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For depth less than 150 m, SHS temperature in MT decreases rapidly near wellhead, while SHS temperature in AT increases rapidly.
For depth less than 50 m, SHS temperature in IJT decreases rapidly near wellhead, while SHS temperature in annuli increases rapidly.
A linear regression equation of allele frequency of A on depth for depth less than 200 m was PA = 0.806−0.0044D (t = −14.6, P≪0.001) or a 0.44% drop in allele frequency per meter.
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The effect of model depth (Fig. 9c) is substantial for depths less than about 50 m.
However, nearly all data published for the Norwegian continental shelf for depths less than 6 km are based on the evaluation of four-arm caliper data, a method with intrinsic limitations.
A fully-coupled (hydrodynamic and morphologic) numerical model is presented, and utilized for the simulation of tsunami-induced scour around a monopile structure, representative of those commonly utilized as offshore wind turbine foundations at moderate depths i.e. for depths less than 30 m.
For shallow burial depth less than 5 m, the Terzaghi arching model is still applicable to estimate the vertical pressure.
Summary statistics are tabulated by primary production, structure type, manned status and water depth for 3054 decommissioned structures in water depth less than 400 ft from 1990 to 2017.
The impact of higher loads and larger number of passes on compaction was more effective in the soil depth less than 30 cm; for example the normal load of 8.40 kN caused the maximum bulk density of 1.53 Mg/m3 after 16 passes.
All SNPs with maximum read depth less than 100 were kept for subsequent analysis.
For sequenced diploid genomes without known and validated SNPs, it has previously been seen to filter out SNPs with a depth less than half the mean depth of the genome [ 12].
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