Water content

  1. Soil moisture drove vegetation change on the Qinghai-Tibetan Plateau
    Soil moisture constraints override atmospheric aridity in governing vegetation dynamics across the warming Qinghai-Tibetan Plateau, with regional variation depending on basin hydrogeography.
  2. Freeze–thaw reshapes water, salt, and heat in saline farmland soil
    Freeze-thaw driven water-salt redistribution in saline farmland soils: quantified hydrothermal parameters and coupled migration mechanisms from field-laboratory verification.