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国家自然科学基金(40025106)

作品数:3 被引量:83H指数:3
相关作者:任图生邵明安巨兆强更多>>
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利用热脉冲-时域反射技术测定土壤水热动态和物理参数 Ⅰ.原理被引量:54
2004年
由于土壤特性的时空变异性 ,对土壤含水量、温度、热特性以及其它物理参数的动态监测是土壤学研究的重要课题。本文以热脉冲技术和时域反射技术的理论为基础 ,介绍了利用热脉冲技术 时域反射技术 (Thermo TDR)连续定位测定土壤含水量、电导率、温度和热特性的原理 ,并利用土壤热特性与容重和含水量的关系 ,导出了土壤容重、饱和度和通气孔度的计算公式。
任图生邵明安巨兆强Horton Robert
关键词:土壤物理性质
利用热脉冲时域反射技术测定土壤水热动态和物理参数Ⅱ.应用被引量:32
2004年
土壤含水量、温度、热特性以及其它物理参数的动态监测是描述土壤中各种物理、化学和生物过程的基础。本文利用热脉冲 -时域反射技术 (Thermo -TDR)对不同质地土壤的含水量、电导率、温度、容积热容量、导热率和热扩散系数进行了测定 ,并利用土壤容积热容量与容重和含水量的关系 ,计算了土壤容重、通气孔度和饱和度。结果表明 ,Thermo -TDR技术能够提供可靠的土壤含水量、温度、容重、通气孔度和饱和度的信息。本文也分析了Thermo
任图生邵明安巨兆强Horton Robert
关键词:土壤物理性质土壤含水量土壤温度导热率热扩散系数
Nitrate Accumulation in Soil Profile of Dry Land Farming in Northwest China被引量:25
2003年
A long-term fertilizer experiment on dry land of the Loess Plateau, northwest China, has been conducted since 1984 to study the distribution and accumulation of NO3-N down to a depth of 400 cm in the profile of a coarse-textured dark loessial soil after continuous winter wheat cropping. Thirteen fertilizer treatments consisted of four levels of N and P applied alone or in combination. Annual N and P (P2O5) rates were 0,45, 90, 135 and 180 kg ha-1. After 15 successive cropping cycles, the soil samples were taken from each treatment for analysis of NO3-N concentration. The results showed that NO3-N distribution in the soil profile was quite different among the treatments. The application of fertilizer N alone resulted in higher NO3-N concentration in the soil profile than the combined application of N and P, showing that application of P could greatly reduce the NO3-N accumulation. With an annual application of 180 kg N ha-1 alone, a peak in NO3-N accumulation occurred at 140 cm soil depth, and the maximum NO3-N concentration in the soils was 67.92 mg kg-1. The amount of NO3-N accumulated in the soil profile decreased as the cumulative N uptake by the winter wheat increased. Application of a large amount of N resulted in lower N recoveries in winter wheat and greater NO3-N accumulation in soil profile. NO3-N did not enter underground water in the study region; therefore, there is no danger of underground water pollution. Amount of NO3-N accumulation can be predicted by an equation according to annual N and P rates based on the results of this experiment.
FAN Jun, HAO Ming-De and SHAO Ming-AnState Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, the Chinese Academy of Sciences, Yangling 712100 (China).
关键词:硝酸盐堆积物土壤剖面农田
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