ArticleMicroorganisms2024
The Process of Soil Carbon Sequestration in Different Ecological Zones of Qingtu Lake in the Arid-Semi-Arid Region of Western China.
Article in Microorganisms, 2024. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 3 papers.
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The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.
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Who cites it
3 citing papers in PubMed.
- Rhizosphere Ion Composition Shapes Microbial Communities and Is Associated with Plant Growth Variation in Saline-Alkali Soils.Microorganisms · 2026Article
- Soil carbon, micronutrients and microbiological dynamics under cash crop-based cropping systems in semi-arid National Capital Region of India.Scientific reports · 2026Article
- Multiscale responses to combined drought and salinity stress inFrontiers in plant science · 2025Review
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Authors and funding
7 authors.
Funding
Abstract
As a vital component of the global carbon pool, soils in arid and semi-arid regions play a significant role in carbon sequestration. In the context of global warming, increasing temperatures and moisture levels promote the transformation of barren land into wetlands, enhancing carbon sinks. However, the overdevelopment of oases and excessive extraction of groundwater lead to the opposite effect, reducing carbon sequestration. This study examines two soil types-meadow soil (MS) and swamp soil (SS)-from Qingtu Lake, an arid lake in western China. It analyzes the sources of soil inorganic carbon, the composition and origin of dissolved organic matter (DOM), and the relationships between microbes, soil organic carbon (SOC), soil inorganic carbon (SIC), mineral composition, and soil texture. The results indicate that inorganic carbon in the study area consists of both primary carbonate minerals and secondary pedogenic carbonates. The DOM primarily consists of two components, both identified as terrestrial humic substances. In meadow soils, bacterial activity drives the weathering of plagioclase, which releases Ca
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