| human | Q5 |
| P1960 | Google Scholar author ID | ktkTbgsAAAAJ |
| P496 | ORCID iD | 0000-0001-5779-0304 |
| P1153 | Scopus author ID | 6701789833 |
| P108 | employer | Wageningen University & Research | Q422208 |
| P735 | given name | Juul | Q20080602 |
| Juul | Q20080602 | ||
| P6104 | maintained by WikiProject | WikiProject Invasion Biology | Q56241615 |
| P106 | occupation | researcher | Q1650915 |
| P21 | sex or gender | female | Q6581072 |
| Q42136028 | A modification of the constant-head permeameter to measure saturated hydraulic conductivity of highly permeable media |
| Q108666255 | Arctic greening, Arctic browning or Arctic drowning? |
| Q35539981 | Atmospheric nitrogen deposition promotes carbon loss from peat bogs. |
| Q57203678 | Background invertebrate herbivory on dwarf birch (Betula glandulosa-nana complex) increases with temperature and precipitation across the tundra biome |
| Q114102222 | Can ash from smoldering fires increase peatland soil pH? |
| Q30790811 | Can frequent precipitation moderate the impact of drought on peatmoss carbon uptake in northern peatlands? |
| Q114197488 | Carbon to nitrogen ratio and quantity of organic amendment interactively affect crop growth and soil mineral N retention |
| Q60567209 | Cell-wall polysaccharides play an important role in decay resistance of Sphagnum and actively depressed decomposition in vitro |
| Q113798982 | Circum‐Arctic distribution of chemical anti‐herbivore compounds suggests biome‐wide trade‐off in defence strategies in Arctic shrubs |
| Q39768180 | Climatic modifiers of the response to nitrogen deposition in peat-forming Sphagnum mosses: a meta-analysis. |
| Q111367670 | Dead wood diversity promotes fungal diversity |
| Q60567211 | Decreased summer water table depth affects peatland vegetation |
| Q112795777 | Determinants of tree seedling establishment in alpine tundra |
| Q60394921 | Dissolved organic nitrogen dominates in European bogs under increasing atmospheric N deposition |
| Q60567208 | Do plant traits explain tree seedling survival in bogs? |
| Q41696096 | Does salt stress constrain spatial distribution of dune building grasses Ammophila arenaria and Elytrichia juncea on the beach? |
| Q37826839 | Ecosystem responses to reduced and oxidised nitrogen inputs in European terrestrial habitats. |
| Q60567216 | Effects of water level and temperature on performance of four Sphagnum mosses |
| Q58643210 | Environmental and taxonomic controls of carbon and oxygen stable isotope composition in Sphagnum across broad climatic and geographic ranges |
| Q58649263 | Environmental and taxonomic controls of carbon and oxygen stable isotope composition in Sphagnum across broad climatic and geographic ranges |
| Q107925264 | Environmental drivers of Sphagnum growth in peatlands across the Holarctic regio |
| Q60567222 | Expansion of Sphagnum fallaxin bogs: striking the balance between N and P availability |
| Q55870391 | Expansion of invasive species on ombrotrophic bogs: desiccation or high N deposition? |
| Q108666360 | Exploring near-surface ground ice distribution in patterned-ground tundra: correlations with topography, soil and vegetation |
| Q60567207 | Exploring the contributions of vegetation and dune size to early dune building using unmanned aerial vehicle (UAV)-imaging |
| Q60567206 | Exploring the contributions of vegetation and dune size to early dune development using unmanned aerial vehicle (UAV) imaging |
| Q114164440 | Extremely wet summer events enhance permafrost thaw for multiple years in Siberian tundra |
| Q33575094 | Forage plants of an Arctic-nesting herbivore show larger warming response in breeding than wintering grounds, potentially disrupting migration phenology |
| Q51564643 | Glasshouse vs field experiments: do they yield ecologically similar results for assessing N impacts on peat mosses? |
| Q110509562 | Global CO2 fertilization of Sphagnum peat mosses via suppression of photorespiration during the twentieth century |
| Q110509333 | Green beach vegetation dynamics explained by embryo dune development |
| Q110871282 | High‐resolution peat volume change in a northern peatland: Spatial variability, main drivers, and impact on ecohydrology |
| Q60567221 | How Phosphorus Availability Affects the Impact of Nitrogen Deposition on Sphagnum and Vascular Plants in Bogs |
| Q30778795 | How does tree density affect water loss of peatlands? A mesocosm experiment |
| Q60567223 | How litter quality affects mass loss and N loss from decomposing Sphagnum |
| Q31151130 | Including hydrological self-regulating processes in peatland models: Effects on peatmoss drought projections |
| Q111496058 | Monitoring Impact of Salt-Marsh Vegetation Characteristics on Sedimentation: an Outlook for Nature-Based Flood Protection |
| Q60567224 | N deposition affects N availability in interstitial water, growth of Sphagnum and invasion of vascular plants in bog vegetation |
| Q60394920 | Nitrogen concentration and delta15N signature of ombrotrophic Sphagnum mosses at different N deposition levels in Europe |
| Q60394922 | Nutritional constraints in ombrotrophic Sphagnum plants under increasing atmospheric nitrogen deposition in Europe |
| Q55208923 | Peatland vegetation composition and phenology drive the seasonal trajectory of maximum gross primary production. |
| Q57263655 | Permafrost collapse after shrub removal shifts tundra ecosystem to a methane source |
| Q39062527 | Persistent versus transient tree encroachment of temperate peat bogs: effects of climate warming and drought events |
| Q59611208 | Phylogenetic or environmental control on the elemental and organo-chemical composition of Sphagnum mosses? |
| Q58412773 | Post-thaw variability in litter decomposition best explained by microtopography at an ice-rich permafrost peatland |
| Q60567219 | Precipitation determines the persistence of hollow Sphagnum species on hummocks |
| Q60499353 | Publisher Correction to: Background invertebrate herbivory on dwarf birch (Betula glandulosa-nana complex) increases with temperature and precipitation across the tundra biome |
| Q30884129 | Rain events decrease boreal peatland net CO2 uptake through reduced light availability |
| Q108666204 | Rapid Vegetation Succession and Coupled Permafrost Dynamics in Arctic Thaw Ponds in the Siberian Lowland Tundra |
| Q113102900 | Restoration of acidified and eutrophied rich fens: Long-term effects of traditional management and experimental liming |
| Q108666034 | Shrub decline and expansion of wetland vegetation revealed by very high resolution land cover change detection in the Siberian lowland tundra |
| Q30741152 | Spatio-temporal trends of nitrogen deposition and climate effects on Sphagnum productivity in European peatlands |
| Q60567213 | Sphagnum re-introduction in degraded peatlands: The effects of aggregation, species identity and water table |
| Q40444540 | Swift recovery of Sphagnum nutrient concentrations after excess supply |
| Q46273473 | The Sphagnome Project: enabling ecological and evolutionary insights through a genus-level sequencing project |
| Q60567215 | The effect of increased temperature and nitrogen deposition on decomposition in bogs |
| Q60567226 | The interaction between epiphytic algae, a parasitic fungus and Sphagnum as affected by N and P |
| Q114162614 | Tundra vegetation change and impacts on permafrost |
| Q126012589 | Upscaling peatland mapping with drone-derived imagery: impact of spatial resolution and vegetation characteristics |
| Q117427384 | Vascular plants affect properties and decomposition of moss-dominated peat, particularly at elevated temperatures |
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