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生态学杂志 ›› 2026, Vol. 45 ›› Issue (4): 1069-1079.doi: 10.13292/j.1000-4890.202604.003

• ·城市生态系统保护与高质量发展专栏· • 上一篇    下一篇

城市化进程中绿地GRSP对土壤有机碳库的贡献及其影响因素

邹庆娴1,2,张佛熠1,3,钟嘉琳1,2,廖桂军1,2,刘玮1,2,王琼1,2*   

  1. 1江西农业大学林学院/园林与艺术学院, 南昌 330045; 2亚热带森林资源培育江西省重点实验室, 南昌 330045; 3云南大学生态与环境学院, 昆明 650000)

  • 出版日期:2026-04-10 发布日期:2026-04-09

Contribution of glomalin-related soil protein in urban greenspace to soil organic carbon storage and its influencing factors during urbanization.

ZOU Qingxian1,2, ZHANG Foyi1,3, ZHONG Jialin1,2, LIAO Guijun1,2, LIU Wei1,2, WANG Qiong1,2*   

  1. (1College of Forestry/Landscape and Art, Jiangxi Agricultural University, Nanchang 330045, China; 2Jiangxi Key Laboratory of Subtropical Forest Resources Cultivation, Nanchang 330045, China; 3School of Ecology and Environmental Science, Yunnan University, Kunming 650000, China).

  • Online:2026-04-10 Published:2026-04-09

摘要: 丛枝菌根真菌分泌的球囊霉素相关土壤蛋白(glomalin-related soil protein,GRSP)是土壤有机碳(SOC)的重要组成部分,是土壤碳汇变化的重要表征指标之一。在快速城市化过程中,GRSP是否能够增强土壤固碳及其影响机制尚不清楚。本研究选取南昌市建成区(505 km2)的184个绿地样地,通过不透水面面积比例来划分城市化强度,并分析城市化对SOC、GRSP及纯化GRSP的C(GRSP-C)等含量的影响及其与土壤理化性质、植被特征和景观格局的相关关系。结果表明:低城市化地区的GRSP和GRSP-C含量显著高于高城市化地区(19.35%和13.21%)(P<0.05);从低城市化到高城市化区域,SOC从18.64 mg·g-1下降到15.02 mg·g-1,而GRSP-C对SOC的贡献率从3.89%减少到2.04%,城市化进程显著降低GRSP与GRSP-C对SOC的固持作用;冗余分析表明,土壤pH、土壤全钾、树木冠幅和绿地斑块总边界长度是城市化进程中影响GRSP固碳差异的主要环境因子;较高的土壤全钾不利于积累GRSP和GRSP-C;土壤pH与GRSP/SOC、GRSP-C对SOC的贡献率呈负相关,而较大的树木冠幅和斑块总边界长度则可以促进GRSP对SOC的贡献率。本研究系统探索了GRSP对SOC的固存作用,尽管这种作用会受到城市化过程影响,但其仍然是一种较新的助力城市绿地土壤碳中和的路径。


关键词: 球囊霉素相关土壤蛋白, 土壤有机碳, 城市化, 城市绿地

Abstract: Glomalin-related soil protein (GRSP) secreted by arbuscular mycorrhizal fungi is an important component of soil organic carbon (SOC) and one of the important indicators of changes in soil carbon sequestration. The ability of GRSP to enhance soil carbon sequestration and its influencing mechanisms during rapid urbanization remains unclear. We selected 184 greenspace plots from the built-up area in Nanchang (505 km2) and categorized urbanization intensity based on the proportion of impervious surface area to total area. We then analyzed the effects of urbanization intensity on the contents of SOC, GRSP, and purified GRSP-containing carbon (GRSP-C), as well as their correlations with soil physicochemical properties, vegetation characteristics, and landscape patterns. The results showed that GRSP and GRSP-C contents were significantly higher in lowly urbanized areas than in highly urbanized areas by 19.35% and 13.21%, respectively (P<0.05). From lowly to highly urbanized areas, SOC content decreased from 18.64 mg·g-1 to 15.02 mg·g-1, accompanied by a decline in the contribution rate of GRSP-C to SOC from 3.89% to 2.04%, indicating that urbanization significantly weakened the roles of GRSP and GRSP-C in SOC sequestration. The redundancy analysis revealed that soil pH, soil total potassium, tree canopy size, and the total boundary length of greenspace patches were the main factors affecting the changes in the GRSP-related carbon sequestration during urbanization. A high soil total potassium content was not conducive to the accumulation of GRSP and GRSP-C. Soil pH was negatively correlated with the GRSP/SOC ratio and the contribution rate of the GRSP-C content to SOC, while larger tree canopy sizes and total boundary length increased the contribution rate of GRSP to SOC. By systematically investigating the role of GRSP in SOC sequestration, this study confirms that GRSP is a relatively novel pathway for contributing to soil carbon neutrality in urban greenspaces, even though its role could be influenced by urbanization.

Key words: glomalin-related soil protein, soil organic carbon, urbanization, urban greenspace