@article{gledocs_11858_7251,
author = {Schweikle, Volker},
title = {Grundlagen zur Wasserbewegung nach Darcy in Moor und Torf},
year = {2017},
volume = {47},
pages = {129-138},

abstract = {Abstract: The legal (Germany) unit of k in the law of Darcy is m3 · s · kg-1 ·10-4 and equal for all physical derivations. k depends distinctly on temperature. The permeable pore volume of peat is probably < 0,1 % of the total pore volume due to a high density of electrical charge and explains the very low water conductivity of the katotelm. It is possible to convert the viscosity η in a value of internal friction µi. The structure of the law of Darcy limits the mathematical possibility to shift elements from one term to another. The use of rules of calculation for a normal distribution in statistics fails for transformed crooked distributions and give no plausible results.},
note = { \url {http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/7251}},
}