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The contaminant plume is 25 m ⁎ 3000 m ⁎ 2000 m (depth, length, width) in size.
A cold-rig experiment of sDFB (0.8 m width × 0.2 m depth × 3.85 m height) was performed to investigate fluid hydrodynamics and solid circulations.
Eleven vertical profile sections (width: 1.10 m, depth: 0.80 m) were excavated in steps of 0.05 m and sampled.
The optimum parameters for fishpond were 30 m length, 16 m breadth, 1.25 m depth, 1.0 m water depth, 75° lining inclination, and 8 air changes per hour for maximum temperature gain, maximum thermal efficiency and minimum thermal load leveling.
These microcosms were immersed for 6 days at 45 m depth on a 220 m mooring.
Average litter abundance per transect ranges from 1.2 items/10 m in Sant'Agata channel at ~300 m depth, to 13.2 items/10 m in Tremestieri channel 1 at 520 580 m depth (Table 1).
The potential effect of habitat on skeleton properties was investigated by comparing sponges from 0.5 m and 30 m depth.
Stemflow contributions generally resulted in greater soil water recharge below 1 m depth at 0.1 m from the tree bole compared to the 1.5 m distance.
The warm pulse reaches MNORTH in mid-January, when it was observed at 350 m depth above a 100 m thick layer of ISW.
Twelve soil pits (0.70 m long × 0.60 m width × 0.30 m depth) were excavated on a bare Mazic Pellic Vertisol.
Soil water contents were measured weekly throughout two growing seasons, from 0.10 to 2.30 m depth at 0.20-m intervals using a neutron moisture meter.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com