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author Prange, Werner
Brümmer, Gerhard
Weber, Ernst
author_facet Prange, Werner
Brümmer, Gerhard
Weber, Ernst
collection Datos científicos de ciencias marinas y ambientales
contents Results from a large scale soil mapping on the North Frisian mainland indicate, that field characteristics, particularly the grain-size, bedding, and degree of compaction, with in general determine the soil units mapped, are closely correlated with each other and with other field and laboratory data. Exchangable ions and the Ca/Mg-ratio, however, indicate no explainable connections with the soil units and with most of the other field characteristics but are determined postsedimentarily by processes of the development of soil and landscape, such as desalting and decalcification, silicate weathering, fresh- and salt-water innundations, salty precipitations, salty groundwater and fertilization. Therefore the Ca/Mg-ratio is not suitable to differentiate between more clayey compacted Knick-marsh soils and less clayey permeable Klei-marsh soils. The results confirm that marsh-soils may only be classified and mapped by means of all available field-data which have to be supplemented by laboratory investigations.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_783344
institution PANGAEA
language en
publishDate 1974
publisher PANGAEA
record_format pangaea
spellingShingle (Tables 2-7) Soil characteristics and geochemistry of marshland in the North Frisian mainland, Schleswig-Holstein, Germany
Prange, Werner
Brümmer, Gerhard
Weber, Ernst
Base saturation; Bedding/banding; Calcium; Calcium/Magnesium ratio; Calcium/Potassium ratio; Calcium/Sodium ratio; Calcium carbonate; Depth, relative; DEPTH, sediment/rock; Description; Elevation 2; Fine particle percentage; Height above sea level; Land use; Layer description; Layer thickness; Magnesium; Magnesium/Potassium ratio; Magnesium/Sodium ratio; North_Frisia1974; Parameter; pH; Phosphorus pentoxide; Potassium; Potassium oxide; Sample amount; Sample code/label; Sample type; Schleswig-Holstein, Germany; Size fraction < 0.002 mm, clay; Size fraction > 0.060 mm; Size fraction 0.006-0.002 mm; Size fraction 0.020-0.006 mm; Sodium; Sodium/Potassium ratio; Substrate type; Sulfur, organic
Results from a large scale soil mapping on the North Frisian mainland indicate, that field characteristics, particularly the grain-size, bedding, and degree of compaction, with in general determine the soil units mapped, are closely correlated with each other and with other field and laboratory data. Exchangable ions and the Ca/Mg-ratio, however, indicate no explainable connections with the soil units and with most of the other field characteristics but are determined postsedimentarily by processes of the development of soil and landscape, such as desalting and decalcification, silicate weathering, fresh- and salt-water innundations, salty precipitations, salty groundwater and fertilization. Therefore the Ca/Mg-ratio is not suitable to differentiate between more clayey compacted Knick-marsh soils and less clayey permeable Klei-marsh soils. The results confirm that marsh-soils may only be classified and mapped by means of all available field-data which have to be supplemented by laboratory investigations.
title (Tables 2-7) Soil characteristics and geochemistry of marshland in the North Frisian mainland, Schleswig-Holstein, Germany
topic Base saturation; Bedding/banding; Calcium; Calcium/Magnesium ratio; Calcium/Potassium ratio; Calcium/Sodium ratio; Calcium carbonate; Depth, relative; DEPTH, sediment/rock; Description; Elevation 2; Fine particle percentage; Height above sea level; Land use; Layer description; Layer thickness; Magnesium; Magnesium/Potassium ratio; Magnesium/Sodium ratio; North_Frisia1974; Parameter; pH; Phosphorus pentoxide; Potassium; Potassium oxide; Sample amount; Sample code/label; Sample type; Schleswig-Holstein, Germany; Size fraction < 0.002 mm, clay; Size fraction > 0.060 mm; Size fraction 0.006-0.002 mm; Size fraction 0.020-0.006 mm; Sodium; Sodium/Potassium ratio; Substrate type; Sulfur, organic
url https://doi.org/10.1594/PANGAEA.783344