Issue |
E3S Web Conf.
Volume 375, 2023
8th International Conference on Energy Science and Applied Technology (ESAT 2023)
|
|
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Article Number | 01010 | |
Number of page(s) | 4 | |
Section | Fossil Energy & Geological Engineering | |
DOI | https://doi.org/10.1051/e3sconf/202337501010 | |
Published online | 27 March 2023 |
Response of rhizosphere microenvironment to coupling of climate warming and soil pollution
1
Institute of Land Engineering and Technology, Shaanxi Provincial Land Engineering Construction Group Co., Ltd,
Xi'an, China
2
Shaanxi Key Laboratory of Land Consolidation,
Xi'an 710075, China
3
Key Laboratory of Degraded and Unused Land Consolidation Engineering, the Ministry of Natural Resources,
Xi'an, China
4
Shaanxi Provincial Land Consolidation Engineering Technology Research Center,
Xi'an, China
* Corresponding author: 619648133@qq.com
With the development of industrialization, the pollution of heavy metals in soil, such as lead (Pb) and cadmium (Cd), has become increasingly serious. On the other hand, the century old climate warming is considered to be the result of the significant increase in the concentration of greenhouse gases, such as CO2, in the atmosphere. These changes will affect the function and stability of the terrestrial ecosystem. Therefore, in recent years, there are more and more studies on the effects of heavy metal pollution and elevated atmospheric CO2 concentration on plants. But most of them focus on the study of the aboveground part of herbaceous plants under the action of single factor, and the study of the soil microenvironment of woody plants under the combined action of these environmental factors is relatively less. This study summarized the response of rhizosphere microenvironment to the coupling of climate warming and soil pollution, in order to provide theoretical reference for improving soil quality and ecological environment.
Key words: Climate warming / Soil pollution / Rhizosphere microenvironment / Coupling effect
© The Authors, published by EDP Sciences, 2023
This is an Open Access article distributed under the terms of the Creative Commons Attribution License 4.0 (http://creativecommons.org/licenses/by/4.0/).
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