Das Ca/Mg—Verhältnis in den Marschböden, eine Folge postsedimentärer Faktoren

Werner Prange
The Ca/Mg-ratio, together with other data drawn in typical maps of a large scale soil mapping on the North Frisian mainland, are compared with each other. The Ca/Mg-ratio indicate no relations with the conditions under sedimentation and therefore no explainable connections with the soil units and most of the other field characteristics. On contrary there is a clear dependence from post-sedimentary factors, which everywhere add in an other kind and determine the Ca/Mg-ratio. Therefore it...