AuthorWrite something about yourself. No need to be fancy, just an overview. ArchivesCategories |
Back to Blog
Atom nuclide new terminal here12/28/2023 Cross section, decay data (.dec) and neutron induced fission yield (.nfy) libraries.If this is not the case, you'll need to replace the sss2 run-commands with the full path to your executable. you either have the executable in your PATH or have created an alias for the executable. This tutorial assumes that you can run Serpent 2 simply by typing sss2 in your terminal, i.e. This tutorial assumes that you have compiled Serpent with OpenMP parallelization and the graphics libraries. 8.2 Unresolved resonance probability table sampling.8.1 Doppler broadening rejection correction.8 Final part: Options for real life calculations.7.10.3 Generating pin power form factors.7.10.2 Generating assembly discontinuity factors.7.9 Post processing the group constant data.7.7 Running the burnup calculation for the historical variations.7.6 Adding important options for group constant generation.7.4 Setting up the historical variations.7 Part 6: Generating a set of group constants for a fuel assembly.6.6 Ideas for additional testing and tinkering in part 5.6.4.8 Plugging the extra holes in the grid plates.6.4.7 Creating 3D models for empty lattice positions. 6.4.6 Setting the fuel pin lattice into the reactor.6.4 Building the Serpent model for the reactor.5.7 Ideas for additional testing and tinkering in part 4.4.6 Ideas for additional testing and tinkering in part 3.4.5 Calculating the pin power distribution.4.4.4 Calculating the k-eff for the modified system.4.4 Testing the power feedback effects in the assembly.4.3 Running the input for the assembly geometry.4 Part 3: A 2D assembly model (infinite lattice).3.7 Ideas for additional testing and tinkering in part 2.3.6 Calculating radial reaction rate distributions in the fuel pellet.3 Part 2: A 2D pin-cell (infinite lattice).2.7 Ideas for additional testing and tinkering in part 1.2.6 Testing the effect of added moderation.2.5 Calculating the flux energy spectrum.2.4 Finding the critical uranium enrichment.2.3 Running the input for the infinite system.The age we propose for Laurentide Ice Sheet retreat from the New Jersey terminal position is broadly consistent with regional and global climate records of the last glacial maximum termination and records of fluvial incision. This cosmogenic nuclide exposure age is consistent with existing limiting radiocarbon ages in the study area and cosmogenic nuclide exposure ages from the terminal moraine on Martha’s Vineyard ~300 km to the northeast. We find that recession of the Laurentide Ice Sheet from the terminal moraine in New Jersey began before 25.2☒.1 ka (10Be, n=16, average, 1 standard deviation). The data set includes field and laboratory replicates, as well as replication of the entire data set five years after initial measurement. Here, we present measurements of in situ produced 10Be and 26Al in 16 quartz-bearing samples collected from bedrock outcrops and glacial erratics just north of the terminal moraine in north-central New Jersey as such, our ages represent a minimum limit on the timing of ice recession from the moraine. The time at which the Laurentide Ice Sheet reached its maximum extent and subsequently retreated from its terminal moraine in New Jersey has been constrained by bracketing radiocarbon ages on preglacial and postglacial sediments.
0 Comments
Read More
Leave a Reply. |