Details
| Original language | English |
|---|---|
| Pages (from-to) | 299-309 |
| Number of pages | 11 |
| Journal | CATENA |
| Volume | 165 |
| Early online date | 20 Feb 2018 |
| Publication status | Published - Jun 2018 |
Abstract
Soil erosion caused by water has been monitored for 17 years on 465 ha cropland in Lower Saxony (Northern Germany). The 86 monitored fields are representative for three different typical agricultural landscapes with an intermediate to high water erosion risk in Northern Germany. The monitoring scheme included regularly conducted erosion damage mapping and cultivation surveys. The collected data encompasses 1275 field years and 1355 mapped erosion systems, giving evidence on the extent, frequency and rate of soil erosion by water. Mean mapped soil loss for all fields was relatively small at 0.85 t ha −1 a −1. The highest rate for a single field amounted to 7.02 t ha −1 a −1. Variability of soil loss in time and space was high: annual losses (mean of all fields) ranged between 0.04 and 2.81 t ha −1 a −1. The highest annual loss on a single field was 53.07 t ha −1. Every year, at least 24% of the monitored fields were not affected by erosion, only 1.3% of the monitored area eroded at least once a year. Spatial analysis of mapped erosion features shows that the highest soil loss is located in topographically-defined flow paths and in wheel tracks oriented in line of the steepest slope. Cultivated crops and tillage management have a high influence on loss rates ranging from 0.07 for catch crop to 2.78 t ha −1 a −1 for potato. Additionally, the results prove that farmers in the investigation areas were able to significantly reduce soil loss rates of the five most important crops from 0.6 to 0.37 t ha −1 a −1 by using conservation tillage measures. The annual variability in the collected data emphasises the importance of appropriate long-term monitoring programmes to create sound data on the extent, frequency and rate of soil erosion by water at a field to landscape scale.
Keywords
- Monitoring, Rill erosion, Sheet erosion, Soil erosion, Tillage, Water erosion
ASJC Scopus subject areas
- Earth and Planetary Sciences(all)
- Earth-Surface Processes
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In: CATENA, Vol. 165, 06.2018, p. 299-309.
Research output: Contribution to journal › Article › Research › peer review
}
TY - JOUR
T1 - Soil erosion by water in Northern Germany: long-term monitoring results from Lower Saxony
AU - Steinhoff-Knopp, Bastian
AU - Burkhard, Benjamin
N1 - Publisher Copyright: © 2018 Elsevier B.V. Copyright: Copyright 2018 Elsevier B.V., All rights reserved.
PY - 2018/6
Y1 - 2018/6
N2 - Soil erosion caused by water has been monitored for 17 years on 465 ha cropland in Lower Saxony (Northern Germany). The 86 monitored fields are representative for three different typical agricultural landscapes with an intermediate to high water erosion risk in Northern Germany. The monitoring scheme included regularly conducted erosion damage mapping and cultivation surveys. The collected data encompasses 1275 field years and 1355 mapped erosion systems, giving evidence on the extent, frequency and rate of soil erosion by water. Mean mapped soil loss for all fields was relatively small at 0.85 t ha −1 a −1. The highest rate for a single field amounted to 7.02 t ha −1 a −1. Variability of soil loss in time and space was high: annual losses (mean of all fields) ranged between 0.04 and 2.81 t ha −1 a −1. The highest annual loss on a single field was 53.07 t ha −1. Every year, at least 24% of the monitored fields were not affected by erosion, only 1.3% of the monitored area eroded at least once a year. Spatial analysis of mapped erosion features shows that the highest soil loss is located in topographically-defined flow paths and in wheel tracks oriented in line of the steepest slope. Cultivated crops and tillage management have a high influence on loss rates ranging from 0.07 for catch crop to 2.78 t ha −1 a −1 for potato. Additionally, the results prove that farmers in the investigation areas were able to significantly reduce soil loss rates of the five most important crops from 0.6 to 0.37 t ha −1 a −1 by using conservation tillage measures. The annual variability in the collected data emphasises the importance of appropriate long-term monitoring programmes to create sound data on the extent, frequency and rate of soil erosion by water at a field to landscape scale.
AB - Soil erosion caused by water has been monitored for 17 years on 465 ha cropland in Lower Saxony (Northern Germany). The 86 monitored fields are representative for three different typical agricultural landscapes with an intermediate to high water erosion risk in Northern Germany. The monitoring scheme included regularly conducted erosion damage mapping and cultivation surveys. The collected data encompasses 1275 field years and 1355 mapped erosion systems, giving evidence on the extent, frequency and rate of soil erosion by water. Mean mapped soil loss for all fields was relatively small at 0.85 t ha −1 a −1. The highest rate for a single field amounted to 7.02 t ha −1 a −1. Variability of soil loss in time and space was high: annual losses (mean of all fields) ranged between 0.04 and 2.81 t ha −1 a −1. The highest annual loss on a single field was 53.07 t ha −1. Every year, at least 24% of the monitored fields were not affected by erosion, only 1.3% of the monitored area eroded at least once a year. Spatial analysis of mapped erosion features shows that the highest soil loss is located in topographically-defined flow paths and in wheel tracks oriented in line of the steepest slope. Cultivated crops and tillage management have a high influence on loss rates ranging from 0.07 for catch crop to 2.78 t ha −1 a −1 for potato. Additionally, the results prove that farmers in the investigation areas were able to significantly reduce soil loss rates of the five most important crops from 0.6 to 0.37 t ha −1 a −1 by using conservation tillage measures. The annual variability in the collected data emphasises the importance of appropriate long-term monitoring programmes to create sound data on the extent, frequency and rate of soil erosion by water at a field to landscape scale.
KW - Monitoring
KW - Rill erosion
KW - Sheet erosion
KW - Soil erosion
KW - Tillage
KW - Water erosion
UR - http://www.scopus.com/inward/record.url?scp=85042181855&partnerID=8YFLogxK
U2 - 10.1016/j.catena.2018.02.017
DO - 10.1016/j.catena.2018.02.017
M3 - Article
VL - 165
SP - 299
EP - 309
JO - CATENA
JF - CATENA
SN - 0341-8162
ER -