Welcome to Chinese Journal of Ecology! Today is Share:

cje

Previous Articles     Next Articles

Integrated diagnostic model of soil moisture.

MI Chang-hong1, ZHENG Hong-yan1, HOU Xian-da2, HOU Yan-lin1,2*, LIU Shu-tian1,2, HUANG Zhi-ping1, DING Jian1, WANG Shuo-jin2   

  1. (1Agro-Environmental Protection Institute, Ministry of Agriculture, Tianjin 300191, China;  2Key Laboratory of Environment Change and Resources Use in Beibu Gulf (Guangxi Teachers Education University), Ministry of Education/Guangxi Key Laboratory of Earth Surface Processes and Intelligent Simulation (Guangxi Teachers Education University), Nanning 530001, China).
  • Online:2017-12-10 Published:2017-12-10

Abstract:

The principle and method of integrated diagnostic model of soil moisture were introduced, which synthesizes balance diagnostic model, statistical diagnostic model, subtractive statistical diagnostic model, ratio statistical diagnostic model, interval days statistics diagnostic model and moving statistics diagnostic model. The model was established by using the data of 87 monitoring sites in 23 counties in 7 provinces during the period of 2012-2014, and was validated by using the data of 2015. The results showed that the integrated model had high qualification rate (>97%) in diagnosis and prediction. The advantages of integrated diagnostic model are embodied as: (1) the parameters of the six independent models are different under different climates, underlying surface and management measures. Therefore, the six independent models are not universal even by sitespecific statistics. (2) In the same prediction, one of the prediction results of the six models always has relatively high accuracy. This result is highly correlated with the sum of the precipitation in different periods and the initial soil water content. After adaptive optimization of the six models, the predicted result is selected according to the sum of water income by the probability.
 

Key words: conservation tillage, soil total porosity, soil infiltration rate, evaporation characteristics., soil bulk density, saturated water conductivity