Lineare Erosion in Niedersachsen - Ergebnisse einer elfjährigen Messreihe zu Ausmaß, kleinräumiger Verbreitung und Ursachen des Bodenabtrags

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Translated title of the contributionRill erosion in Lower Saxony - Results of an 11-year survey on the expansion, small-scale distribution and cause of soil erosion
Original languageGerman
Pages (from-to)63-75
Number of pages13
JournalBodenkultur
Volume63
Issue number2-3
Publication statusPublished - 5 Sept 2012

Abstract

Since 2000, for more than 11 years, the project "Long-term monitoring of erosion in Lower Saxony" has measured linear erosion. The rate of soil erosion, spatial distribution and the specific factors of linear erosion were documented. Rill erosion shows high spatial and temporal variability. One of the most important causes for temporal variability is the interaction between crops, soil cover and precipitation. The rate of linear soil erosion is higher in winter than in summer. A locally differentiated analysis shows that spatial variability within plots is mostly due to slope form and steepness and direction of tillage. This article presents the results of the 11-year study in detail and describes the implications for modeling and practice.

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Lineare Erosion in Niedersachsen - Ergebnisse einer elfjährigen Messreihe zu Ausmaß, kleinräumiger Verbreitung und Ursachen des Bodenabtrags. / Bug, J.; Mosimann, T.
In: Bodenkultur, Vol. 63, No. 2-3, 05.09.2012, p. 63-75.

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title = "Lineare Erosion in Niedersachsen - Ergebnisse einer elfj{\"a}hrigen Messreihe zu Ausma{\ss}, kleinr{\"a}umiger Verbreitung und Ursachen des Bodenabtrags",
abstract = "Since 2000, for more than 11 years, the project {"}Long-term monitoring of erosion in Lower Saxony{"} has measured linear erosion. The rate of soil erosion, spatial distribution and the specific factors of linear erosion were documented. Rill erosion shows high spatial and temporal variability. One of the most important causes for temporal variability is the interaction between crops, soil cover and precipitation. The rate of linear soil erosion is higher in winter than in summer. A locally differentiated analysis shows that spatial variability within plots is mostly due to slope form and steepness and direction of tillage. This article presents the results of the 11-year study in detail and describes the implications for modeling and practice.",
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TY - JOUR

T1 - Lineare Erosion in Niedersachsen - Ergebnisse einer elfjährigen Messreihe zu Ausmaß, kleinräumiger Verbreitung und Ursachen des Bodenabtrags

AU - Bug, J.

AU - Mosimann, T.

PY - 2012/9/5

Y1 - 2012/9/5

N2 - Since 2000, for more than 11 years, the project "Long-term monitoring of erosion in Lower Saxony" has measured linear erosion. The rate of soil erosion, spatial distribution and the specific factors of linear erosion were documented. Rill erosion shows high spatial and temporal variability. One of the most important causes for temporal variability is the interaction between crops, soil cover and precipitation. The rate of linear soil erosion is higher in winter than in summer. A locally differentiated analysis shows that spatial variability within plots is mostly due to slope form and steepness and direction of tillage. This article presents the results of the 11-year study in detail and describes the implications for modeling and practice.

AB - Since 2000, for more than 11 years, the project "Long-term monitoring of erosion in Lower Saxony" has measured linear erosion. The rate of soil erosion, spatial distribution and the specific factors of linear erosion were documented. Rill erosion shows high spatial and temporal variability. One of the most important causes for temporal variability is the interaction between crops, soil cover and precipitation. The rate of linear soil erosion is higher in winter than in summer. A locally differentiated analysis shows that spatial variability within plots is mostly due to slope form and steepness and direction of tillage. This article presents the results of the 11-year study in detail and describes the implications for modeling and practice.

KW - Erosion damage mapping

KW - Long-term monitoring

KW - Rill erosion

KW - Soil erosion

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M3 - Artikel

AN - SCOPUS:84873843975

VL - 63

SP - 63

EP - 75

JO - Bodenkultur

JF - Bodenkultur

SN - 0006-5471

IS - 2-3

ER -