Erik Cammeraat

ORCID: 0000-0003-4398-206X
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About
Contact & Profiles
Research Areas
  • Soil erosion and sediment transport
  • Aeolian processes and effects
  • Soil Carbon and Nitrogen Dynamics
  • Hydrology and Watershed Management Studies
  • Hydrology and Sediment Transport Processes
  • Geology and Paleoclimatology Research
  • Tree Root and Stability Studies
  • Ecology and Vegetation Dynamics Studies
  • Plant Water Relations and Carbon Dynamics
  • Landslides and related hazards
  • Fire effects on ecosystems
  • Land Use and Ecosystem Services
  • Peatlands and Wetlands Ecology
  • Plant Ecology and Soil Science
  • Historical and socio-economic studies of Spain and related regions
  • Soil and Water Nutrient Dynamics
  • Agroforestry and silvopastoral systems
  • Mediterranean and Iberian flora and fauna
  • Forest Ecology and Biodiversity Studies
  • Horticultural and Viticultural Research
  • Rangeland Management and Livestock Ecology
  • Botany and Plant Ecology Studies
  • Climate variability and models
  • Clay minerals and soil interactions
  • Geological and Geophysical Studies Worldwide

University of Amsterdam
2014-2024

Vrije Universiteit Amsterdam
2007-2021

Institute for Biodiversity
2017-2020

Naturalis Biodiversity Center
2011

GGD Amsterdam
1988

Abstract Green water, or plant‐available soil moisture, is a substantial subset of terrestrial fresh water. Land‐use change (LUC) alters green water dynamics through interactions on the micro‐level (i.e., between and vegetation) macro‐level land surface atmosphere). Ongoing global deforestation, growing interest in reforestation projects, begs question whether such large‐scale LUCs have major eco‐hydrological impacts via process moisture recycling. This requires systematic, mechanistic...

10.1029/2020wr029234 article EN cc-by-nc Water Resources Research 2021-06-25

Abstract Agricultural land abandonment is currently widely spread in Mediterranean countries and a further increase expected. Previous research has shown that abandoned fields semi‐arid areas are more vulnerable to gully erosion. The absence of ploughing slow vegetation recovery cause the formation soil crusts with low infiltration rates, resulting increased runoff erosion risk. objective our study was assess extent causes terrace failure on discuss options for mitigation. carried out...

10.1002/esp.1676 article EN Earth Surface Processes and Landforms 2008-05-13

Abstract Runoff connectivity depends on topography, rainfall, man‐made elements (terraces, trails, roads and drainage systems) vegetation. In this study, we quantified the effects of 70 years human activities runoff in mountainous Araguás afforested sub‐catchment (17·2 ha; Central Spanish Pyrenees). The IC index hydrological was chosen to perform metric over six land use scenarios at high spatial resolution (1 × 1 m cell size). current scenario (year 2012) simulated with three flow...

10.1002/ldr.2531 article EN Land Degradation and Development 2016-04-15

Mediterranean mountains are sensitive agroecosystems that have suffered intense land use and cover changes (LULCC) during the last century. From middle of twentieth century, most cultivated lands in were abandoned, allowing recovery vegetation (through natural revegetation afforestation programmes). To examine effects farmland abandonment, secondary succession (natural revegetation) afforestation, an intensive soil sampling was carried out Araguás catchment (Central Spanish Pyrenees)...

10.1016/j.catena.2023.107062 article EN cc-by-nc-nd CATENA 2023-03-17

Abstract Soil dwelling ants are important soil engineers that have a large impact on the ecosystem. This is reflected in alteration of properties by due to burrowing activities, accumulation organic matter and other nutrients soil, which, turn, alters physical, chemical (micro) biological processes. A review recent literature these fine scale changes resulting from ant activity presented this paper. However, do not only affect at but also effects hillslope catchment scales with respect...

10.1111/j.1439-0418.2008.01281.x article EN Journal of Applied Entomology 2008-04-09

Soil erosion phenomena occur at a range of time and space scales, from the plot in which individual measurements are made, via field scale concerns farmer, up to national or regional scales where they can influence major planning decisions. A number approaches problems up-scaling have been developed context climate soil erosion, within projects EU Environment Programme (MEDALUS, EFEDA, ERMES). Some these relate dominant dynamic interactions create patterns different spatial ways interact....

10.1080/00224561.1996.12457097 article EN Journal of Soil and Water Conservation 1996-09-01

A better process understanding of how water erosion influences the redistribution soil organic carbon (SOC) is sorely needed to unravel role for (C) budget from local global scales. The main objective this study was determine SOC and complete C a loess affected by erosion. We measured fluxes SOC, dissolved (DOC) CO2 in pseudo-replicated rainfall-simulation experiment. characterized different fractions soils redistributed sediments using density fractionation determined enrichment ratios...

10.1371/journal.pone.0096299 article EN cc-by PLoS ONE 2014-05-06
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