Water Transport Through Soil, Plant, and Atmosphere

摘要: A quantitative model of water movement through any part the soil, plant, or Atmosphere requires a number physical assumptions. Sometimes this is in interest simplicity and economy, other times it required because experimental data fundamental theoretical information are not available. further set assumptions to interface each component representation with proper interaction feedback into an overall whole process. With introduction large complex models recent years, make selection necessary for modeler soil-plant-Atmosphere continuum (SPAC) examine more detail kind approaches being taken, as well degree success model.