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Author Title Type [ Year
] Filters: Author is Santruckova, Hana [Clear All Filters]
. 2021. Coupling the resource stoichiometry and microbial biomass turnover to predict nutrient mineralization and immobilization in soil. Geoderma 385: 114884.
(797.47 KB). 2021. Soil Microbiome Composition along the Natural Norway Spruce Forest Life Cycle. Forests 12: 410.
. 2020. Positive response of soil microbes to long-term nitrogen input in spruce forest: Results from Gårdsjön whole-catchment N-addition experiment. Soil Biology & Biochemistry 143: 107732.
. 2018. In situ phosphorus dynamics in soil: long-term ion-exchange resin study. Biogeochemistry 139: 307-320.
2018. Significance of dark CO2 fixation in arctic soils. Soil Biology and Biochemistry 119: 11 - 21.
. 2018. Soil microbial biomass, activity and community composition along altitudinal gradients in the High Arctic (Billefjorden, Svalbard). Biogeosciences 15: 1879–1894.
. 2018. Species effects and seasonal trends on plant efflux quantity and quality in a spruce swamp forest. Plant and Soil 426: 179-196.
(1.15 MB). 2017. Indications that long-term nitrogen loading limits carbon resources for soil microbes. Soil Biology & Biochemistry 115: 310-321.
. 2017. Microbial communities with distinct denitrification potential in spruce and beech soils differing in nitrate leaching. Scientific Reports 7: 9738.
. 2017. Recovery of the ectomycorrhizal community after termination of long-term nitrogen fertilisation of a boreal Norway spruce forest. FUNGAL ECOLOGY 29: 116-122.
. 2017. Rhizodeposition flux of competitive versus conservative graminoid: contribution of exudates and root lysates as affected by N loading. Plant and Soil 412: 331 - 344.
2016. The Effect of P Enrichment on Exudate Quantity and Bioavailability - a Comparison of Two Macrophyte Species. WETLANDS 36: 789-798.
2016. Potential carbon emissions dominated by carbon dioxide from thawed permafrost soils. Nature Climate Change , doi:10.1038/NCLIMATE3054
2015. A larger investment into exudation by competitive versus conservative plants is connected to more coupled plant-microbe N cycling. Biogeochemistry 122: 47-59.