Application of Soil Temperature and Humidity Recorder in Arid Area of ​​Desert

In agricultural production, especially in arid regions, soil temperature and humidity are one of the most important factors affecting plant growth. Soil temperature and humidity generally include soil moisture, soil moisture temperature, soil moisture content, soil water potential, etc. Currently, soil temperature and humidity recorders are generally used to measure soil temperature and humidity. Soil temperature and humidity recorder can measure soil temperature and humidity. ,recording.

The spatial heterogeneity of soil temperature and humidity has a certain influence on the spatial distribution pattern of vegetation productivity. The dynamics of soil temperature and humidity are affected by the effects of water supplementation (rainfall, groundwater regulation, etc.) and water consumption (surface evaporation, vegetation transpiration, etc.). Through the secondary distribution of light, heat, water and other resources, the terrain has direct and indirect effects on the ecological processes of water supply and water consumption, resulting in spatial and temporal differences in soil moisture content and grassland productivity under different topographic conditions. There are different correlations between vegetation productivity and soil temperature and humidity at different temporal and spatial scales of biological systems.

Therefore, it is of great significance to carry out multi-scale studies to elucidate various ecological processes that affect the temperature and humidity migration of soil and the spatial and temporal differentiation of grassland productivity. In this paper, through the observation of soil moisture and grassland biomass in desert grassland of Yanchi County, Ningxia, the effects of topography on spatial and temporal heterogeneity of soil temperature and moisture and biomass were discussed. The relationship between soil moisture content at different depths and grassland biomass in different growth seasons was analyzed. To reveal the spatial-temporal distribution of soil temperature, humidity, and biomass under different topographic conditions and the key ecological factors affecting temperature and humidity migration and plant growth, and to provide a theoretical basis for explaining the stability of desert ecosystems and in-depth study of desertification areas.

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