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Published on: November 10, 2023
Nitrogen-mediated effects of elevated CO2 on intra-aggregate soil pore structure
Joshua S Caplan1, Daniel Giménez1, Vandana Subroy1
1Department of Environmental Sciences, Rutgers, The State University of New Jersey, 14 College Farm Road, New Brunswick, New Jersey, 19010, USA.
Nitrogen fertilization and elevated carbon dioxide (CO2) alter soil pore structure and water retention. These changes, driven by plant and microbial activity, impact water availability and soil functions.
Area of Science:
- Soil Science
- Ecology
- Biogeochemistry
Background:
- Soil pore structure critically influences water retention, affected by plant and microbial dynamics.
- Interactions between nitrogen (N) availability and elevated atmospheric CO2 (eCO2) on soil biota are known, but their impact on soil structure and water retention is unclear.
Purpose of the Study:
- To investigate how factorial additions of N and eCO2 affect soil pore structure and water retention in a long-term experiment.
- To understand the role of biotic factors in mediating these structural changes.
Main Methods:
- Analysis of soil aggregate fractal properties using 3D microtomographic imagery.
- Long-term field experiment with factorial N and eCO2 treatments on a sandy loam soil with Paspalum notatum.
Main Results:
- N fertilization increased intra-aggregate porosity and pore space in larger aggregates, an effect amplified by eCO2, leading to higher water retention near the wilting point.
- eCO2 alone reduced pore space in larger aggregates, decreasing water retention.
- Observed structural changes were linked to organic matter dynamics.
Conclusions:
- Rising atmospheric CO2 concentrations may induce N-dependent changes in soil pore structure, impacting global water balance, carbon storage, and rhizosphere functions.
- Understanding these soil structural shifts is crucial for predicting ecosystem responses to climate change.
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