ORIGINAL RESEARCH
Impact of CO2 Leakage from Geological
Storage on the Eco-environment: Rhizosphere
Microenvironment of Soybean Case
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1
College of Advanced Agricultural Sciences, Yulin University, Yulin, Shaanxi 719000, China
2
Shaanxi Key Laboratory of Carbon Neutralization Technology, Carbon Neutral College (Yulin), Northwest University,
Xi'an, Shaanxi, 710069, China
3
National & Local Joint Engineering Research Center of Carbon Capture and Storage Technology, Department of
Geology, Northwest University, Xi'an, Shaanxi, 710069, China
4
China National Logging Corporation, Xi'an, Shaanxi, 710077, China
5
College of Resources and Environment, University of Chinese Academy of Sciences, Beijing, 101408, China
Submission date: 2025-05-28
Final revision date: 2025-11-05
Acceptance date: 2025-11-15
Online publication date: 2026-03-09
Corresponding author
Lua Xue
College of Advanced Agricultural Sciences, Yulin University, Yulin, Shaanxi 719000, China
Yu Mou
China National Logging Corporation, Xi'an, Shaanxi, 710077, China
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ABSTRACT
As a crucial technology for global CO2 reduction, CO2 capture and storage (CCS) faces leakage risks
that endanger surrounding organisms and the environment. This study aimed to clarify how CO2 leakage
impacts the rhizosphere soil's physicochemical properties and microbial communities, supporting CCS
environmental risk assessments. A simulation platform was built, and the 16S rDNA high-throughput
sequencing, correlation, and redundancy analyses were used to examine soybean cultures. Results
showed that as soil CO2 concentration rose, pH and O2 significantly declined, while Soil Organic
Carbon and Ammonium Nitrogen increased. Total Nitrogen and Nitrate Nitrogen decreased, with the
latter dropping notably. Microbial Biomass Carbon and Nitrogen in soybean rhizosphere soil rose at
10% and 30% CO2 but fell at 50%. CO2 leakage reduced the Chao1 index of rhizosphere soil bacteria
yet increased the Pielou’s evenness index. Although dominant bacterial phyla remained consistent,
Bacteroidetes became more abundant, while Proteobacteria, Acidobacteria, and Nitrospirae decreased.
O2 and pH were key factors shaping bacterial diversity and phylum-level community abundance.