇಯಿಂಗ್,

gleying's Usage Examples:

During soil formation (gleying), the oxygen supply in the soil profile is restricted due to soil moisture.

At great depth, gleying is likely.

sufficient periods of time, such that there is evidence of poor aeration (gleying and mottling); Common in wetlands Udic Soil moisture is sufficiently high.

Aquo (latin: water): poor drainage (mottles and gleying not needed) evident by saturated soils, a high water table or water-adapted.

that are not contiguous to an overlying genetic horizon; and layers with gleying but no other pedogenic changes.

signs of earlier contact with swamp, carbonated chernozem with signs of gleying in loess, solonchak chernozem, carbonated and sporadically salted swampy.

During soil formation (gleying), the oxygen supply in the soil profile is restricted due to soil moisture at saturation.

areas of reddening are due to burning or other natural processes such as gleying (waterlogging).

It is predominantly of a brown forest soil type with some gleying, the lower parts being formed from raised beach sands and gravels derived.