Plant diversity and soil microbial diversity are closely related, and they maintain the health
and stability of terrestrial ecosystems. As a hotspot region of global biodiversity research …

Alterations in aboveground plant litter inputs due to global climate change can strongly
change soil nitrogen (N) cycling, which will influence soil processes and functions. However …

Enhanced frequency and intensity of freeze-thaw cycle (FTC) owing to global climate
change may influence soil carbon (C) and phosphorus (P) cycling in terrestrial ecosystems …

Reduction in snow cover is a prominent aspect of global change. Freeze–thaw cycles
(FTCs) of different amplitudes and durations in soil due to insufficient thermal insulation may …

Altered drying-rewetting patterns due to climate change may affect soil nitrogen (N) and
phosphorus (P) cycling in terrestrial ecosystems. The responses of soil N and P cycling to …

Interactions between nitrogen (N) and phosphorus (P) are important for plant growth and
ecosystem carbon (C) sequestration. While effects of N supply on P dynamics have been …

Climate change in Arctic landscapes may increase freeze–thaw frequency within the active
layer as well as newly thawed permafrost. Freeze-thaw is a highly disruptive process that …

Denitrification and leaching nitrogen (N) losses are poorly constrained in Earth System
Models (ESMs). Here, we produce a global map of natural soil 15N abundance and quantify …

Freeze-thaw cycles (FTCs) usually occur in the nongrowing season of crops, and the
temporal mismatch between soil nitrogen (N) supply and crop N utilization increases the risk …

Freeze–thaw (FT) cycles would alter physical and chemical properties of soil and thus
influence the transport of plastic particles (one type of emerging contaminant with great …