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Estimation of annual soil CO2 efflux under the erosion and deposition conditions by measuring and modeling its respiration rate in southern China

文献类型： 外文期刊

作者： Guo, Geng 1 ; Li, Xiao 2 ; Kuai, Jie 1 ; Zhang, Xiang 3 ; Peng, Xiaoying 1 ; Xu, Yanyin 4 ; Zeng, Guangruo 5 ; Liu, Jun 6 ; Zhang, Chen 7 ; Lin, Jie 1 ;

作者机构： 1.Nanjing Forestry Univ, Coinnovat Ctr Sustainable Forestry Southern China, Key Lab Soil & Water Conservat & Ecol Restorat Jia, Nanjing 210037, Jiangsu, Peoples R China

2.Huazhong Agr Univ, Coll Resources & Environm, Wuhan 430070, Hubei, Peoples R China

3.Suzhou Yihua Biomed Technol Co Ltd, Suzhou 215000, Jiangsu, Peoples R China

4.Yunnan Inst Trop Crops, Jinghong 666100, Yunnan, Peoples R China

5.Acad Forestry Jian City, Jian 343000, Jiangxi, Peoples R China

6.Soil & Water Conservat Ctr Xingguo Cty, Ganzhou 341000, Jiangxi, Peoples R China

7.Jiangxi Inst Red Soil & Germplasm Resources, Nanchang 330096, Jiangxi, Peoples R China

8.Nanjing Forestry Univ, 159 Longpan Rd, Nanjing 210037, Jiangsu, Peoples R China

关键词： Soil carbon efflux; Soil temperature; Soil moisture; Water erosion; Red soil

期刊名称：JOURNAL OF ENVIRONMENTAL MANAGEMENT （ 影响因子：8.7； 五年影响因子：8.4 ）

ISSN： 0301-4797

年卷期： 2024 年 351 卷

页码：

收录情况： SCI

摘要： Soil respiration (Rs) is a crucial ecological process of carbon (C) cycling in the terrestrial ecosystems, and soil erosion has a significant impact on its C budget and balance. However, the variations of Rs rate and their CO2 efflux induced by erosion are currently poorly understood. To this end, four landscape positions (top, up, middle and toe) with different erosional and depositional characteristics were selected on a typical eroded slope in southern China to conduct field experiments, aiming to explore the effects of erosion and deposition on Rs among various sites. From March 2021 to February 2022, the in-situ Rs were measured using an automated soil respiration system, together with soil temperature at 5 cm depth (T-s5) and water content at 10 cm depth (SWC10). We initially constructed various Rs models across a one-year period, based on its relationships with T-s5 and SWC10. Subsequently, the seasonal changes of Rs at different erosional sites were simulated by the optimum models, and their annual CO(2 )fluxes were further estimated. The results showed that Rs rates at all sites displayed a bimodal seasonal pattern, with the highest values in May and August. And the measured Rs of the eroding and depositional sites were 0.05-7.71 and 1.47-13.03 mu mol m(-2) s(-1), respectively. Also, remarkably higher T-s5 and SWC10 were observed in depositional sites versus the eroding sites (P < 0.05). Additionally, Rs rates at all sites were positively correlated with SOC and T-s5, but negatively correlated with SWC10. Herein, Rs models to single-and double-variable were established at different positions, and we found that the fitted R-2 and AIC differed on various sites, primarily in erosional and depositional sites. Furthermore, through the best-fitting models (higher R-2 and lowest AIC) we screened, the average Rs values of 3.03 and 4.46 mu mol m(-2) s(-1) were quantitatively estimated for the eroding and depositional sites, respectively. Finally, it could be further assessed that the mean annual soil CO2-C efflux of eroded site (1104.14 g m(-2)) was significantly lower than that of depositional site (1629.46 g m(-2)). These findings highlighted the effect of erosion and deposition on Rs, which will facilitate a better understanding of C cycling in terrestrial ecosystems.

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