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Ecology, classification and soil pattern of colluvial soils of the bornhoeved lake district (North‐Germany)
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| Zeitschriftentitel: | Zeitschrift für Pflanzenernährung und Bodenkunde |
|---|---|
| Personen und Körperschaften: | , |
| In: | Zeitschrift für Pflanzenernährung und Bodenkunde, 159, 1996, 1, S. 23-29 |
| Format: | E-Article |
| Sprache: | Englisch |
| veröffentlicht: |
Wiley
|
| Schlagwörter: |
| author_facet |
Schleuß, Uwe Blume, Hans‐Peter Schleuß, Uwe Blume, Hans‐Peter |
|---|---|
| author |
Schleuß, Uwe Blume, Hans‐Peter |
| spellingShingle |
Schleuß, Uwe Blume, Hans‐Peter Zeitschrift für Pflanzenernährung und Bodenkunde Ecology, classification and soil pattern of colluvial soils of the bornhoeved lake district (North‐Germany) Soil Science |
| author_sort |
schleuß, uwe |
| spelling |
Schleuß, Uwe Blume, Hans‐Peter 0044-3263 Wiley Soil Science http://dx.doi.org/10.1002/jpln.1996.3581590104 <jats:title>Abstract</jats:title><jats:p>Water erosion causes the accumulation of soil material, especially at the bottom slope and in landscape depressions. According to <jats:italic>FAO</jats:italic>‐<jats:italic>UNESCO</jats:italic> (1990) colluvial soils can be classified as <jats:italic>Cumuli</jats:italic>‐<jats:italic>Aric Anthrosols</jats:italic> if the minimum thickness of the altered topsoil is 5 dm or more. These soils are characterized by addition of small amounts of soil material that has been incorporated into the underlying material by tillage and/or turbation. As a result of geological factors and land‐use intensities, <jats:italic>Cumuli</jats:italic>‐<jats:italic>Aric Anthrosols</jats:italic> differ markedly in their ecological properties. In the study area ‘Bornhoeved Lake District (Schleswig‐Holstein, North‐Germany)’ soil patterns have been investigated showing the interdependence of soil landscapes and their soil units by water erosion and accumulation. Examples of various colluvial soils in catenary sequences in the study area are presented. Colluvial soils in the study area are characterized by a layer thickness between 5 and 14 dm and show significantly higher quantities of organic matter, nitrogen and plant‐available water in comparison with eroded soils.</jats:p> Ecology, classification and soil pattern of colluvial soils of the bornhoeved lake district (North‐Germany) Zeitschrift für Pflanzenernährung und Bodenkunde |
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Zeitschrift für Pflanzenernährung und Bodenkunde |
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| title |
Ecology, classification and soil pattern of colluvial soils of the bornhoeved lake district (North‐Germany) |
| title_unstemmed |
Ecology, classification and soil pattern of colluvial soils of the bornhoeved lake district (North‐Germany) |
| title_full |
Ecology, classification and soil pattern of colluvial soils of the bornhoeved lake district (North‐Germany) |
| title_fullStr |
Ecology, classification and soil pattern of colluvial soils of the bornhoeved lake district (North‐Germany) |
| title_full_unstemmed |
Ecology, classification and soil pattern of colluvial soils of the bornhoeved lake district (North‐Germany) |
| title_short |
Ecology, classification and soil pattern of colluvial soils of the bornhoeved lake district (North‐Germany) |
| title_sort |
ecology, classification and soil pattern of colluvial soils of the bornhoeved lake district (north‐germany) |
| topic |
Soil Science |
| url |
http://dx.doi.org/10.1002/jpln.1996.3581590104 |
| publishDate |
1996 |
| physical |
23-29 |
| description |
<jats:title>Abstract</jats:title><jats:p>Water erosion causes the accumulation of soil material, especially at the bottom slope and in landscape depressions. According to <jats:italic>FAO</jats:italic>‐<jats:italic>UNESCO</jats:italic> (1990) colluvial soils can be classified as <jats:italic>Cumuli</jats:italic>‐<jats:italic>Aric Anthrosols</jats:italic> if the minimum thickness of the altered topsoil is 5 dm or more. These soils are characterized by addition of small amounts of soil material that has been incorporated into the underlying material by tillage and/or turbation. As a result of geological factors and land‐use intensities, <jats:italic>Cumuli</jats:italic>‐<jats:italic>Aric Anthrosols</jats:italic> differ markedly in their ecological properties. In the study area ‘Bornhoeved Lake District (Schleswig‐Holstein, North‐Germany)’ soil patterns have been investigated showing the interdependence of soil landscapes and their soil units by water erosion and accumulation. Examples of various colluvial soils in catenary sequences in the study area are presented. Colluvial soils in the study area are characterized by a layer thickness between 5 and 14 dm and show significantly higher quantities of organic matter, nitrogen and plant‐available water in comparison with eroded soils.</jats:p> |
