Manure applications support crop production, maintain soil fertility, and recycle locally
available nutrients in cold humid temperate regions, consistent with the principles of …

There are increasing demands to reduce greenhouse gas emissions from agricultural soils
worldwide. A significant portion of these emissions occur in cold regions during soil's …

Global climate change may result in changes in snow cover, which may enhance freeze-
thaw phenomena in mid and high latitude and high elevation ecosystems, especially in the …

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 …

Altered freeze‐thaw cycle (FTC) patterns due to global climate change may affect nitrogen
(N) cycling in terrestrial ecosystems. However, the general responses of soil N pools and …

Agricultural activity is the major anthropogenic source of nitrous oxide (N2O) emissions from
terrestrial ecosystems. Conservation agriculture including crop residue management can …

Nitrous oxide (N 2 O) emissions are highly variable in space and time due to the complex
interplay between soil, management practices and weather conditions. Micrometeorological …

Crop residues are sources of carbon and nitrogen (N) after harvest, releasing inorganic N
through mineralization or protecting soil N through immobilization. Inorganic N controls …

As an important factor regulating soil carbon cycle, freeze-thaw cycle significantly affects
winter soil respiration in temperate regions. However, few in situ studies have been carried …

The winter climate is changing in many parts of the world, and it is predicted that winter
climate change will modify the structure and function of plant–soil systems. An …