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Muck and peat soils are found within the coastal marshes, while the bottoms hold rich alluvial soils: the lighter and coarser bottom soils of the Mississippi and Red River valleys and the older alluvium and loessial, or windblown, soils.
This study was designed to assess the common carp (Cyprinus carpio L) potential to improve conditions in pond bottom soils.
In the predominantly agrarian medieval period, this combination of access to fertile, if flood-prone, valley bottom soils and drier (but heavier and more clay-rich) hillside/ hilltop soils seems to have been good for a mixed agricultural base.
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Moreover, attention to bottom soil condition increases in importance as culture intensity increases.
After saturation from the bottom, soil samples were drained for 24 h to release the gravitational water.
Bioturbation activity generated by fish has the potential to improve bottom soil quality by increasing oxygen supply to a greater depth in aquaculture ponds bottoms.
Five different biogenic materials (windrow compost-WC; vermicompost-VC; landfill top cover-LTC; landfill bottom soil-LBS; and river soil sediment-SS) were screened.
In this setting, the heavier isotopes enrich the bottom soil horizons, which become progressively more available to the roots over the course of the season.
The top and bottom soil layers possessed distinct communities from the original inoculum, but their structure dynamics were different from each other.
This study suggested a methodology and device system to supply water from the bottom soil layer at the different locations of slopes.
As a result of the decrease in soil support at the sidewalls of the foundation by stiffness degradation due to hysteresis, the stress caused by the structural weight on the bottom soil is increased during earthquakes.
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