Climate Change Data Portal
DOI | 10.1111/sum.12895 |
Examining soil organic carbon in the mountainous peat swamps of the Zoige Plateau in China's Qinghai-Tibet Plateau | |
Zhang, Zhiwei; Zhao, Cheng-Zhang; Bai, Xuqian; Li, Qun; Ma, Min | |
发表日期 | 2023 |
ISSN | 0266-0032 |
EISSN | 1475-2743 |
起始页码 | 757 |
结束页码 | 770 |
卷号 | 39期号:2 |
英文摘要 | Mountainous peatlands are one of the most important terrestrial ecosystems for carbon storage and play an important role in the global carbon cycle. An insight into the carbon cycle of peat swamps located in mountainous regions can be obtained by studying the distribution of soil organic carbon (SOC) and its relationships with environmental factors. This study focused on the development conditions of peat swamps in the Gahai wetlands, located on the Zoige Plateau, China, with four different altitudinal gradients as experimental sample sites. The distribution of SOC and its relationship with environmental factors were analysed through vegetation surveys and a generalized additive model (GAM). The results show that with increasing altitude, soil temperature decreased while the soil pH and bulk density initially decreased then increased. On the contrary, the topographic wetness index (TWI), SOC content, above-ground biomass and litter count initially increased then decreased. The SOC content of the 0-30 cm soil layer was in the range 226-330 g center dot kg(-1) (coefficient of variation (CV) = 21.4%), and the 30-60 cm layer was 178-257 g center dot kg(-1) (CV = 17.5%) and was significantly correlated (p < .05) with above-ground biomass and litter count. Meanwhile, the SOC content in the 60-90 cm soil layer was in the range 132-167 g center dot kg(-1) (CV = 9.2%) with a significant correlation (p < .05) with soil temperature, pH, bulk density and topographic moisture index. The study showed that the SOC content exhibited more pronounced spatial patterns with increasing altitude, with the peak value in the shallow soil layer appearing in lower elevation areas compared with the deep soil layer. The level of variation changed from medium to low, reflecting the stable mechanism for maintaining SOC within the heterogeneous peat swamp environment. |
关键词 | elevationgeneralized additive modelpeat swampsoil organic carbonZoige Plateau |
英文关键词 | TERRESTRIAL ECOSYSTEMS; STOCKS; DECOMPOSITION; TEMPERATURE; GRASSLANDS; HOLOCENE; FLUXES; IMPACT |
WOS研究方向 | Soil Science |
WOS记录号 | WOS:000950073200001 |
来源期刊 | SOIL USE AND MANAGEMENT |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/283506 |
作者单位 | Northwest Normal University - China; Northwest Normal University - China; Northwest Normal University - China |
推荐引用方式 GB/T 7714 | Zhang, Zhiwei,Zhao, Cheng-Zhang,Bai, Xuqian,et al. Examining soil organic carbon in the mountainous peat swamps of the Zoige Plateau in China's Qinghai-Tibet Plateau[J],2023,39(2). |
APA | Zhang, Zhiwei,Zhao, Cheng-Zhang,Bai, Xuqian,Li, Qun,&Ma, Min.(2023).Examining soil organic carbon in the mountainous peat swamps of the Zoige Plateau in China's Qinghai-Tibet Plateau.SOIL USE AND MANAGEMENT,39(2). |
MLA | Zhang, Zhiwei,et al."Examining soil organic carbon in the mountainous peat swamps of the Zoige Plateau in China's Qinghai-Tibet Plateau".SOIL USE AND MANAGEMENT 39.2(2023). |
条目包含的文件 | 条目无相关文件。 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。