Evidence for late winter biogeochemical connectivity in permafrost soils

Keyphrases

• Late Winter 100%
• Permafrost Soils 100%
• Active Layer 100%
• Soil Pore Water 80%
• Isotope Composition 40%
• Water Exchange 40%
• Soil Water 40%
• Organic Carbon 40%
• Layer Soil 40%
• Silicon Isotopes 40%
• Dormant Season 20%
• Seasonal Flux 20%
• Mineral nutrients 20%
• Soil Organic Carbon Stock 20%
• Soil Organic Carbon 20%
• Summer Months 20%
• Organic nutrients 20%
• Water in Soil 20%
• Arctic Rivers 20%
• Permafrost Active Layer 20%
• Organic Minerals 20%
• Organic Carbon Transport 20%
• Nutrient Mobilization 20%
• Hot Moments 20%
• Carbon Mobilization 20%
• Key Supplier 20%

Earth and Planetary Sciences

• Active Layer 100%
• Porewater 66%
• Organic Carbon 50%
• Soil Water 33%
• Soil Organic Carbon 33%
• Water Exchange 33%
• Silicon Isotopes 33%
• Carbon Transport 16%