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Updated: Jun 20, 2025

A CO2 Concentration Gradient Facility for Testing CO2 Enrichment and Soil Effects on Grassland Ecosystem Function
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纳米级栗子土壤孔状特征的变化是由温带草原的非生长季节降水引起的

Yifan Song1, Tiejun Liu1, Rui Jiao2

  • 1Yinshanbeilu Grassland Eco-hydrology National Observation and Research Station, China Institute of Water Resources and Hydropower Research, Beijing 100038, China; State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing 100044, China.

The Science of the total environment
|July 18, 2024
PubMed
概括

非生长季节降水变化显著影响温带草原土壤结构和营养循环. 改变的降水增加了土壤的多孔性,特定表面积和孔积,增强了土壤的碳积累.

关键词:
在纳米尺度上的纳米尺度.没有生长季节的季节.降水量 降水量 降水量土壤营养物质土壤营养物质土壤孔的特征 土壤孔的特征协同变化的协同变化.

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Though evaporation from plant leaves drives transpiration, it also results in loss of water. Because water is critical for photosynthetic reactions and other cellular processes, evolutionary pressures on plants in different environments have driven the acquisition of adaptations that reduce water loss.
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