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Nitrogen‐mediated effects of elevated CO 2 on intra‐aggregate soil pore structure
Author(s) -
Caplan Joshua S.,
Giménez Daniel,
Subroy Vandana,
Heck Richard J.,
Prior Stephen A.,
Runion G. Brett,
Torbert H. Allen
Publication year - 2017
Publication title -
global change biology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 4.146
H-Index - 255
eISSN - 1365-2486
pISSN - 1354-1013
DOI - 10.1111/gcb.13496
Subject(s) - soil structure , water retention , soil water , chemistry , soil science , bulk soil , rhizosphere , nitrogen , agronomy , environmental chemistry , soil organic matter , environmental science , biology , organic chemistry , bacteria , genetics
Soil pore structure has a strong influence on water retention, and is itself influenced by plant and microbial dynamics such as root proliferation and microbial exudation. Although increased nitrogen (N) availability and elevated atmospheric CO 2 concentrations (eCO 2 ) often have interacting effects on root and microbial dynamics, it is unclear whether these biotic effects can translate into altered soil pore structure and water retention. This study was based on a long‐term experiment (7 yr at the time of sampling) in which a C 4 pasture grass ( Paspalum notatum ) was grown on a sandy loam soil while provided factorial additions of N and CO 2 . Through an analysis of soil aggregate fractal properties supported by 3D microtomographic imagery, we found that N fertilization induced an increase in intra‐aggregate porosity and a simultaneous shift toward greater accumulation of pore space in larger aggregates. These effects were enhanced by eCO 2 and yielded an increase in water retention at pressure potentials near the wilting point of plants. However, eCO 2 alone induced changes in the opposite direction, with larger aggregates containing less pore space than under control conditions, and water retention decreasing accordingly. Results on biotic factors further suggested that organic matter gains or losses induced the observed structural changes. Based on our results, we postulate that the pore structure of many mineral soils could undergo N‐dependent changes as atmospheric CO 2 concentrations rise, having global‐scale implications for water balance, carbon storage, and related rhizosphere functions.