Erik Cammeraat
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Ph.D. in Environmental Sciences at the Universiteit van Amsterdam, 1992
Research topic: Hydro-geomorphological processes in a small forested sub-catchment: preferred flow paths of water
During my PhD research I worked on the role of preferred flow paths in
relation to hydrological and geomorphological processes in a small catchment in
Luxembourg under semi-natural forest. A 4 Ha catchment was instrumented following
a nested design, enabling the monitoring of runoff and the spatial and temporal
dynamics of the perched water table for different sub-catchments. 3 years of
intensive monitoring showed that
- Most runoff is generated in small partial areas, which were draining
faster than the surrounding non-partial areas through macro-pores.
- Biological activity in the topsoil, especially moles and earthworms played
an important role in the development preferential flow paths
- Soil hydraulic conductivity showed strong seasonal dynamics, also after
correction for evapotranspiration and interception
- Several fine scale processes (organic matter turnover by biological
activity, swelling and shrinkage of topsoil) resulted in emerging broader
scale patterns and properties (micro topography, perched water spatial
dynamics, soil depth, runoff dynamics)
- Which resulted at the catchment scale in faster hydrological response to
rainfall in forest when compared to nearby catchments under grass on similar
substratum from late summer to early winter, related to the presence of
semi-permanent soil pipes, increasing in importance and connectivity during
summer
M.Sc. in Physical Geography, University of Amsterdam, 1986
with specialization in Glacial Geomorphology and Quaternary Geology.
Research topic: The deglaciation and glacial geomorphology of the
Lechquellengebirge, Voralrberg, Austria
Within the framework of
my Masters studies I investigated:
- The deglaciation history of the Lechquellengebirge in Vorarlberg, Austria using:
geomorphological mapping techniques and material analysis such as gravel
countings, heavy mineral analysis, thin section analysis and grain size distributions of lodgement and ablation tills
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Hydrochemical characteristics of mixed carbonate-gypsum waters in relation to cementation of Holocene and Pre-Würm breccia's,
using
hydrological EC routing techniques, field analysis of pH and alkalinity,
hydrochemical water sample analysis, sediment description and mapping of materials and sedimentary rocks,
thin section analysis
- Consultancy work with Dr. J. Rupke for the the Swiss Cantons of Appenzell and St Gallen on active mass movement areas on the Rhine valley hillslopes
-detailed 1:2000 geomorphological mapping
-mass wasting risk analysis
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