不同土地利用方式下冻融期黑土水热过程观测研究

Dynamics of soil water and soil temperature during freezing and thawing period under different types of land use in Mollisols

  • 摘要: 冻融是我国季节性冻土区重要的自然环境特征,冻融过程中土壤水热变化影响着生态系统的功能。本文利用长期定位试验,监测对比分析了东北典型黑土冻融过程中,传统耕作、草地和裸地3种土地利用方式下黑土水热动态变化规律。结果表明:观测期内,月尺度和日尺度上土壤温度、液态含水量和电导率变化趋势基本一致。不同冻融阶段,土壤温度表现为解冻期>始冻期>完全冻结期,土壤液态含水量表现为始冻期≈解冻期>完全冻结期,土壤电导率表现为始冻期>解冻期>完全冻结期。对于不同土地利用方式,土壤温度在各冻融阶段均表现为裸地>草地>传统耕作。在始冻期,土壤液态含水量和电导率均表现为裸地>传统耕作>草地。在完全冻结期,土壤液态含水量表现为传统耕作>裸地>草地,土壤电导率表现为裸地>传统耕作>草地。在解冻期,土壤液态含水量表现为草地>传统耕作>裸地,土壤电导率表现为传统耕作>草地>裸地。

     

    Abstract: Soil thawing-freezing process is one of the important environment characteristics in the seasonal frozen soil regions, and the dynamics of soil water and soil temperature influences ecosystem functions.Based on a longterm field experiment, the variations of soil water, temperature and electrical conductivity under conventional tillage, grassland and bare land were observed and analyzed during the thawing-freezing process in a typical Mollisols of China.Results showed that the dynamics of soil water, temperature and electrical conductivity was similar at daily and monthly scale during the observation period.In different freezing-thawing periods, soil temperature decreased in the order of thawing period, freezing period and frozen period.Soil water content in thawing period and freezing period was greater than that in frozen period, respectively.Soil electrical conductivity decreased in the order of freezing period, thawing period and frozen period.For different land use types, soil temperature decreased in the order of bare land, grassland and conventional tillage.During freezing period, both soil water content and soil electrical conductivity decreased was in the order of bare land, conventional tillage and grassland, respectively.During frozen period, soil water content decreased in the order of conventional tillage, bare land and grassland; soil electrical conductivity decreased in the order of bare land, conventional tillage and grassland.During thawing period, soil water content decreased in the order of grassland, conventional tillage and bare land; soil electrical conductivity decreased in the order of conventional tillage, grassland and bare land.

     

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