@article{gledocs_11858_7353,
author = {Chmieleski, Jana and Zeitz, Jutta},
title = {Bodenbildung in entwässerten Mudden},
year = {2006},
volume = {36},
pages = {39-52},

abstract = {Abstract: The formation of soils from gyttja takes place under aeration, due to artificial drainage. In northern Europe gyttja deposits are found in northern Germany, Poland, Finland and Sweden. Their investigations date back to the middle of the last century. Their cultivation led to a pedogenesis, which is reflected by chemical and physical properties. Subhydric material is rich in organic matter and often in CaCO3 ranging from 5 to 95 %. It is fine-grained with a high pore space, particularly of the meso- and micro-pores. As a result of pedogenesis the volume of micropores increases while the volume of meso-pores decreases.},
note = { \url {http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/7353}},
}