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Hydrothermal variations in soils resulting from the freezing and thawing processes in the active layer of an alpine grassland in the Qilian Mountains, northeastern Tibetan Plateau

Northeastern Tibetan PlateauGround Heat FluxBiogeochemistryFreeze-thaw CyclingEngineeringHydrothermal GeochemistryAlpine GrasslandGeographyGeologyMountain UpliftGeochemistryEarth ScienceHydrothermal VariationsTibetan PlateauClimate Change