Miriam Marzen

Ms. Miriam Marzen

Trier University, Department of Physical Geography, Trier, Germany

Research Focus & Metrics

Academic Career Length

14Years (2013-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 November 2013 in CATENA
Verified
Journal Article
Closed access
TIT. Iserloh
T. Iserloh
JRJ.B. Ries
J.B. Ries
JAJ. Arnáez
J. Arnáez
CBC. Boix-Fayos
C. Boix-Fayos
VBV. Butzen
V. Butzen
SWS. Wirtz
S. Wirtz

1 September 2016 in Science of The Total Environment
Verified
Journal Article
Closed access
Jesús Rodrigo-CominoJesús Rodrigo-Comino
Jesús Rodrigo-Comino
TIT. Iserloh
T. Iserloh
TLT. Lassu
T. Lassu
ACA. Cerdà
A. Cerdà
SKS.D. Keestra
S.D. Keestra
JRJ.B. Ries
J.B. Ries

1 July 2017 in Science of The Total Environment
Verified
Journal Article
Closed access
MMMiriam Marzen
Miriam Marzen
TIThomas Iserloh
Thomas Iserloh
Isabel De LimaIsabel De Lima
Isabel De Lima
WFWolfgang Fister
Wolfgang Fister
JRJohannes B. Ries
Johannes B. Ries

1 April 2015 in CATENA
Verified
Journal Article
Closed access
MMMiriam Marzen
Miriam Marzen
TIThomas Iserloh
Thomas Iserloh
Markus C. CasperMarkus C. Casper
Markus C. Casper
JRJohannes B. Ries
Johannes B. Ries

14 November 2019 in Geosciences
Verified
Journal Article
Open access
PDF file
MMMiriam Marzen
Miriam Marzen
TIThomas Iserloh
Thomas Iserloh
WFWolfgang Fister
Wolfgang Fister
Karl Manuel, SeegerKarl Manuel, Seeger
Karl Manuel, Seeger
Jesús Rodrigo-CominoJesús Rodrigo-Comino
Jesús Rodrigo-Comino
JRJohannes B. Ries
Johannes B. Ries
The relative impact of water and wind on total erosion was investigated by means of an experimental-empirical study. Wind erosion and water erosion were measured at five different sites: (1) Mediterranean fallow, (2) Mediterranean orchard, (3) wheat field, (4) vineyard and (5) sand substrate. Mean erosion rates ranged from 1.55 to 618 g·m−2·h−1 for wind and from 0.09 to 133.90 g·m−2·h−1 for rain eroded material over all tested sites. Percentages (%) of eroded sediment for wind and rain, respectively, were found to be 2:98 on Mediterranean fallow, 11:89 on Mediterranean orchard, 3:97 on wheat field, 98:2 on vineyard and 99:1 on sand substrate. For the special case of soil surface crust destroyed by goat trampling, the measured values emphasize a strong potential impact of herding on total soil erosion. All sites produced erosion by wind and rain, and relations show that both erosive forces may have an impact on total soil erosion depending on site characteristics. The results indicate a strong need to focus on both wind and water erosion particularly concerning soils and substrates in vulnerable environments. Measured rates show a general potential erosion depending on recent developments of land use and climate change and may raise awareness of scientist, farmers and decision makers about potential impact of both erosive forces. Knowledge about exact relationship is key for an adapted land use management, which has great potential to mitigate degradation processes related to climate change.

1 October 2016 in CATENA
Verified
Journal Article
Closed access
MMMiriam Marzen
Miriam Marzen
TIThomas Iserloh
Thomas Iserloh
JLJoão L.M.P. de Lima
João L.M.P. de Lima
JRJohannes B. Ries
Johannes B. Ries