利用热脉冲技术测量土壤表层含水率  

Measuring soil water content in surface layer with heat-pulse technique

作　　者：张晓[1] 王月月[2] 任图生[2] 

机构地区：[1]中国林业科学院荒漠化研究所,北京100091 [2]中国农业大学土壤与水科学系,北京100193

出　　处：《农业工程学报》2015年第2期72-78,共7页Transactions of the Chinese Society of Agricultural Engineering

基　　金：国家自然科学基金项目(41271238;41071155)

摘　　要：准确测定表层土壤水分对陆地-大气间水热交换研究具有重要意义。由于对土壤结构影响轻微,热脉冲技术在原位监测含水率方面具有较大优越性,但目前田间应用集中在5 cm以下土层。该研究利用多针热脉冲传感器测定土壤容积热容量,然后基于热脉冲含水率法和热脉冲含水率变化法分别得到了3、9、21和39 mm的土壤含水率。结果表明,与烘干法含水率比较,热脉冲含水率变化法含水率在4个深度的均方根误差分别为0.022、0.006、0.004和0.006 m3/m3,均小于相应深度上热脉冲含水率法含水率的均方根误差。另外,热脉冲含水率变化法也降低了4个热脉冲传感器测定含水率的变异性。因此,热脉冲技术能够监测表层的土壤水分动态,表层土壤含水率的均方根误差在0.022 m3/m3以内。Accurate measurement of near-surface soil water content （0-5 cm） is essential for studying water and heat exchange between land and atmosphere. Heat-pulse technique has potential to measure soil volumetric water content, but only used in laboratory, greenhouse and field at depths below 5 cm. The objective of this study was to test the possibility of heat-pulse technique for measuring water content in near-surface soil layer （0-5 cm） in the field. The experiment was conducted in a sandy loam soil in an experimental plot （2 m×2 m×2m） in China Agricultural University. Multi-needle heat-pulse sensor was used to measure volumetric heat capacity in various depths above 5 cm and four multi-needle heat-pulse sensors were used. Average volumetric heat capacity from four multi-needle heat-pulse sensors was calculated at each depth and the values at four depths （3, 9, 21 and 39 mm） were extracted to be analyzed. When calculating soil volumetric heat capacity from temperature change versus time data, the pulse infinite line source theory was used at 9, 21 and 39 mm, while for volumetric heat capacity at 3 mm, the pulse infinite line source-adiabatic boundary condition was used because of the soil-air interface effect. Based on the linear relationship of soil volumetric heat capacity and volumetric water content in mineral soil, soil volumetric water content could be calculated from soil volumetric heat capacity, volumetric heat capacity of water, soil bulk density and solid heat capacity, which was named heat-pulse water content method. When the temporal series of soil volumetric heat capacity were measured, the change in soil water content could be calculated without knowledge of soil-specific properties. With the initial water content measured by another independent method, dynamic of soil water content could be determined from the change in soil water content series data and this method was called heat-pulse water content change method. Water contents at those four depths were calculated by the above two

关 键 词：土壤 水分 热传导 热脉冲技术 表层 

分 类 号：S152.8[农业科学—土壤学]