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A New Approach for Determination of Volumetric Water Content in Soil Samples by Gamma-Ray Transmission

机译:伽马射线透射法测定土壤样品中含水量的新方法

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A new method was presented for the purpose of volumetric water content determination in any soil sample by gamma-ray transmission. Monte Carlo (MC) simulation technique was used to determine the functional behavior of the linear attenuation coefficient of soil samples having different water contents for three soil samples. Using this functional behavior, the linear attenuation coefficients of dry soil and water were obtained from the intercept and the slope, respectively. It was experimentally shown that the mass attenuation coefficients of soil samples were not sensitive to the chemical composition but only to the physical density. This independence was exploited in this study to obtain the linear attenuation coefficient of a completely dry soil which was found to be 0.1409, 0.1274, and 0.1657 cm(-1) for Gumushane, Ardahan, and Trabzon soil, respectively. The linear attenuation coefficient of water was determined to be 0.09 cm(-1). Then, the volumetric water contents were obtained by measuring the gamma-ray intensities passed through three wet soil samples. The results were found to be 0.186, 0.182, and 0.214 cm(3) cm(-3) for Gumushane, Ardahan, and Trabzon soil, respectively. The results obtained by the method introduced were compared with the results obtained using gravimetric method. A very good agreement was observed.
机译:提出了一种新方法,用于通过伽马射线透射法测定任何土壤样品中的含水量。使用蒙特卡洛(MC)模拟技术来确定三个土壤样品中含水量不同的土壤样品的线性衰减系数的功能行为。利用这种功能行为,分别从截距和斜率获得了干燥土壤和水的线性衰减系数。实验表明,土壤样品的质量衰减系数对化学成分不敏感,而对物理密度敏感。在这项研究中利用了这种独立性来获得完全干燥的土壤的线性衰减系数,对于Gumushane,Ardahan和Trabzon的土壤,线性衰减系数分别为0.1409、0.1274和0.1657 cm(-1)。水的线性衰减系数确定为0.09 cm(-1)。然后,通过测量穿过三个湿土壤样品的伽马射线强度来获得体积水含量。结果被发现分别为Gumushane,Ardahan和Trabzon土壤的0.186、0.182和0.214 cm(3)cm(-3)。将通过介绍的方法获得的结果与使用重量分析法获得的结果进行比较。观察到非常好的协议。

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