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Development of a Rapid Soil Water Content Detection Technique Using Active Infrared Thermal Methods for In-Field Applications

机译:主动红外热法在土壤中快速检测土壤水分的技术开发

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摘要

The aim of this study was to investigate the suitability of active infrared thermography and thermometry in combination with multivariate statistical partial least squares analysis as rapid soil water content detection techniques both in the laboratory and the field. Such techniques allow fast soil water content measurements helpful in both agricultural and environmental fields. These techniques, based on the theory of heat dissipation, were tested by directly measuring temperature dynamic variation of samples after heating. For the assessment of temperature dynamic variations data were collected during three intervals (3, 6 and 10 s). To account for the presence of specific heats differences between water and soil, the analyses were regulated using slopes to linearly describe their trends. For all analyses, the best model was achieved for a 10 s slope. Three different approaches were considered, two in the laboratory and one in the field. The first laboratory-based one was centred on active infrared thermography, considered measurement of temperature variation as independent variable and reported r = 0.74. The second laboratory–based one was focused on active infrared thermometry, added irradiation as independent variable and reported r = 0.76. The in-field experiment was performed by active infrared thermometry, heating bare soil by solar irradiance after exposure due to primary tillage. Some meteorological parameters were inserted as independent variables in the prediction model, which presented r = 0.61. In order to obtain more general and wide estimations in-field a Partial Least Squares Discriminant Analysis on three classes of percentage of soil water content was performed obtaining a high correct classification in the test (88.89%). The prediction error values were lower in the field with respect to laboratory analyses. Both techniques could be used in conjunction with a Geographic Information System for obtaining detailed information on soil heterogeneity.
机译:这项研究的目的是研究主动红外热成像和测温法与多元统计偏最小二乘分析相结合作为实验室和现场快速土壤含水量检测技术的适用性。这样的技术可以快速测量土壤水分,这对农业和环境领域都非常有用。这些技术基于散热理论,通过直接测量加热后样品的温度动态变化进行了测试。为了评估温度动态变化,在三个时间间隔(3、6和10 s)内收集了数据。为了说明水和土壤之间存在的比热差异,使用斜率对分析进行调节以线性描述其趋势。对于所有分析,均以10 s的斜率获得了最佳模型。考虑了三种不同的方法,其中两种在实验室中,一种在现场。第一个基于实验室的实验室以主动红外热成像技术为中心,将温度变化的测量视为独立变量,报告的r = 0.74。第二个基于实验室的实验室专注于主动红外测温,将辐射作为独立变量进行了补充,据报道r = 0.76。田间试验通过主动红外测温法进行,暴露于初次耕作后,通过太阳辐照加热裸土。将一些气象参数作为自变量插入到预测模型中,得出r = 0.61。为了获得更一般和广泛的估计,对土壤水分的三类百分比进行了偏最小二乘判别分析,在测试中获得了较高的正确分类率(88.89%)。相对于实验室分析,该领域的预测误差值较低。两种技术都可以与地理信息系统结合使用,以获得有关土壤异质性的详细信息。

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