识别由SAR和实验室测量得出的地表热特性

A. Saepuloh, E. K. Army, Agustan
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引用次数: 1

摘要

合成孔径雷达(SAR)数据为冠层植被下的地表制图提供了巨大的潜力。不考虑时间和大气条件的SAR观测对印度尼西亚等热带地区的制图具有优势。利用SAR后向散射数据可以得到地表参数,包括表面粗糙度、湿度和介电常数。然而,由于传感器工作在微波区,基于SAR遥感的地表热物性估算比较复杂。同时,地表热特性对于估算自然或人为源(如火山活动、城区、森林火灾或蒸汽点)引起的地表温度至关重要。为了从SAR数据中识别热特征,我们进行了实验室实验,将从SAR参数中获得的材料的热特性结合起来。实验通过加热地热田蚀变岩和密集植被田泥炭等地表物质进行。我们测量了样品随温度变化的水分、电势、磁化率和磁导率。测量温度由热像仪FLIR C2和地面温度计FLUKE 52控制至250°C。根据测量,我们发现在温度超过100°C时,材料的水分和电势明显下降。一个有趣的现象是,磁化率和渗透率对蚀变岩石和泥炭样品温度的响应相似。温度升高一般会导致磁化率和磁导率降低。岩石和泥炭的矿物和有机含量控制着它们的磁性。然后将实验室测量结果与地热系统蒸汽场的磁导率反演sar后向散射数据进行了比较。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Identifying Thermal Properties of Ground Surface Derived by SAR and Laboratory Measurements
The Synthetic Aperture Radar (SAR) data provide great potential for ground surface mapping under canopy vegetation. The SAR observations regardless time and atmospheric condition are superior for mapping under torrid zones such as Indonesia. The ground surface parameters including surface roughness, moisture, and dielectric constant could be derived by SAR backscattering data. However, estimating thermal properties of ground surface based on SAR remote sensing is complicated because of sensor operation in microwave region. Meanwhile, the thermal properties of ground surface are crucial for estimating surface temperature originated from natural or anthropogenic sources such volcanic activity, urban area, forest fire, or steam spots. To identify the thermal signature from the SAR data, we performed laboratory experiments by incorporating thermal property of materials to be derived from SAR parameters. The experiments were performed by heating ground surface materials including altered rocks from geothermal field and peats from dense vegetation field. We measured moisture, electric potential, magnetic susceptibility, and permeability of the samples with variation of temperature. The measured temperature was controlled by thermal camera FLIR C2 and ground thermometer FLUKE 52 up to 250°C. According to the measurement, we identified that the moisture and electric potential of materials are decrease significantly at temperature more than 100°C. An interesting phenomenon could be reported that the magnetic susceptibility and permeability response to the altered rock and peat samples temperature similarly. The increasing temperature leads to decrease magnetic susceptibility and permeability in general. The mineral and organic content of the rocks and peats controlled their magnetic properties. The laboratory measurement results were then compared to the magnetic permeability derived-SAR backscattering data at a steam field of geothermal system.
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