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首页> 外文期刊>International journal of remote sensing >Potential of polarimetric Radarsat-2 data in geological mapping -a case study in parts of Dharwar craton, India
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Potential of polarimetric Radarsat-2 data in geological mapping -a case study in parts of Dharwar craton, India

机译:极化Radarsat-2数据在地质测绘中的潜力-以印度Dharwar克拉通部分地区为例

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摘要

Polarimetry is a technique for quantitatively estimating the change in polarization in a backscattered electromagnetic signal (in this case a radar signal) with reference to the polarization of the incident signal for estimating the geophysical properties (roughness and dielectric constant) of surface elements. In this study, quadrapole Radarsat-2 data have been utilized for mapping geological elements in Archaean terrain based on their geophysical parameters preserved in the four polarization channels of Radarsat-2 data. The study illustrates how single-look complex polarimetric data can be processed to extract information on lithology, geological structure, and land covers (i.e. soil type, etc.) preferentially developed over each rock type. The study revealed that C-band polarization power images can be used indirectly to delineate lithounits provided each unit has characteristic surface roughness and moisture resulting from the surface cover or exposure pattern developed over each lithounit. Moreover, polarimetric data (inclusive of phase and amplitude) provide complementary information when we compare this information with the information derived from simple polarization composites, derived from the backscattered image of each polarization channel. It is also observed that structural imprints are enhanced in co-polarized (HH, VV) data, whereas the cross-polarized channel (HY VH) provides information on land cover.
机译:极化测定法是一种技术,它根据入射信号的极化量定量地估计后向散射电磁信号(在这种情况下为雷达信号)中的极化量变化,以估算表面元素的地球物理性质(粗糙度和介电常数)。在这项研究中,基于保留在Radarsat-2数据的四个极化通道中的地球物理参数,利用四极Radarsat-2数据绘制了古生界地形中的地质元素。这项研究说明了如何处理单一的复杂极化数据,以提取优先于每种岩石类型开发的岩性,地质结构和土地覆盖(即土壤类型等)信息。该研究表明,只要每个单元具有特征性的表面粗糙度和水分(由于每个岩石单元上形成的表面覆盖物或曝光图案而产生),就可以间接使用C波段极化功率图像来描绘岩石单元。此外,当我们将偏振数据(包括相位和幅度)与从简单偏振复合材料得到的信息(从每个偏振通道的反向散射图像得到的信息)进行比较时,它会提供补充信息。还可以观察到,同极化(HH,VV)数据中的结构印记得到了增强,而交叉极化通道(HY VH)提供了土地覆盖的信息。

著录项

  • 来源
    《International journal of remote sensing》 |2013年第6期|1893-1904|共12页
  • 作者单位

    Geosciences Division, National Remote Sensing Centre, Indian Space Research Organization,Hyderabad, Andhra Pradesh 500625, India;

    Geosciences Division, National Remote Sensing Centre, Indian Space Research Organization,Hyderabad, Andhra Pradesh 500625, India;

    Geosciences Division, National Remote Sensing Centre, Indian Space Research Organization,Hyderabad, Andhra Pradesh 500625, India;

    Geosciences Division, National Remote Sensing Centre, Indian Space Research Organization,Hyderabad, Andhra Pradesh 500625, India;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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