GPR测量滨海盐渍土剖面分层的实验研究
作者:
作者单位:

山东农业大学农业资源利用博士后流动站,山东农业大学农业资源利用博士后流动站,山东农业大学农业资源利用博士后流动站,山东农业大学农业资源利用博士后流动站,山东农业大学农业资源利用博士后流动站,山东农业大学农业资源利用博士后流动站,曲阜师范大学地理与旅游学院

作者简介:

通讯作者:

中图分类号:

S152;S159

基金项目:

山东省自然科学基金项目(ZR2015PD001)资助。


Experimental Study on GPR Measurement of Coastal Saline Soil Profile
Author:
Affiliation:

Qufu Normal University,Postdoctoral Research Station of Agricultural Resources and Environment, Shandong Agricultural University,Postdoctoral Research Station of Agricultural Resources and Environment, Shandong Agricultural University,Postdoctoral Research Station of Agricultural Resources and Environment, Shandong Agricultural University,Postdoctoral Research Station of Agricultural Resources and Environment, Shandong Agricultural University,Postdoctoral Research Station of Agricultural Resources and Environment, Shandong Agricultural University,School of Geography and Tourism, Qufu Normal University

Fund Project:

  • 摘要
  • |
  • 图/表
  • |
  • 访问统计
  • |
  • 参考文献
  • |
  • 相似文献
  • |
  • 引证文献
  • |
  • 资源附件
  • |
  • 文章评论
    摘要:

    土壤剖面分层是GPR调查研究工作的主要内容,也是时域信息提取和定量反演的基础。使用250 MHz的pulseEKKO PRO探地雷达,探测不同植被覆盖或同一植被长势差异的地块,开挖剖面实测对比GPR的分层结果,剖析电磁波信号对土壤水分、盐分、粒径组成3个因子的响应特征。结果表明,从GPR波谱特征中可以区分表层盐渍化程度不同的地块,误差多小于0.5 m;综合波谱影像和振幅变化数据,能够辨晰0 ~ 1 m的土层信息,分层误差可达0.1 m;土壤盐分对电磁波信号的影响特征在该地区表现得十分显著。

    Abstract:

    The identification of soil profile layers is the main research content of GPR investigation and also the basis job of time-domain signals extraction and quantitative inversion. In this study, pulseEKKO PRO GPR of 250 MHz central frequency was used to detect the soil profile layers of plots covered by different vegetation coverages or plots covered by same vegetation but with different growing conditions, and the results were compared the soil profile layers obtained by the method of digging profiles, and the response characteristics of electromagnetic wave signals to soil water, salinity and grain size composition were also analysed. The results showed that: 1) By observing GPR spectral images, soil profile variation with different vegetation coverages and growing conditions can be distinguished with errors mostly are less than 0.5 m. 2) Soil layer information in the depth of 0–1 m can be clearly distinguished with comprehensive analyses of soil profile spectral images and amplitude-time data with 0.1 m discriminating error of soil layering. 3) The effects of soil salinity on electromagnetic wave signals are very significant in this region.

    参考文献
    相似文献
    引证文献
引用本文

王 萍,李新举,闵祥宇,杨 东,王 新,李俊颖,孙小银. GPR测量滨海盐渍土剖面分层的实验研究[J].土壤,2016,48(6):1261-1269. WANG Ping, LI Xinju, MIN Xiangyu, YANG Dong, WANG Xin, LI Junying, SUN Xiaoyin. Experimental Study on GPR Measurement of Coastal Saline Soil Profile[J]. Soils,2016,48(6):1261-1269

复制
分享
文章指标
  • 点击次数:
  • 下载次数:
  • HTML阅读次数:
  • 引用次数:
历史
  • 收稿日期:2016-05-18
  • 最后修改日期:2016-07-09
  • 录用日期:2016-07-14
  • 在线发布日期: 2016-11-14
  • 出版日期: 2016-12-25