Soils from cold and snowy temperate deciduous forests release more nitrogen and phosphorus after soil freeze–thaw cycles than soils from warmer, snow-poor conditions
- Location
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Deutsche Nationalbibliothek Frankfurt am Main
- Extent
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Online-Ressource
- Language
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Englisch
- Bibliographic citation
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Soils from cold and snowy temperate deciduous forests release more nitrogen and phosphorus after soil freeze–thaw cycles than soils from warmer, snow-poor conditions ; volume:17 ; number:15 ; year:2020 ; pages:4103-4117
Biogeosciences ; 17, Heft 15 (2020), 4103-4117
- Creator
- DOI
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10.5194/bg-17-4103-2020
- URN
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urn:nbn:de:101:1-2020082005453636187132
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
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14.08.2025, 11:03 AM CEST
Data provider
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Associated
- Kreyling, Jürgen
- Schumann, Rhena
- Weigel, Robert
Other Objects (12)
Soils from cold and snowy temperate deciduous forests release more nitrogen and phosphorus after soil freeze-thaw cycles than soils from warmer, snow-poor conditions
Impact of freeze–thaw cycles on soil structure and soil hydraulic properties
Impact of freeze-thaw cycles on soil structure and soil hydraulic properties
Dinitrogen (N2) pulse emissions during freeze-thaw cycles from montane grassland soil
Material cycling of wetland soils driven by freeze-thaw effects
Soil dielectric characterization during freeze–thaw transitions using L-band coaxial and soil moisture probes
Litter removal reduced soil nitrogen mineralization in repeated freeze-thaw cycles
Soil dielectric characterization at L-band microwave frequencies during freeze-thaw transitions
Effects of freeze–thaw on bank soil mechanical properties and bank stability
Freeze-thaw strength increases microbial stability to enhance diversity-soil multifunctionality relationship
Soil age and soil organic carbon content shape biochemical responses to multiple freeze–thaw events in soils along a postmining agricultural chronosequence
Seasonal freeze‒thaw processes impact microbial communities of soil aggregates associated with soil pores on the Qinghai–Tibet Plateau
Soils from cold and snowy temperate deciduous forests release more nitrogen and phosphorus after soil freeze-thaw cycles than soils from warmer, snow-poor conditions
Impact of freeze–thaw cycles on soil structure and soil hydraulic properties
Impact of freeze-thaw cycles on soil structure and soil hydraulic properties
Dinitrogen (N2) pulse emissions during freeze-thaw cycles from montane grassland soil
Material cycling of wetland soils driven by freeze-thaw effects
Soil dielectric characterization during freeze–thaw transitions using L-band coaxial and soil moisture probes
Litter removal reduced soil nitrogen mineralization in repeated freeze-thaw cycles
Soil dielectric characterization at L-band microwave frequencies during freeze-thaw transitions
Effects of freeze–thaw on bank soil mechanical properties and bank stability
Freeze-thaw strength increases microbial stability to enhance diversity-soil multifunctionality relationship
Soil age and soil organic carbon content shape biochemical responses to multiple freeze–thaw events in soils along a postmining agricultural chronosequence
Seasonal freeze‒thaw processes impact microbial communities of soil aggregates associated with soil pores on the Qinghai–Tibet Plateau
Soils from cold and snowy temperate deciduous forests release more nitrogen and phosphorus after soil freeze-thaw cycles than soils from warmer, snow-poor conditions
Impact of freeze–thaw cycles on soil structure and soil hydraulic properties
Impact of freeze-thaw cycles on soil structure and soil hydraulic properties
Dinitrogen (N2) pulse emissions during freeze-thaw cycles from montane grassland soil
Material cycling of wetland soils driven by freeze-thaw effects
Soil dielectric characterization during freeze–thaw transitions using L-band coaxial and soil moisture probes
Litter removal reduced soil nitrogen mineralization in repeated freeze-thaw cycles
Soil dielectric characterization at L-band microwave frequencies during freeze-thaw transitions
Effects of freeze–thaw on bank soil mechanical properties and bank stability
Freeze-thaw strength increases microbial stability to enhance diversity-soil multifunctionality relationship
Soil age and soil organic carbon content shape biochemical responses to multiple freeze–thaw events in soils along a postmining agricultural chronosequence