Changes of Soil Ecological Stoichiometry in Rhizosphere of Alfalfa Under Salt Stress

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      Soil ecological stoichiometry in the rhizosphere of alfalfa undergoes significant alterations under salt stress, affecting nutrient cycling, microbial activity, and plant-microbe interactions. Salt stress influences the balance of carbon (C), nitrogen (N), and phosphorus (P), disrupting the elemental ratios critical for optimal growth. In the rhizosphere, these changes often lead to a reduction in microbial biomass C and N, as well as shifts in the C:N:P ratio, indicating microbial nutrient limitation and altered decomposition processes. Alfalfa roots may adapt by modifying exudation patterns and nutrient uptake strategies, influencing the surrounding soil microenvironment. Understanding these stoichiometric changes is crucial for improving alfalfa resilience, optimizing fertilization, and enhancing productivity in saline soils.

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#SoilStoichiometry #RhizosphereEcology #AlfalfaUnderStress #SaltStressImpact #SoilMicrobiology #NutrientCycling #SoilHealth #CarbonNitrogenPhosphorus #MicrobialEcology #SalinityTolerance #SoilPlantInteractions #RhizosphereDynamics #AlfalfaRoots #SalineSoils #SustainableAgriculture #SoilBiochemistry #ElementalStoichiometry #SoilStressResponse #PlantMicrobeInteraction #Agroecology




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