Cotton Production and Processing Unit, USDA-ARS, Lubbock, TX 79403, USA.
Sensors (Basel). 2011;11(3):2592-610. doi: 10.3390/s110302592. Epub 2011 Mar 1.
Accurate measurement of moisture content is a prime requirement in hydrological, geophysical and biogeochemical research as well as for material characterization and process control. Within these areas, accurate measurements of the surface area and bound water content is becoming increasingly important for providing answers to many fundamental questions ranging from characterization of cotton fiber maturity, to accurate characterization of soil water content in soil water conservation research to bio-plant water utilization to chemical reactions and diffusions of ionic species across membranes in cells as well as in the dense suspensions that occur in surface films. In these bound water materials, the errors in the traditional time-domain-reflectometer, "TDR", exceed the range of the full span of the material's permittivity that is being measured. Thus, there is a critical need to re-examine the TDR system and identify where the errors are to direct future research. One promising technique to address the increasing demands for higher accuracy water content measurements is utilization of electrical permittivity characterization of materials. This technique has enjoyed a strong following in the soil-science and geological community through measurements of apparent permittivity via time-domain-reflectometery as well in many process control applications. Recent research however, is indicating a need to increase the accuracy beyond that available from traditional TDR. The most logical pathway then becomes a transition from TDR based measurements to network analyzer measurements of absolute permittivity that will remove the adverse effects that high surface area soils and conductivity impart onto the measurements of apparent permittivity in traditional TDR applications. This research examines the theoretical basis behind the coaxial probe, from which the modern TDR probe originated from, to provide a basis on which to perform absolute permittivity measurements. The research reveals currently utilized formulations in accepted techniques for permittivity measurements which violate the underlying assumptions inherent in the basic models due to the TDR acting as an antenna by radiating energy off the end of the probe, rather than returning it back to the source as is the current assumption. To remove the effects of radiation from the experimental results obtain herein, this research utilized custom designed coaxial probes of various diameters and probe lengths by which to test the coaxial cell measurement technique for accuracy in determination of absolute permittivity. In doing so, the research reveals that the basic models available in the literature all omitted a key correction factor that is hypothesized by this research as being most likely due to fringe capacitance. To test this theory, a Poisson model of a coaxial cell was formulated to calculate the effective extra length provided by the fringe capacitance which is then used to correct the experimental results such that experimental measurements utilizing differing coaxial cell diameters and probe lengths, upon correction with the Poisson model derived correction factor, all produce the same results thereby lending support for the use of an augmented measurement technique, described herein, for measurement of absolute permittivity, as opposed to the traditional TDR measurement of apparent permittivity.
准确测量水分含量是水文、地球物理和生物地球化学研究以及材料特性描述和过程控制的首要要求。在这些领域中,对于从棉花纤维成熟度的表征到土壤保水研究中土壤水分含量的准确表征,再到生物植物水分利用以及离子物种在细胞膜中的化学反应和扩散,以及在表面膜中发生的密集悬浮液中,表面面积和结合水含量的准确测量变得越来越重要。在这些结合水材料中,传统时域反射仪(“TDR”)的误差超出了正在测量的材料介电常数的全跨度范围。因此,迫切需要重新检查 TDR 系统并确定误差所在,以便指导未来的研究。一种满足日益增长的高精度水分含量测量需求的有前途的技术是利用材料的电介电特性描述。通过时域反射仪测量表观介电常数,该技术在土壤科学和地质界以及许多过程控制应用中得到了广泛应用。然而,最近的研究表明,需要提高传统 TDR 提供的精度。然后,最合理的途径是从基于 TDR 的测量过渡到网络分析仪对绝对介电常数的测量,这将消除高表面积土壤和电导率对传统 TDR 应用中表观介电常数测量的不利影响。本研究从同轴探头的理论基础出发,该探头是现代 TDR 探头的起源,为进行绝对介电常数测量提供了依据。研究揭示了目前在公认的介电常数测量技术中使用的公式,这些公式由于 TDR 通过从探头末端辐射能量而不是将其返回源,从而违反了基本模型中固有的基本假设,从而违反了基本模型。为了消除本文实验结果中的辐射影响,本研究使用了各种直径和探头长度的定制设计的同轴探头来测试同轴电池测量技术在确定绝对介电常数方面的准确性。通过这样做,研究表明,文献中可用的基本模型都省略了一个关键的校正因子,本研究假设该因子很可能是由于边缘电容引起的。为了验证该理论,本文建立了一个同轴电池的泊松模型,以计算边缘电容提供的有效附加长度,然后利用该有效附加长度来校正实验结果,使得利用不同的同轴电池直径和探头长度进行的实验测量在经过泊松模型导出的校正因子校正后,均产生相同的结果,从而支持使用本文所述的增强测量技术来测量绝对介电常数,而不是传统的 TDR 测量表观介电常数。