ArticleFrontiers in microbiology2023
Responses of soil microbial biomass, microbial entropy and soil-microorganism stoichiometry imbalance to different utilization patterns in the artificial grassland of karst desertification area.
Article in Frontiers in microbiology, 2023. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 6 papers.
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Who cites it
6 citing papers in PubMed.
- Microbial Quotients and Stoichiometric Imbalance Reflect Divergent Responses to Wetland Land-Use Conversion.Microorganisms · 2026Article
- Stoichiometric properties of soil and microbial carbon, nitrogen, and phosphorus on the Jingpohu lava plateau.Scientific reports · 2026Article
- Fertilization Improves the Yield ofPlants (Basel, Switzerland) · 2025Article
- Biochar Addition Reduces the Effect of High Nitrogen on Soil-Microbial Stoichiometric Imbalance in Abandoned Grassland on the Loess Plateau of China.Ecology and evolution · 2025Article
- Responses of soil fertility indicators and fungi community diversity to fertilization strategies in legume-grass mixtures.Frontiers in plant science · 2025Article
- Impact of different forest types on soil microbial biomass and microbial entropy in the karst region of southwestern China.Frontiers in plant science · 2025Article
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5 authors.
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Abstract
Different utilization patterns can alter the C, N, P cycles and their ecological stoichiometry characteristics in grassland soils. However, the effects of different utilization patterns on soil microbial biomass, microbial entropy and soil-microorganism stoichiometry imbalance of artificial grassland are not clear. So this study was took different utilization patterns of artificial grassland [i.e., grazing grassland (GG), mowing grassland (MG), enclosed grassland (EG)] as the research object to investigate responses of soil microbial biomass, microbial entropy and soil-microorganism stoichiometry imbalance to different utilization patterns in the karst rocky desertification control area. We found that the contents of microbial biomass carbon (MBC) and microbial biomass nitrogen (MBN) were highest in GG, and the content of microbial biomass phosphorus (MBP) was highest in EG. Soil microbial biomass entropy carbon (qMBC) and soil microbial biomass entropy nitrogen (qMBN) of GG and MG were higher than those of EG, but soil microbial biomass entropy phosphorus (qMBP) was opposite. C:N stoichiometry imbalance (C:N
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