实现土壤失水过程的原位监测,对红壤区水土资源管理、自然灾害预警及防灾减灾具有重要意义。热脉冲法是目前土壤水热特性原位测量的常用方法,但红壤土失水时极易产生裂缝,单探针热脉冲法能否准确测定失水过程目前尚不清楚。通过室内模...实现土壤失水过程的原位监测,对红壤区水土资源管理、自然灾害预警及防灾减灾具有重要意义。热脉冲法是目前土壤水热特性原位测量的常用方法,但红壤土失水时极易产生裂缝,单探针热脉冲法能否准确测定失水过程目前尚不清楚。通过室内模拟土壤从饱和到干燥的连续失水过程,用时域反射法(TDR)作为标准对照,验证热脉冲方法测定土壤失水过程的准确性,并评估土壤裂缝产生后对单探针热脉冲法的影响。结果表明:随着土壤失水,土壤热导率K值由1.8 W/(m·K)减小到1.1 W/(m·K),热扩散率α值由1.0×10^(-8)m^(2)/s增加到3.0×10-8 m 2/s,比热容C值由1.8×108 J/(kg·K)减小到0.4×10^(8)J/(kg·K);接触热导率H值随着土壤失水具有台阶状变化特征,与土壤含水率变化速率的转折相吻合;与TDR测定结果相比,MAE和RMSE值分别为1.66和1.94 cm 3/cm^(3),R^(2)值为0.96;单探针热脉冲法能提供可靠的红壤土失水过程测定结果,且H值的变化能指征土壤裂隙的产生,可为土壤干湿循环过程、边坡和堤坝稳定性的动态监测提供技术和理论支撑。展开更多
We have developed an automatic emissive probe apparatus based on the improved inflection point method of the emissive probe for accurate measurements of both plasma potential and vacuum space potential.The apparatus c...We have developed an automatic emissive probe apparatus based on the improved inflection point method of the emissive probe for accurate measurements of both plasma potential and vacuum space potential.The apparatus consists of a computer controlled data acquisition card,a working circuit composed by a biasing unit and a heating unit,as well as an emissive probe.With the set parameters of the probe scanning bias,the probe heating current and the fitting range,the apparatus can automatically execute the improved inflection point method and give the measured result.The validity of the automatic emissive probe apparatus is demonstrated in a test measurement of vacuum potential distribution between two parallel plates,showing an excellent accuracy of 0.1 V.Plasma potential was also measured,exhibiting high efficiency and convenient use of the apparatus for space potential measurements.展开更多
Two different entry vehicles are presented here： the Inflatable Reentry and Descent Demonstrator （IRDT）, and Huygens. Both missions involve （re）entries at conditions close to orbital, and have been performed in 2...Two different entry vehicles are presented here： the Inflatable Reentry and Descent Demonstrator （IRDT）, and Huygens. Both missions involve （re）entries at conditions close to orbital, and have been performed in 2005. Specific aspects of the design and the mission of IRDT are briefly outlined. The preliminary results of the recent flight of IRDT and the methodology followed at ESTEC for the assessment of radiative fluxes for Huygens are summarised.展开更多
文摘实现土壤失水过程的原位监测,对红壤区水土资源管理、自然灾害预警及防灾减灾具有重要意义。热脉冲法是目前土壤水热特性原位测量的常用方法,但红壤土失水时极易产生裂缝,单探针热脉冲法能否准确测定失水过程目前尚不清楚。通过室内模拟土壤从饱和到干燥的连续失水过程,用时域反射法(TDR)作为标准对照,验证热脉冲方法测定土壤失水过程的准确性,并评估土壤裂缝产生后对单探针热脉冲法的影响。结果表明:随着土壤失水,土壤热导率K值由1.8 W/(m·K)减小到1.1 W/(m·K),热扩散率α值由1.0×10^(-8)m^(2)/s增加到3.0×10-8 m 2/s,比热容C值由1.8×108 J/(kg·K)减小到0.4×10^(8)J/(kg·K);接触热导率H值随着土壤失水具有台阶状变化特征,与土壤含水率变化速率的转折相吻合;与TDR测定结果相比,MAE和RMSE值分别为1.66和1.94 cm 3/cm^(3),R^(2)值为0.96;单探针热脉冲法能提供可靠的红壤土失水过程测定结果,且H值的变化能指征土壤裂隙的产生,可为土壤干湿循环过程、边坡和堤坝稳定性的动态监测提供技术和理论支撑。
基金supported by National Natural Science Foundation of China(No.11675039)
文摘We have developed an automatic emissive probe apparatus based on the improved inflection point method of the emissive probe for accurate measurements of both plasma potential and vacuum space potential.The apparatus consists of a computer controlled data acquisition card,a working circuit composed by a biasing unit and a heating unit,as well as an emissive probe.With the set parameters of the probe scanning bias,the probe heating current and the fitting range,the apparatus can automatically execute the improved inflection point method and give the measured result.The validity of the automatic emissive probe apparatus is demonstrated in a test measurement of vacuum potential distribution between two parallel plates,showing an excellent accuracy of 0.1 V.Plasma potential was also measured,exhibiting high efficiency and convenient use of the apparatus for space potential measurements.
文摘Two different entry vehicles are presented here： the Inflatable Reentry and Descent Demonstrator （IRDT）, and Huygens. Both missions involve （re）entries at conditions close to orbital, and have been performed in 2005. Specific aspects of the design and the mission of IRDT are briefly outlined. The preliminary results of the recent flight of IRDT and the methodology followed at ESTEC for the assessment of radiative fluxes for Huygens are summarised.
