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首页> 外文期刊>Transactions of the ASABE >Soil Structure and Texture Effects on the Precision of Soil Water Content Measurements with a Capacitance-Based Electromagnetic Sensor
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Soil Structure and Texture Effects on the Precision of Soil Water Content Measurements with a Capacitance-Based Electromagnetic Sensor

机译:土壤结构与纹理效应对土壤水分含量测量的精度,电容基电磁传感器

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摘要

The physical properties of soil, such as structure and texture, can affect the performance of an electromagnetic sensor in measuring soil water content. Historically, calibrations have been performed on repacked samples in the laboratory and on in situ soils in the field, but little research has been done on laboratory calibrations with intact (undisturbed) soil cores. In this study, three replications each of disturbed and undisturbed soil samples were collected from two soil texture classes (Yutansilty clay loam and Fillmore silt loam) at a field site in eastern Nebraska to investigate the effects of soil structure and texture on the precision of a METER Group GS-1 capacitance-based sensor calibration. In addition, GS-1 sensors were installed inthe field near the soil collection sites at three depths (0.15, 0.46, and 0.76 m). The soil moisture sensor had higher precision in the undisturbed laboratory setup, as the undisturbed calibration had a better correlation [slope closer to one, R~2 _undisturbed (0.89) > R~2 _disturbed (0.73)] than the disturbed calibrations for the Yutan and Fillmore texture classes, and the root mean square difference using the laboratory calibration (RMSD_L) was higher for pooled disturbed samples (0.053 m~3 m~(-3)) incomparison to pooled undisturbed samples (0.023 m~3 m~(-3)). The uncertainty in determination of volumetric water content (theta_v )was higher using the factory calibration (RMSD_F) in comparison to the laboratory calibration (RMSD_L) for the differentsoil structures and texture classes. In general, the uncertainty in estimation of soil water depth was greater than the uncertainty in estimation of soil water depletion by the sensors installed in the field, and the uncertainties in estimation of depthand depletion were lower using the calibration developedfrom the undisturbed soil samples. The undisturbed calibration of soil water depletion would determine water demand mth better precision and potentially avoid over-watering, offering relief from water shortages. Further investigation ofsensor calibration techniques is required to enhance the applicability of soil moisture sensors for efficient irrigation management.
机译:土壤的物理性质,如结构和质地,可以影响电磁传感器在测量土壤含水量方面的性能。从历史上看,已经在实验室的重新包装样本和现场原位土壤中进行了校准,但在具有完整(未受干扰的)土核的实验室校准中已经完成了较少的研究。在这项研究中,从内布拉斯加州东部的一个土壤纹理类(Yutansilty粘土壤土和Fillmore Silt Loam)收集了每种干扰和未受干扰的土壤样品的三种复制,以研究土壤结构和质地对A的精度的影响仪表组GS-1基于电容的传感器校准。此外,GS-1传感器在三个深度(0.15,0.46和0.76米)附近安装了靠近土壤收集部位的田间。未受干扰的实验室设置中的土壤湿度传感器具有更高的精度,因为未受干扰的校准具有更好的相关性[斜坡更靠近一个,R〜2 _未经(0.89)> R〜2 _Disturbed(0.73)]而不是yatan的受扰动的校准和Fillmore纹理类,并且使用实验室校准(RMSD_L)的根均线差异对于池的干扰样品(0.053m〜3 m〜(3))且融合到汇集不受干扰的样品(0.023 m〜3 m〜( - 3))。与不同的实验室校准(RMSD_L)相比,使用工厂校准(RMSD_F)测定体积含水量(THETA_V)的不确定性,用于不同的结构和纹理等级。通常,估计土壤水深的不确定性大于安装在该领域中的传感器估计土壤水耗尽的不确定性,并且使用校准的校准,估计深度耗尽的不确定性,从未受干扰的土壤样品开发。未受干扰的土壤水耗尽校准将决定水需求最佳精确度,避免过度浇水,从水短缺提供救济。需要进一步调查衡量传感器校准技术,以提高土壤湿度传感器的适用性,以实现有效的灌溉管理。

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