Influences of Quaternary sedimentary facies on soil organic carbon pool in Juhe watershed, Hebei Province

SUN Zijian; SHEN Wei; CHEN Ziran; FU Daqing; ZHANG Shoulin; ZHANG Huiqiong; CUI Xiaoying; FANG Weixuan

doi:10.12097/j.issn.1671-2552.2023.2-3.020

2023 Vol. 42, No. 2-3

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Article navigation > Geological Bulletin of China > 2023 > 42(2-3): 431-442

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SUN Zijian, SHEN Wei, CHEN Ziran, FU Daqing, ZHANG Shoulin, ZHANG Huiqiong, CUI Xiaoying, FANG Weixuan. 2023. Influences of Quaternary sedimentary facies on soil organic carbon pool in Juhe watershed, Hebei Province. Geological Bulletin of China, 42(2-3): 431-442. doi: 10.12097/j.issn.1671-2552.2023.2-3.020

Citation:

SUN Zijian, SHEN Wei, CHEN Ziran, FU Daqing, ZHANG Shoulin, ZHANG Huiqiong, CUI Xiaoying, FANG Weixuan. 2023. Influences of Quaternary sedimentary facies on soil organic carbon pool in Juhe watershed, Hebei Province. Geological Bulletin of China, 42(2-3): 431-442. doi: 10.12097/j.issn.1671-2552.2023.2-3.020

Influences of Quaternary sedimentary facies on soil organic carbon pool in Juhe watershed, Hebei Province

1.
School of Earth Sciences and Resources, China University of Geosciencs, Beijing 100083, China
2.
Beijing Institute of Geology for Mineral Resources CO., LTD., Beijing 100012, China
3.
514 Brigade of North China Geological Exploration Burea, Chengde 067060, Hebei, China
4.
China Non-ferrous Metals Resource Geological Survey, Beijing 100012, China

More Information

Corresponding author: FANG Weixuan, weixuanfang123@163.com

Received Date: 05 September 2022

Revised Date: 18 November 2022

Publish Date: 15 March 2023

Abstract

Abstract

The effects of parent materials on soil organic carbon (SOC) should not be ignored.This paper took Juhe watershed in Sanhe County, Hebei Province as the research object to discuss the difference of soil organic carbon density (SOCD) in different soils and influencing mechanism by their parent materials.According to the sedimentary environment of Holocene, the parent materials in the area were divided into alluvial-proluvial facies sediments (APFS), alluvial facies sediments (AFS) and lacustrine facies sediments (LFS).It was shown that there were significant variations of SOCD between soils developed in various parent materials via one-way analysis of variance, following the order AFS < APFS < LFS.Furthermore, the texture, nutrient elements concentrations, as well as physicochemical properties of soil, were comparatively analyzed, indicating that the influences of parent material on SOC were reflected on the influences of physicochemical property of soil on vegetation growth and development, the activity of soil flora, fauna and microorganism, and on the sequestration of organic carbon.From AFS, to APFS and to LFS, soil clay fraction gradually increased, which protect SOC from being decomposed by microorganisms since SOC were subjected to be coordinated with clay minerals into organo-mineral complex.On the other hand, LFS and APFS were characterized by more abundant water and nutrients than AFS, which contributed to vegetation growth and then input of SOC.In addition, microbial activity was strengthened, whose metabolites and residues after death are crucial source of SOC, increasing the storage of SOC.Our results could provide technological supports for the conservation and utilization of SOC in the Juhe watershed.
- sedimentary facies /
- clay fraction /
- soil organic carbon /
- Hebei plain /
- parent materials

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References

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