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Increases of primary production and organic matter sedimentation may also influence the recruitment of metals, both natural and anthropogenic, to sediments.
Landfill leachate aeration ponds could treat the water via aeration and particulate matter sedimentation.
Parameters that were measured and compared between the two treatments included chlorophyll-a, particulate organic and inorganic matter, sedimentation, nitrate, ammonia, selected phytoplankton species and oyster growth rates.
In scenario sediments, corresponding to a decrease in the organic content of the sediments, a reduction in the concentrations of total P and phytoplankton is expected in the first two years of simulation, but this effect, would be attenuated throughout the years due to organic matter sedimentation.
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Besides the oxidation of metal components in the stone, the staining can be originated by the reaction of organic matter, trapped during sedimentation and lithification of the rock, and alkalis from the cement [2].
Pronounced increases in sedimentation rate, sediment density, and the influx of terrestrial organic matter, between 8.7 and 7.9 ka suggest early Holocene warmth was interrupted by two distinct pulses of cold summers leading to widespread landscape destabilization and possibly glacier growth.
It is assumed that the organic N in sediment was the most abundant form since sedimentation of organic matter was caused by the sum of accumulated leachated commercial feed and shrimp feces as suggested [ 11, 36].
Organic matter can be recovered by sedimentation with efficiencies higher than 90%, the velocity of sedimentation being 2 · 10−4 s−10−4
It can simulate reaeration, algal respiration and growth, organic matter degradation, mineralization, nitrification, denitrification, sedimentation, and benthic activity.
This was mainly caused by uptake (benthic algae, macrophytes), sorption onto Fe III) hydroxides, and sedimentation of particulate matter in dead zones and on flood plains.
Sedimentation is a matter of grave concern with respect to the Koshi rivers/tributaries which spans a staggering length of 720 km with about 92,538 km2 of drainage area (Nayak 1996).
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