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| description | <jats:title>Abstract</jats:title><jats:p>Water erosion causes the accumulation of soil material, especially at the bottom slope and in landscape depressions. According to <jats:italic>FAO</jats:italic>‐<jats:italic>UNESCO</jats:italic> (1990) colluvial soils can be classified as <jats:italic>Cumuli</jats:italic>‐<jats:italic>Aric Anthrosols</jats:italic> if the minimum thickness of the altered topsoil is 5 dm or more. These soils are characterized by addition of small amounts of soil material that has been incorporated into the underlying material by tillage and/or turbation. As a result of geological factors and land‐use intensities, <jats:italic>Cumuli</jats:italic>‐<jats:italic>Aric Anthrosols</jats:italic> differ markedly in their ecological properties. In the study area ‘Bornhoeved Lake District (Schleswig‐Holstein, North‐Germany)’ soil patterns have been investigated showing the interdependence of soil landscapes and their soil units by water erosion and accumulation. Examples of various colluvial soils in catenary sequences in the study area are presented. Colluvial soils in the study area are characterized by a layer thickness between 5 and 14 dm and show significantly higher quantities of organic matter, nitrogen and plant‐available water in comparison with eroded soils.</jats:p> |
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| institution | DE-D275, DE-Bn3, DE-Brt1, DE-D161, DE-Gla1, DE-Zi4, DE-15, DE-Pl11, DE-Rs1, DE-105, DE-14, DE-Ch1, DE-L229 |
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| spelling | Schleuß, Uwe Blume, Hans‐Peter 0044-3263 Wiley Soil Science http://dx.doi.org/10.1002/jpln.1996.3581590104 <jats:title>Abstract</jats:title><jats:p>Water erosion causes the accumulation of soil material, especially at the bottom slope and in landscape depressions. According to <jats:italic>FAO</jats:italic>‐<jats:italic>UNESCO</jats:italic> (1990) colluvial soils can be classified as <jats:italic>Cumuli</jats:italic>‐<jats:italic>Aric Anthrosols</jats:italic> if the minimum thickness of the altered topsoil is 5 dm or more. These soils are characterized by addition of small amounts of soil material that has been incorporated into the underlying material by tillage and/or turbation. As a result of geological factors and land‐use intensities, <jats:italic>Cumuli</jats:italic>‐<jats:italic>Aric Anthrosols</jats:italic> differ markedly in their ecological properties. In the study area ‘Bornhoeved Lake District (Schleswig‐Holstein, North‐Germany)’ soil patterns have been investigated showing the interdependence of soil landscapes and their soil units by water erosion and accumulation. Examples of various colluvial soils in catenary sequences in the study area are presented. Colluvial soils in the study area are characterized by a layer thickness between 5 and 14 dm and show significantly higher quantities of organic matter, nitrogen and plant‐available water in comparison with eroded soils.</jats:p> Ecology, classification and soil pattern of colluvial soils of the bornhoeved lake district (North‐Germany) Zeitschrift für Pflanzenernährung und Bodenkunde |
| spellingShingle | Schleuß, Uwe, Blume, Hans‐Peter, Zeitschrift für Pflanzenernährung und Bodenkunde, Ecology, classification and soil pattern of colluvial soils of the bornhoeved lake district (North‐Germany), Soil Science |
| title | Ecology, classification and soil pattern of colluvial soils of the bornhoeved lake district (North‐Germany) |
| title_full | Ecology, classification and soil pattern of colluvial soils of the bornhoeved lake district (North‐Germany) |
| title_fullStr | Ecology, classification and soil pattern of colluvial soils of the bornhoeved lake district (North‐Germany) |
| title_full_unstemmed | Ecology, classification and soil pattern of colluvial soils of the bornhoeved lake district (North‐Germany) |
| title_short | Ecology, classification and soil pattern of colluvial soils of the bornhoeved lake district (North‐Germany) |
| title_sort | ecology, classification and soil pattern of colluvial soils of the bornhoeved lake district (north‐germany) |
| title_unstemmed | Ecology, classification and soil pattern of colluvial soils of the bornhoeved lake district (North‐Germany) |
| topic | Soil Science |
| url | http://dx.doi.org/10.1002/jpln.1996.3581590104 |