...
首页> 外文期刊>Geosciences >Prospecting and Evaluation of Underground Massive Ice by Ground-Penetrating Radar
【24h】

Prospecting and Evaluation of Underground Massive Ice by Ground-Penetrating Radar

机译:地下透过雷达勘探与评价地下冰块

获取原文
           

摘要

Data from geocryological studies of soil and rock massifs in permafrost zone are very important as a basis for predicting possible negative consequences associated with climate change. A promising technique for studying geocryological structures (various types of underground ice) is the ground-penetrating radar (GPR) method. This paper presents the applications of the GPR method to prospect and evaluate massive ice in a frozen rock mass. To study the features of GPR signals received during sounding of underground ice, a model of a single GPR trace for the structure “frozen rock-ice-frozen rock” was developed. As a result, regularities were established in the kinematic and dynamic characteristics of GPR signals at the upper and lower boundaries of massive ice, depending on its geometric parameters. The established features were confirmed by the results of computer and physical simulation of GPR measurements of a frozen rock mass model. The main result of the study was to obtain a set of criteria for identifying massive ice according to GPR measurements. The developed criteria will allow the use of GPR for a detailed study of the structure of permafrost rocks to prevent the development of dangerous cryogenic processes in undisturbed and urban areas of the Arctic.
机译:多年冻土区土壤和岩石地块地理学研究的数据非常重要,作为预测与气候变化相关的可能负面后果的基础。用于研究地理统计学结构的有希望的技术(各种类型的地下冰)是地面穿透雷达(GPR)方法。本文介绍了GPR方法在冷冻岩体中展望和评价巨大冰的应用。为了研究地下冰的发声期间收到的GPR信号的特征,开发了结构“冷冻岩石 - 冰冻岩”的单个GPR迹线模型。结果,根据其几何参数,在大规模冰的上边界和下边界的GPR信号的运动和动态特征中建立了规律。通过冻结岩质量模型的GPR测量的计算机和物理模拟来确认已建立的特征。该研究的主要结果是根据GPR测量获得一组用于识别大量冰的标准。发达的标准将允许使用GPR进行详细研究多年冻土岩石结构,以防止在北极的未受干扰和城市地区的危险低温过程的发展。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号